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Evolution of Early Human Traits Not Simple and Straightforward, Say Scientists

Gone are the days when paleoanthropologists could characterize the path of human evolution as a simple, single homogenous line of progressive changes in human morphology and behavior. Or so suggests a collaborative group of scientists who, as detailed in a study published in the July 4, 2014 issue of Science, came up with a new synthesis, or at least the rudimentary framework of one. It is a developing scenario that, they argue, more accurately explains how earlier forms of Homo (early humans) and their Australopithecus forerunners eventually led to the emergence of Homo sapiens (modern humans), the last surviving hominin.

Led jointly by Susan Antón, professor of anthropology at New York University, paleoanthropologist Richard Potts, curator of anthropology and director of the Human Origins Program at the Smithsonian’s National Museum of Natural History, and Leslie Aiello, president of the Wenner-Gren Foundation for Anthropological Research, the team studied paleoclimate, fossil, and stone tool evidence, leading to a developing consensus that suggests a rethinking of long-held assumptions about human origins and evolution. Based on a synthesis of the data, the researchers point to change and diversity of environmental conditions and the compelling need to survive by adapting to the changing conditions as a key to understanding how early humans were able to vary, survive and begin spreading from Africa to Eurasia 1.85 million years ago. The process entailed a diversification of species and genera differentiating and overlapping in time and morphology, beginning with some key elements once thought to define Homo but actually evolving in earlier Australopithecus ancestors between 3 and 4 million years ago.

Significant to the development of the new synthesis, Potts developed a new climate framework for East African human evolution that depicts most of the era from 2.5 million to 1.5 million years ago as a time of strong climate instability and shifting intensity of annual wet and dry seasons.

“Unstable climate conditions favored the evolution of the roots of human flexibility in our ancestors,” said Potts.  “The narrative of human evolution that arises from our analyses stresses the importance of adaptability to changing environments, rather than adaptation to any one environment, in the early success of the genus Homo.”

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homoevolution1Between 2.1 and 1.8 million years ago, the oldest known species of the human genus, Homo, exhibited diverse traits. These species include the 1470 Group and the 1813 Group, based on the Kenyan fossils KNM-ER 1470 (left) and KNM-ER 1813 (second from left), respectively. By 1.8 to 1.9 million years ago, the species Homo erectus had evolved in Africa and started to spread to Eurasia. Early populations of this long-lived species are represented by the Kenyan fossil KNM- ER 3733 (right) and the Georgian fossil Dmanisi Skull 5 (second from right). The three lineages — the 1470 group, the 1813 group, and Homo erectus — overlapped in time for several hundred thousand years. The Kenyan fossils, from the site of Koobi Fora in the Lake Turkana region of Kenya, are housed in the National Museums of Kenya. Fossils from Dmanisi are housed in the Georgian National Museum. Credits: Kenyan fossil casts – Chip Clark, Smithsonian Human Origins Program; Dmanisi Skull 5 – Guram Bumbiashvili, Georgian National Museum

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homoevolution2Hominin evolution from 3.0 to 1.5 Ma. Green: Australopithecus, Yellow: Paranthropus, Red: Homo. The icons indicate from the bottom the first appearance of stone tools at ~2.6 Ma, the dispersal of Homo to Eurasia at ~1.85 Ma, and the appearance of the Acheulean technology at ~1.76 Ma. The number of contemporaneous hominin taxa during this period reflects different strategies of adaptation to habitat variability. The cultural milestones do not correlate with the known first appearances of any of the currently recognized Homo taxa. Image courtesy of Antón et al., Science/AAAS 2014

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homoevolution3Evolutionary timeline of important anatomical, behavioral and life history characteristics that
were once thought to be associated with the origin of the genus Homo or earliest H. erectus. Image courtesy of Antón et al., Science/AAAS 2014

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Their analysis and conclusions could explain, at least in part, much of the new evidence that has emerged in recent years suggesting that multiple coexisting species of Homo overlapped geographically and developed differentiating morphological and behavioral characeristics. It contrasts with the long-held model of a large brain, long legs, the ability to craft tools and prolonged maturation periods evolving together as a single package at the start of the Homo lineage as African grasslands expanded and Earth’s climate became cooler and drier.

The researchers also analyzed ancient stone tools, isotopes found in teeth and cut marks found on animal bones in East Africa.

“Taken together, these data suggest that species of early Homo were more flexible in their dietary choices than other species,” said Aiello. “Their flexible diet—probably containing meat—was aided by stone tool-assisted foraging that allowed our ancestors to exploit a range of resources.”

The study authors concluded that flexibility likely strengthened the ability of human ancestors to successfully adapt to changing environments and emerge out of Africa, and explains the ability of the modern human species to occupy diverse habitats throughout the world.

The detailed study is published in the July 4, 2014 issue of Science magazine.

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Source: Adapted and edited from a press release of the Smithsonian Institution, Smithsonian scientist and collaborators revise timeline of human origins, 3 July 2014; and Early Human Traits Not Delivered in Single Package, Science, 3 July 2014.

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discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

Gene From Extinct Human Made Tibetans Adaptable to High Altitudes

Tibetans were able to adapt to high altitudes thanks to a gene acquired when their ancestors mated with a species of human they helped push to extinction, according to a new report by University of California, Berkeley, scientists.

An unusual variant of a gene involved in regulating the body’s production of hemoglobin – the molecule that carries oxygen in the blood – became widespread in Tibetans after they moved onto the high-altitude plateau several thousand years ago. This variant allowed them to survive despite low oxygen levels at elevations of 15,000 feet or more, whereas most people develop thick blood at high altitudes, leading to cardiovascular problems.

“We have very clear evidence that this version of the gene came from Denisovans,” a mysterious human relative that went extinct 40,000-50,000 years ago, around the same time as the more well-known Neanderthals, under pressure from modern humans, said principal author Rasmus Nielsen, UC Berkeley professor of integrative biology. “This shows very clearly and directly that humans evolved and adapted to new environments by getting their genes from another species.”

This is the first time a gene from another species of human has been shown unequivocally to have helped modern humans adapt to their environment, he said.

Nielsen and his colleagues at BGI-Shenzhen in China will report their findings online July 2 in advance of publication in the journal Nature.

The gene, called EPAS1, is activated when oxygen levels in the blood drop, triggering production of more hemoglobin. The gene has been referred to as the superathlete gene because at low elevations, some variants of it help athletes quickly boost hemoglobin and thus the oxygen-carrying capacity of their blood, upping endurance. At high altitude, however, the common variants of the gene boost hemoglobin and its carrier, red blood cells, too much, increasing the thickness of the blood and leading to hypertension and heart attacks as well as low-birth-weight babies and increased infant mortality. The variant or allele found in Tibetans raises hemoglobin and red blood cell levels only slightly at high elevation, avoiding the side-effects seen in most people who relocate to elevations above 13,000 feet.

“We found part of the EPAS1 gene in Tibetans is almost identical to the gene in Denisovans and very different from all other humans,” Nielsen said. “We can do a statistical analysis to show that this must have come from Denisovans. There is no other way of explaining the data.”

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tibetangeneA Chinese researcher collects a blood sample from an ethnic Tibetan man participating in the DNA study. Credit: Beijing Genomics Institute (BGI-Shenzhen) photo

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The researchers first reported the prevalence of a high-altitude version of EPAS1 in Tibetans in 2010, based on sequencing of the genomes of numerous Han Chinese and Tibetans. Nielsen and his colleagues argued that this was the result of natural selection to adapt to about 40 percent lower oxygen levels on the Tibetan plateau. That is, people without the variant died before reproducing at a much higher rate than those with it. About 87 percent of Tibetans now have the high-altitude version, compared to only 9 percent of Han Chinese, who have the same common ancestor as Tibetans.

Nielsen and his colleagues subsequently sequenced the EPAS1 gene in an additional 40 Tibetans and 40 Han Chinese. The data revealed that the high-altitude variant of EPAS1 is so unusual that it could only have come from Denisovans. Aside from its low frequency in Han Chinese, it occurs in no other known humans, not even Melanesians, whose genomes are nearly 5 percent Denisovan. A high quality sequence of the Denisovan genome was published in 2012.

Nielsen sketched out a possible scenario leading to this result: modern humans coming out of Africa interbred with Denisovan populations in Eurasia as they passed through that area into China, and their descendants still retain a small percentage – perhaps 0.1 percent – Denisovan DNA. The group that invaded China eventually split, with one population moving into Tibet and the other, now known as Han Chinese, dominating the lower elevations.

He and his colleagues are analyzing other genomes to pin down the time of Denisovan interbreeding, which probably happened over a rather short period of time.

“There might be many other species from which we also got DNA, but we don’t know because we don’t have the genomes,” Nielsen said. “The only reason we can say that this bit of DNA is Denisovan is because of this lucky accident of sequencing DNA from a little bone found in a cave in Siberia. We found the Denisovan species at the DNA level, but how many other species are out there that we haven’t sequenced?”

Nielsen’s coauthors include former UC Berkeley postdoctoral fellow Emilia Huerta-Sánchez, now at UC Merced; postdocs Benjamin Peter and Nicolas Vinckenbosch of UC Berkeley’s Department of Integrative Biology; and colleagues in China, Hong Kong, Denmark, Saudi Arabia and Turkey.

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Source: Adapted and edited from a University of California press release: Extinct human cousin gave Tibetans advantage at high elevation

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Read about the most fascinating discoveries with a premium subscription to Popular Archaeology Magazine.  Find out what Popular Archaeology Magazine is all about.  AND MORE:

On the go? Purchase the mobile version of a recent issue of Popular Archaeology Magazine here for only $2.99.

discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

University of Pennsylvania Museum of Archaeology and Anthropology Plans Summer Events for Public

For the Indiana Jones in all of us, the University of Pennsylvania Museum of Archaeology and Anthropology, arguably the finest museum of its kind in the United States, is offering a summer packed with special guided tours, musical performances and other activities for all ages during the summer of 2014. Events and activities will include such things as Egyptian gallery tours, a Mexico and Central American gallery tour, summer night concerts, and special performances for children. This, of course, is in addition to the usual offering of galleries and exhibits always available to visitors on a regular basis.

Otherwise known as the Penn Museum, it is located at 3260 South Street, Philadelphia, PA 19104 at the intersection of Spruce Street and 33rd Street. Nearby landmarks include Franklin Field, across South Street, and the Hospital of the University of Pennsylvania, across 34th Street.

See the schedule and the website for more information about the museum.

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Cover Photo, Top Left: View of the Penn Museum. Mefman00, Wikimedia Commons

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Read about the most fascinating discoveries with a premium subscription to Popular Archaeology Magazine.  Find out what Popular Archaeology Magazine is all about.  AND MORE:

On the go? Purchase the mobile version of a recent issue of Popular Archaeology Magazine here for only $2.99.

discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

Researchers Discover Population Boom in Ancient American Southwest

Researchers have found that birth rates and life expectancy in the American Southwest between 900 BC and 1400 AD indicated a period of rapid population growth between about 500 AD and 1100 AD followed by a significant decline after 1300 AD, never again to recover the former growth.

The study, conducted with National Science Foundation funding by anthropology professor Tim Kohler and graduate student Kelsey Reese, both of Washington State University, analyzed data on thousands of human remains found at hundreds of sites across the Four Corners region of the Southwest. The data helped to create a chronology of the region’s “Neolithic Demographic Transition” — a time period when stone tool artifacts signaled the agricultural transition from cutting meat to pounding grain.  

“It’s the first step towards all the trappings of civilization that we currently see,” said Kohler.

Maize (corn), the region’s staple crop, was introduced as early as 2000 BC, but productivity was slow to rise until about 400 BC, said Kohler, when the crop is estimated to have provided around 80 percent of the regional population’s calories. A corresponding gradual rise in birth rates ensued until about 500 A.D.

Then, growth rates varied across the region. People in the Sonoran Desert and Tonto Basin, in what is today Arizona, were more culturally advanced, with irrigation, ball courts, and eventually elevated platform mounds and compounds housing elite families. Yet birth rates were higher among people to the north and east, in the San Juan basin and northern San Juan regions of northwest New Mexico and southwest Colorado.

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pueblobonitobobadamsAerial view of Pueblo Bonito in Chaco Canyon, New Mexico. Bob Adams, Wikimedia Commons

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Kohler suggested that the Sonoran and Tonto people might have had difficulty finding new farming opportunities for their posterity, as corn farming required irrigation. Water from canals may have also carried harmful protozoa, bacteria and viruses. But groups to the northeast would have been able to expand maize production into new areas as their populations grew, he said.

Around 900 A.D., populations remained high but birth rates began to fluctuate. The mid-1100s saw one of the largest known droughts in the Southwest, when the region had likely hit its carrying capacity, with continued population growth and limited resources similar to what Thomas Malthus predicted for the industrial world in 1798.

From the mid-1000s to 1280—by which time all the farmers had left—evidence indicates that conflicts raged across the northern Southwest, but birth rates remained high.

“They didn’t slow down—birth rates were expanding right up to the depopulation,” said Kohler. “Why not limit growth? Maybe groups needed to be big to protect their villages and fields.”

“It was a trap,” said Kohler. “A Malthusian trap but also a violence trap.”

The northern Southwest had as many as 40,000 people in the mid-1200s, but within 30 years it was empty. Kohler hypothesizes that the population may have become too large to be sustained as climates deteriorated, and the lower population would not have adequately maintained the social unity needed for defense and new infrastructure.

But whatever the reason, he said, the experience of the ancient Puebloans could suggest that “population growth has its consequences.”

The paper is published in the Proceedings of the National Academy of Sciences as “Long and spatially variable Neolithic Demographic Transition in the North American Southwest,” by Timothy A. Kohler and Kelsey M. Reese.

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Edited and adapted from a Washington State University press release, “WSU Researchers chart an ancient baby boom”.

Cover Photo, Top Left: A digital model of ancient Pueblo Bonito (Chaco Canyon, New Mexico, U.S.) before it was abandoned. Wikimedia Commons

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Read about the most fascinating discoveries with a premium subscription to Popular Archaeology Magazine.  Find out what Popular Archaeology Magazine is all about.  AND MORE:

On the go? Purchase the mobile version of the current issue of Popular Archaeology Magazine here for only $2.99.

discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

Scientists Uncover Evidence of Early Human Diet

Researchers continue to make progress in their efforts to understand an essential aspect of prehistoric lifeways and a major contributing factor in the dynamics of human evolution — the human diet. In two studies, one focusing on an archaeological site in Spain, the other in the Turkana Basin in Africa, scientists are suggesting that early humans had a more diverse diet than traditionally thought.

In the first study, published June 25 in the open access journal PLOS ONE, Ainara Sistiaga from the Massachusetts Institute of Technology and University of La Laguna and colleagues examine human fecal matter (poop) detected in sediment samples taken from different occupational floor levels at the site of El Salt in Spain, a site known to have been inhabited by Neanderthals 50,000 years ago. The fecal matter indicated, based on the analysis of fecal biomarkers, that these Neanderthals predominantly consumed meat, consistent with the widely accepted dietary model for Neanderthals, but that they also consumed plant foods. One of the fecal biomarkers was formed by the bacterial reduction of cholesterol in the gut (coprostanol), an indicator of meat consumption, but the other showed the presence of a compound found in plant sources, evidence of significant plant intake.

“Taken together, these data suggest that the Neanderthals from El Salt consumed both meat and vegetables, in agreement with recent hypotheses based on indirect evidence,” conclude Sistiaga and colleagues in the study. “Future studies in Middle Palaeolithic sites using the fecal biomarker approach will help clarify the nature, role and proportion of the plant component in the Neanderthal diet, and allow us to assess whether our results reflect occasional consumption or can be representative of their staple diet.”*

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humanpooppicView of El Salt archeological site. Credit: Ainara Sistiaga

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In another study, to be published soon in the Journal of Human Evolution, scientists have found that aquatic fauna (fish and other water-based animals) may have been a highly nutritious source of food for early Pleistocene humans living in the Turkana Basin of East Africa almost 2 million years ago. In this case, Will Archer of the Max Planck Institute for Evolutionary Anthropology and colleagues employed multiple datasets to examine aquatic resource use in the early Pleistocene by focusing on four components of aquatic faunal assemblages: taxonomic diversity; skeletal element proportions; bone fragmentation; and bone surface modification from tool use. These components were used to identify associations between early Pleistocene aquatic remains and hominin behavior at the site of FwJj20 in the Koobi Fora Formation of the Turkana Basin in Kenya. The researchers focused on two dominant aquatic species: catfish and turtles.

Based on their findings, the researchers suggest that aquatic food sources provided hominins (early humans) with a significant alternative or supplement to other, terrestrial food sources. They also suggest that aquatic food sources provided some important advantages, such as “(1) a probable reduction in required investment of energy relative to economic return in the form of nutritionally dense food items, (2) a decrease in the technological costs of resource acquisition, and (3) a reduced level of inter-specific competition associated with carcass access and an associated reduction of predation risk relative to terrestrial sources of food.”**

The Turkana Basin, which includes Lake Turkana and the Koobi Fora (ridge) Formation, is well known in human evolution studies as one of the richest and most important sources of hominin fossils shedding light on the evolution of man over the past 4.2 million years.

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laketurkanadoronLake Turkana in the Turkana Basin. Near the ancient shores of this lake, some of the most important early human finds were discovered. Doron, Wikimedia Commons

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*Sistiaga A, Mallol C, Galvan B, Summons RE (2014) The Neanderthal Meal: A New Perspective Using Faecal Biomarkers. PLOS ONE 9(6): e101045. doi:10.1371/journal.pone.0101045  http://dx.plos.org/10.1371/journal.pone.0101045

** Will Archera, David R. Braunb, Jack W.K. Harrisc, Jack T. McCoyd, Brian G. Richmond, Early Pleistocene aquatic resource use in the Turkana Basin http://www.sciencedirect.com/science/article/pii/S004724841400056

Cover Photo, Top Left: View of El Salt archeological site. Credit: Ainara Sistiaga

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Read about the most fascinating discoveries with a premium subscription to Popular Archaeology Magazine.  Find out what Popular Archaeology Magazine is all about.  AND MORE:

On the go? Purchase the mobile version of the current issue of Popular Archaeology Magazine here for only $2.99.

discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

Archaeologists Return to Ancient Megiddo

Archaeologists are now onsite at Tel Megiddo, in northern Israel, to continue large-scale excavations at what has often been called the “crown jewel” of archaeological sites of the Levant, or Eastern Mediterranean region.

Led by well-known archaeologists Israel Finkelstein of Tel Aviv University and Eric Cline of the George Washington University, a team of archaeologists, students, volunteers and other specialists will be excavating where they left off in 2012, when they encountered a large building featuring 18 pillars dated to the Iron Age IIA period, (around 1000 BCE).  South of the building they uncovered a hoard of six iron daggers and two bronze bowls, dating to the Iron Age I (1200 – 1000 BCE).

Tel Megiddo, a World Heritage site, is best known for the remains of a large Canaanite center that once ruled at a location strategically placed at one of the most important military and trade routes in the ancient Near East, the Via Maris, dominating trade and commercial traffic for over 6,000 years beginning around 7000 BCE. The city is often mentioned in ancient literature and documents such as the Hebrew Bible and the el-Amarna letters of ancient Egypt, particularly as the site of epic battles that changed the course of ancient history in the region. As the inspiration for James Michener’s novel, The Source, the site affords a layer-cake of remains of ancient civilizations that came and went at the location, each succeeding civilization building upon the ruins of predecessors. This has created a treasure for archaeologists and their sponsors, who for decades have been unearthing monumental temples, palace complexes, massive fortifications, and sophisticated water systems, adding to our understanding of Bronze Age and Iron Age settlement and lifeways in the Levant. Some of the major finds of recent seasons have included a hoard of gold, silver and bronze jewelry, all wrapped in fabric and hidden in a vessel dated to around 1100 B.C.; and an Early Christian prayer hall with a mosaic floor discovered at a prison site near the Tel.

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megiddocitygategolfbravoThe Iron Age city gate at Megiddo, one of the main attractors for toursits at the site. Golf Bravo, Wikimedia Commons

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modelmegiddoalamguinnessModel of Megiddo in its ancient fortified glory. Alma Guinness, Wikimedia Commons

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For the 2014 season, archaeologists will continue work on the pillared structure exposed in 2012; expose some late Middle Bronze Age (1800 – 1540 BCE) domestic architecture; continue to excavate parts of the early Middle Bronze Age fortification system which includes a massive mudbrick wall and glacis (defensive slope construction); study areas related to Late Bronze-Iron Age street levels; expose more of the Late Bronze Age levels excavated previously; and conduct exploratory soundings in three new locations.

The Tel Megiddo Expedition offers one of the best field school and excavation experiences for students and volunteers in the Levant. More information about the Expedition and the field school can be obtained at their website.

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Cover Photo, Top Left: The Megiddo altar. James Emery, Wikimedia Commons

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Read about the most fascinating discoveries with a premium subscription to Popular Archaeology Magazine.  Find out what Popular Archaeology Magazine is all about.  AND MORE:

On the go? Purchase the mobile version of the current issue of Popular Archaeology Magazine here for only $2.99.

discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

News for June 19, 2014

Stonehenge’s Singing Stones 

Could the massive standing stones of Stonehenge also have made sounds? The New York Times 

 

Archaeologists to Assess Condition of Kedarnath Temple

A team of archaeologists and officials left Wednesday for the Kedarnath temple in Uttarakhand to assess the condition of the shrine that was badly damaged in flash floods a year ago……. Mid-Day

 

The Last Biblical Frontier

Archeologists unearth findings in biblical site dating back to Joshua and the Judges. The Jerusalem Post

 

Archaeologists discover 4,000-year-old necklace was made from dog whelk and tusk shells

Bronze Age Brits were wearing bling around 4,000 years before today’s flashy pop stars and footballers, reveals new research. Daily Mail

 

Fossil Human Skulls Unearthed in Spanish Cave Shed Light on Neandertal Evolution

The recent recovery and analysis of 17 early human fossil skulls from the Sima de los Huesos (“Pit of Bones”) cave pit site in the Sierra de Atapuerca cave system of northern Spain have illuminated our understanding of how Neandertals, a more ancient, extinct sister species of Homo sapiens (modern humans), actually evolved, according to a study report published this week in Science.

Currently led by Juan Luis Arsuaga of the Universidad Complutense de Madrid, Spain, archaeological teams have been excavating at the site for four decades, and have recovered the largest assemblage of early human fossils ever discovered at any one site in the world. 

“After thirty years, we have recovered nearly 7,000 human fossils corresponding to all skeletal regions of at least 28 individuals,” says study co-author Ignacio Martinez, Professor of Paleontology at the University of Alcalá. “This extraordinary collection includes 17 fragmentary skulls, many of which are very complete.”

The 17 skulls, according to the researchers, represent a single population of a hominin (early human) species. Although some of have been studied before, seven are presented anew here, and six are more complete than ever before, after many hours of painstaking assemblage in the lab. Now, with the mostly intact samples for study, the researchers have been able to more clearly define the common features of what they believe to be a single population. 

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simasiteThe Sima de los Huesos site. Image courtesy Javier Trueba / Madrid Scientific Films

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The fossils exhibited a mosaic of physical characteristics that could not be wholly attributed to any single, recognized human species to date. The skull samples showed clear Neandertal features in the face and teeth. The researchers suggest these ‘Neandertal-derived’ features were functionally related to mastication, or chewing. “It seems these modifications had to do with an intensive use of the frontal teeth,” Arsuaga said. “The incisors show a great wear as if they had been used as a ‘third hand,” typical of Neanderthals.” But elsewhere, the skulls showed characteristics that diverted from the Neandertal model. The braincase itself, for example, still showed features associated with more primitive hominins.

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simaskull17Skull 17 from the Sima de los Huesos site in Sierra de Atapuerca, Spain. Image courtesy Javier Trueba / Madrid Scientific Films

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simaskull15Skull 15. Image courtesy Javier Trueba / Madrid Scientific Films

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simaskull9Skull 9. Image courtesy Javier Trueba / Madrid Scientific Films

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Observations like these led the researchers to suggest support for the ‘accretion model’ of Neandertal evolution, or something similar to cladogenesis, wherein evolution takes place through a splitting of species into branches or “clades”, leading to the development of a greater variety of sister species.

However, according to Arsuaga,”we think based on the morphology that the Sima people were part of the Neanderthal clade, although not necessarily direct ancestors to the classic Neanderthals.”

“One thing that surprised me about the skulls we analyzed,” Arsuaga continued, “is how similar the different individuals were. The other fossils of the same geological period are different and don’t fit in the Sima pattern. This means that there was a lot of diversity among different populations in the Middle Pleistocene.”

In other words, because other European Middle Pleistocene fossil specimens found in Europe do not exhibit the suite of features seen in this fossil group, the researchers suggest that more than one evolutionary lineage appears to have coexisted during the European Middle Pleistocene, with that represented by the Sima sample being closer to the Neandertals. The work of Arsuaga et al. suggests that facial modification was the first step in Neandertal evolution, a mosaic pattern fitting the prediction of the accretion model.

Key to the study findings was the homogeneity of the Sima samples. “All of the individuals recovered at the site represent the same biological population which makes it possible for anthropologists to study individual variation as well as sexual differences in the skeleton and patterns of growth and development, among other aspects,” report Arsuaga, et al. in a press release of the Centro Mixto UCM-ISCIII de Evolución y Comportamiento Humano. “While considerable differences in size are apparent within the collection, with some larger skulls and some smaller ones, the anatomical features that anthropologists study to examine evolutionary relationships do not vary much within the Sima population. This combination of mosaic evolution and anatomical homogeneity led the authors to favor a branching pattern of evolution, known as cladogenesis in evolutionary studies, in the European Middle Pleistocene.”

So what species do these Sima fossils represent? The study authors do not assign the fossils to any specific species. But mitochondrial DNA was recently extracted and analyzed from one of the Sima fossils. The results suggest that this population was not a group of “early Neandertals”. Nor, as has been previously suggested, were they representatives of another early human species called Homo heidelbergensis, thought to be ancestral to the Neandertals. The Sima jawbones (mandibles) were observed to be anatomically distinct from that of heidelbergensis. 

But there is much more to come from the Pit of Bones.

“With excavations continuing and new fossils being discovered each field season,” report Arsuaga, et al., “there is certainly reason to believe that the Sima de los Huesos will yield more surprising findings in the future.”

A detailed feature article about the work and latest findings at Sima de los Huesos will be published in the upcoming September 2014 issue of Popular Archaeology Magazine.

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Information Sources: Press releases of the Centro Mixto UCM-ISCIII de Evolución y Comportamiento Humano and the American Association for the Advancement of Science

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discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

News for June 18, 2014

Joseph Smith Cabin Foundation Excavated at Historic Site

Archaeologists are excavating the early nineteenth-century cabin of Joseph Smith Sr. and wife Lucy Mack, who were parents of Joseph Smith, the founder of the Mormon church. They have also uncovered prehistoric artifacts. The Quincy Herald-Whig 

 

Tiwanaku Tombs Uncovered in Peru

Archaeologists have discovered tombs from the Tiwanaku culture in Peru’s Tambo Valley. Peru This Week

 

Archaeologists Dig Outside the James Fort

Excavations at historic Jamestown in Virginia are now focusing on searching for evidence of the outlying palisades, soldiers’ tents, and other structures. The Daily Press

 

Remains of Plague Victims Discovered at Thebes in Egypt

Archaeologists have unearthed the remains of third-century plague victims at the Funerary Complex of Harwa and Akhimenru of ancient Thebes.  Live Science

Archaeologists Return to Excavate Ancient Jaffa

Teams of archaeologists, students and volunteers will return this month to the site of ancient Jaffa on the central coast of Israel to pick up where they left off in 2013, when they uncovered more of the sensational evidence of a fiery destruction at the site’s ancient Amarna period New Kingdom Egyptian fortress gate. The continuing investigations will also include new elements — the search for the ancient harbor complex, and excavation of evidence of a 14th century B.C. destruction layer at the remains of the site’s Lion Temple. 

Under the direction of project co-directors Aaron Burke, Associate Professor of the Archaeology of Ancient Israel at the University of California, Los Angeles, and Martin Peilstöcker of the Isral Antiquities Authority, one team will continue the excavations at the famous fourteenth century B.C. Egyptian fortress gate complex, where in 2013 they uncovered the stark remains of an extensive violent destruction.

Excavations in 2012 first revealed the evidence, with clues to its extent indicated when excavators discovered a commemorative scarab of Amenhotep III dated to the mid-fourteenth century B.C., found within the upper destruction layers and apparently fallen from what the archaeologists interpreted as a second story administrative office floor. A year later, in 2013, they exposed the city gate’s passageway below more than 1.5 meters of destruction debris. The finds included arrowheads, a spearhead and lead weight, decorative ivory inlays, numerous charred seeds, a number of ceramic vessels, antlers from deer, and nearly two dozen cedar timbers thought to have once made up the gate’s roof and upper story. The seeds, identified as those of barley, olive pits, grape pips, and chick peas were a welcome find, as they provide an insight to the foods consumed at the site.

The assortment of artifacts paint a picture of a city gate that functioned as something more than purely a defensive structure — a complex that housed administrators, storerooms, and other support facilities. Speaking of the antlers, for example, Burke and Peilstöcker noted that they “suggest that the gate was not a stark and utilitarian space as many reconstructions of Egyptian gates suggest. Instead, it would seem that Egyptian soldiers hung these items within the passageway as trophies of their hunting around Jaffa.”**

The timbers, the earliest and largest such ancient timbers from that time period found in Israel to date, are thought to have been used in the construction of the gate’s second story and roof. Reported Burke and Peilstöcker in a press release: “They will provide not only important chronological data such as evidence for the date of the construction of the gate complex but also will contribute to refining our understanding of the evolution of Egyptian rule in Canaan since the gate is one in a sequence of gates providing evidence for the earliest Egyptian fortress in Canaan. As important proxies for climate change, the timbers also offer a unique opportunity for an improved study of the Late Bronze Age environment.”**

Burke and Peilstöcker hope to shed light on the nature of coexistence between the Egyptian occupiers and the native Canaanite inhabitants of the area. “New archaeological data combined with well-known historical texts of the Late Bronze Age are now shedding light on the nature of interactions between the Canaanite inhabitants of Jaffa and its environs and the Egyptian inhabitants of the New Kingdom fortress built atop the city’s earlier remains,” reports Burke and Peilstöcker. “The resulting picture is one colored by episodes of violence and peaceful social interactions in Jaffa over a period of more than 300 years, from ca. 1460 to 1130 BC.”*

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jaffa3Above: The Gate passageway and south tower following excavations in July 2013. Photo 2013-P0408, courtesy Jaffa Cultural Heritage Project.
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jaffa2The charred remains of cedar timber/beams were encountered during the 2013 excavation. Courtesy Jaffa Cultural Heritage Project

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The city of Jaffa has been an important port city for over 4,000 years. By the Late Bronze Age, Jaffa had become a principal port and garrison for the New Kingdom Egyptian empire. Mentioned four times in the Hebrew Bible, it was named as one of the cities given to the Hebrew Tribe of Dan (Book of Joshua 19:46), as a port-of-entry for the cedars of Lebanon for Solomon’s Temple (2 Chronicles 2:16), as the place from which the prophet Jonah embarked for Tarshish (Book of Jonah 1:3) and as the port-of-entry for the cedars of Lebanon that were used in the construction of the Second Temple of Jerusalem (Book of Ezra 3:7). The city is also mentioned in the ancient Egyptian Amarna letters.

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jaffa4The view of Jaffa from the sea (as seen in 1895). From the Detroit Publishing Company Collection, Trialsanderrors, Wikimedia Commons

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Additional investigation at the site will entail excavation in the area of the “Lion Temple”, a structure thought to exhibit characteristics of a sacred or religious nature. The structure acquired its name from the discovery of a lion skull in its southeastern corner by Jacob Kaplan during his excavations there in the early 1970’s. It is thought to be a Caananite building.

The 2014 season will also see exploratory efforts under Shelley Wachsmann of Texas A&M University, whose team will be investigating the area thought to contain the remains of the ancient harbor of Jaffa. The team will use remote-sensing in a deep-water survey for ancient shipwrecks, testing the application of archaeogeophysical and geoarchaeological techniques to identify the ancient harbor. The investigation will also employ a Remotely Operated Vehicle (ROV) to verify anomalies at the 50 to 300 meter depth range that were previously detected.

More information about the Jaffa project can be obtained at the Jaffa Cultural Heritage Project website, and a detailed article about the Jaffa excavations was published in the March 2013 issue of Popular Archaeology.

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https://popular-archaeology.com/issue/march-2013/article/the-egyptian-fortress-in-jaffa

** http://www.nelc.ucla.edu/jaffa/assets/2013_JCHP_Press_Release.pdf (2013 excavation summary)

Cover Photo, Top Left: Excavations of the 14th century BC destruction debris in the Egyptian gateway in Jaffa during fourth week. — with Kandis Gordon, Kris Kowa, Molly Stevens, Kayla Allen, Amy Karoll, Nadia Ben-Marzouk, Jon Schadeberg, Tania Fenwick, Heidi Dodgen and Dani Zwang in Jaffa, Israel. Caption text and photo courtesy Jaffa Cultural Heritage Project

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discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

Climate Change Prompted Migrations in Ancient Peru, Says Genetic Study

“The weather made me do it,” as the saying might have gone for many, long-deceased and unnamed ancient Peruvians. Like some other populations throughout history, they were refugees of climate change who then flourished in their newly found home.

This is the story told by a recent genetic study that suggests that the evidence indicates periods of migration in pre-Columbian Andean societies in Peru, spurred on by local climate changes. It supports the archaeologists, who for years have been saying that the excavated evidence hints of such shifts by the Nasca, Wari and Tiwanaku peoples.

To get to this conclusion, anthropologist Lars Fehren-Schmitz and colleagues collected samples of mitochondrial DNA from 207 individuals in Peru’s Rio Grande de Nasca region and determined that the mitochondrial DNA likely represented Andean populations living between approximately 840 BC and 1450 AD. Using a Bayesian modeling approach, the authors found that the genetic results suggest a migration from the coastal valleys of Southern Peru to the Andean highlands during a period of increasing climate variability around 640 AD. They also found a possible backward migration from the highlands to the coast during a period of drought in the highlands and favorable conditions at the coast around 1200 AD. The study results suggest that climate-driven migrations may have led to a genetic homogenization in Southern Peru over time. 

“The supported migration events coincide with observed climatic alterations, which must have led to a genetic homogenization in the RGND [Rio Grande de Nasca drainage area in southern coastal Peru] over time,” report Fehren-Schmitz and colleagues in the published study. “Most studies analyzing the impact of climate on the mobility and demography of ancient populations have concentrated on foraging societies. Here we reveal climatic impacts on socially complex, agricultural societies. Despite a range of anticipatory agricultural adaptations observed in the archaeological record, the instability of the coastal and highland ecosystems in southern Peru exceeded critical points in the past in which migration became inevitable to sustain the population.”*

The detailed study report is published in the Proceedings of the National Academy of Sciences (PNAS).

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*“Climate change underlies global demographic, genetic, and cultural transitions in pre-Columbian southern Peru,” by Lars Fehren-Schmitz et al., www.pnas.org/cgi/doi/10.1073/pnas.1403466111

Source: Adapted and edited from a University of California, Santa Cruz press release.

Cover Photo, Top Left: Piquillacta archaeological site (ancient Wari construction). AgainErick, Wikimedia Commons

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discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

Archaeologists Excavate Roman Temple Area at Maryport

Beginning the fourth year of a five-year program of investigation, a team of archaeologists, students and volunteers commissioned by the Senhouse Museum Trust have returned to a site near the Maryport Roman fort in the U.K. to continue excavation of the remains of a Roman temple and associated structures and features.

Led by Newcastle University’s Professor Ian Haynes and site director Tony Wilmott, they hope to recover more of the structural remains and artifacts at a site that had undergone investigation in previous years, yielding some intriguing results.

“This year we will be looking at the eastern edge of the [Maryport] settlement, to the north east of the fort, where at least one temple stood,” said Haynes. “This structure was originally excavated in the 1880s, and we re-examined it last year. 

“Immediately under this building we found the remains of a burnt lamb and bird bones. At other sites across Britain and in other countries these have signified a ritual dedication or offering for the building.

“We also found evidence of a mysterious circular structure next to the rectangular temple and we’re going to be investigating this area to find out what this might have been built for – maybe it was another temple, or a mausoleum.” 

Haynes hopes that investigation of this site will help shed additional light on the meaning and importance of stone military altars from the Roman fort of Alauna Carvetiorum and its associated civilian settlement located at what is now Maryport. 

“The Temples project is designed to learn more about the internationally famous altars which form the core of the Senhouse Roman Museum display and to understand better the complex religious landscape of Roman Maryport,” said Haynes.

“The collection of altars in the museum is really remarkable. The inscriptions provide information on the lives of the commanders of the fort and their postings across the Roman Empire. 

“We want to find out more about exactly where and how they were originally displayed here in Roman times, and how people living in the fort and settlement used rituals such as dedications and offerings.” 

Nigel Mills, heritage advisor to the Hadrian’s Wall Trust, said: “The Roman fort and nearby civilian settlement at Maryport were a significant element of the coastal defenses lining the north western boundary of the Roman Empire for more than 300 years.

“Both the Temples project and the Settlement project show there is huge potential to attract more visitors to the Roman Cumbrian coastal defenses which, along with Hadrian’s Wall, are part of the transnational Frontiers of the Roman Empire World Heritage Site.” 

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maryport2-001

Team at work on the Maryport Roman Temples site. Courtesy Senhouse Museum/ Hadrians Wall Trust

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maryport1-001

Artist’s impression of Maryport Roman Temple. Courtesy Oxford Archaeology Ltd, commissioned by Hadrian’s Wall Trust

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The fort built at Maryport was ordered by Hadrian for construction in the second century AD. It served as the command headquarters and supply base for a series of small forts and towers that extended southward along the west coast from Hadrian’s Wall. The Roman fort and civilian settlement at Maryport are part of the Frontiers of the Roman Empire World Heritage Site, which includes Hadrian’s Wall and its attendant forts. The FRE WHS represents the borderline of the Roman Empire at its furthest extent in the 2nd century AD. It stretched from the west coast of northern Britain, through Europe to the Black Sea, and from there to the Red Sea and across North Africa to the Atlantic coast.

More information about the project, how to participate, and the Senhouse Museum generally can be obtained at their website.

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Additional Information

Tours of the Temples excavation site led by the museum’s volunteer guides start from the museum on weekday afternoons at 2pm and 3.30pm until 18 July. They include entry to the museum and costs are adult £3, child £1, family £8.

Lectures, open days and workshops have also been arranged.

Lectures

  • ·         Thursday 12 June, 7.30pm: The archaeology of drains and cesspits – Don O’Meara. £3
  • ·         Tuesday 1 July, 7.30pm: Interim lecture about the Temples Excavation – Professor Ian Haynes and Tony Wilmott. £3
  • ·         Thursday 17 July, 7.30pm: Final lecture about the Temples Excavation – Professor Ian Haynes and Tony Wilmott. £3

Open days

  • ·         Saturday 21 June, 11am – 5pm: Temples excavation open day. Museum admission applies – adult £3, child £1, family £8
  • ·         Saturday 19 July, 11am – 5pm: Temples excavation open day. Museum admission applies – adult £3, child £1, family £8

Workshops

  • ·         Monday 30 June, 7.30pm: Soils, sediments and landscape – with Don O’Meara. £3 (prebooking essential, limited places)
  • ·         Friday 18 July, 7.30pm: Inorganic material from samples  with Don O’Meara. £3 (prebooking essential, limited places)

The Senhouse Roman Museum is open every day from 10am to 5pm. More information is at www.senhousemuseum.co.uk.

For more information on becoming a volunteer contact Jane Laskey, museum manager.

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discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

Archaeologists Campaign to Save Ancient Maya Sites

As you read this article, a team of archaeologists, students and volunteers are busy methodically digging up ancient structures and artifacts at archaeological sites in Belize with names like Xnoha, Nojol Nah, and Tulix Mul. These sites contain the remains of ancient Maya settlements. The work is carefully planned, slow, and meticulously executed; and like any physical labor in a subtropical environment during the summer months, it can be sweaty, dirty, and tiring. For these students and volunteers, there is no monetary reward for this. They do it because of the excitement of discovery and the new knowledge it will generate about the life-ways of people who are long gone.

But this team is working against time. These sites, especially Nojol Nah, face the real possibility of destruction before the investigators can glean all of the information they need, and conserve what they can find. In the interest of local farming, ranching and economic progress, these cultural treasures may have to take a back seat. It is a story much like many others across Central America, not to mention the rest of the world. 

There is a solution. It has already been realized for a site called Grey Fox, also in Belize and not far from where the archaeological team is now excavating. Under the leadership of Dr. Thomas Guderjan of the Maya Research Program (MRP), a U.S.-based non-profit corporation, archaeologists, preservationists and donors successfully purchased the Grey Fox site and now hope to protect it for future conservation and research. It is also under the MRP that teams are now excavating at Xnoha, Nojol Nah, and Tulix Mul. The MRP, affiliated with the University of Texas at Tyler, has been conducting field operations in northwestern Belize for more than two decades.

“We found the site [Grey Fox] about 14 years ago and mapped it in 2010,” said Dr. Thomas Guderjan, current President of MRP. “It is significant in that it is one of several unlooted sites remaining in northwestern Belize. If we had not purchased it, Grey Fox would surely have been bulldozed within the next 5 years. The land was owned by a group of farmers who were preparing to remove the forest and bulldoze the site.”

Guderjan and colleagues now hope to do the same for the other sites; particularly Nojol Nah, which faces the most acute danger. In partnership with Popular Archaeology Magazine’s Adopt-a Site program, the MRP is getting the word out to potential donors who may be interested in becoming a part of saving this Maya heritage for continuing research, conservation, public education, and tourism. The goal is to purchase approximately 100 acres at a cost of $40,000, an acreage and sum that site investigators believe will secure it for posterity.

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tulixmulpietagreavesPieta Greaves, busy at work on the newly discovered mural at Tulix Mul. Pieta is the Staffordshire Hoard Conservation Project Manager at the Birmingham Museums Trust in the U.K. This mural, now being uncovered, examined and preserved, is one among only a few other known Maya murals found in Central America. Courtesy Maya Research Program

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tulixmulmural2Close-up view of the partially uncovered Tulix Mul mural. Courtesy Maya Research Program

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nojolnaheliteresidenceOverview of the excavated remains of an elite residential structure at Nojol Nah. Courtesy Maya Research Program

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“Now that it is possible to purchase more land,” said Guderjan, “I hope to purchase more properties and open an archaeological reserve.”

For more information about the endangered sites and how to donate, anyone can go to the Adopt-a-Site website and help make a difference.

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discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

The Human Face Evolved from a Violent Past, Say Researchers

scientists have reported a study that suggests that all human males can trace their roots to an ancestor with violent tendencies — a hominin who was not a gentle, ‘noble savage’ whose descendents were later corrupted or changed by the onset of society, as depicted or suggested by many theorists.

University of Utah biologist David Carrier and Michael H. Morgan, a University of Utah physician, have been conducting a comprehensive study of the human fossil record, including that of Australopithecus, an extinct hominin species that is thought to be ancestral to Homo (the human genus of which Homo sapiens, or the modern human, is the soul surviving species). What they have consistently found, among other things, is that certain bones of the face of the male skull have become increasingly more robust over several million years of evolution, and that these bones were critical for protection against impact from objects — like a human fist, which, they maintain, has also evolved over time to form a more effective fist for striking.

“The australopiths were characterized by a suite of traits that may have improved fighting ability, including hand proportions that allow formation of a fist; effectively turning the delicate musculoskeletal system of the hand into a club effective for striking,” said Carrier.  “If indeed the evolution of our hand proportions were associated with selection for fighting behavior you might expect the primary target, the face, to have undergone evolution to better protect it from injury when punched.”

Their study of the bones of the face and cranium supported that hunch.

“When modern humans fight hand-to-hand the face is usually the primary target,” said Carrier. “What we found was that the bones that suffer the highest rates of fracture in fights are the same parts of the skull that exhibited the greatest increase in robusticity during the evolution of basal hominins. These bones are also the parts of the skull that show the greatest difference between males and females in both australopiths and humans. In other words, male and female faces are different because the parts of the skull that break in fights are bigger in males. Importantly, these facial features appear in the fossil record at approximately the same time that our ancestors evolved hand proportions that allow the formation of a fist. Together these observations suggest that many of the facial features that characterize early hominins may have evolved to protect the face from injury during fighting with fists.” 

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violencehumanevolutionUniversity of Utah biologist David Carrier and Michael H. Morgan, a University of Utah physician, contend that human faces — especially those of our australopith ancestors — evolved to minimize injury from punches to the face during fights between males. Their research is published in the June 9 issue of Biological Reviews. Image courtesy University of Utah

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The findings may have important implications for understanding human nature, and will no doubt become part of the general debate about human evolution.

“The debate over whether or not there is a dark side to human nature goes back to the French philosopher Rousseau who argued that before civilization humans were noble savages; that civilization actually corrupted humans and made us more violent,” said Carrier. “This idea remains strong in the social sciences and in recent decades has been supported by a handful of outspoken evolutionary biologists and anthropologists. Many other evolutionary biologists, however, find evidence that our distant past was not peaceful.”

“The hypothesis that our early ancestors were aggressive could be falsified if we found that the anatomical characters that distinguish us from other primates did not improve fighting ability. What our research has been showing is that many of the anatomical characters of great apes and our ancestors, the early hominins (such as bipedal posture, the proportions of our hands and the shape of our faces) do, in fact, improve fighting performance.” 

The theory that humans evolved from a violent ancestor is actually a long-standing and contentious one. It was Raymond Dart, South African anatomist and discoverer of the famous fossilized ‘Taung child’ Australopithecus skull in 1924, who advanced the theory that humans evolved from a “killer ape”, supporting the hypothesis that war and interpersonal aggression was the driving force behind human evolution. The writer Robert Ardrey, author of African Genesis and The Territorial Imperative, further popularized the theory through his books during the 1960’s. But the notion has encountered stiff resistance or dispute among other scholars and anthropologists over the years, whose research has indicated that this is not necessarily the case.  

Carrier and Morgan make it clear, however, that their study results are not about casting humans as a hopelessly violent and destructive species.

“Our research is about peace,” said Morgan. “We seek to explore, understand, and confront humankind’s violent and aggressive tendencies. Peace begins with ourselves and is ultimately achieved through disciplined self-analysis and an understanding of where we’ve come from as a species. Through our research we hope to look [at] ourselves in the mirror and begin the difficult work of changing ourselves for the better.”

Their paper, titled “Protective buttressing of the hominin face,” is published in the journal Biological Reviews.

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Source: Statements by David Carrier and Michael Morgan re-published from a University of Utah press release.

Cover Photo, Top Left: Courtesy University of Utah

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discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

Neolithic Peoples Entered Europe Through Maritime Routes, Says Study

A DNA study suggests that early Neolithic people may have migrated into Europe about 9,000 years ago by island-hopping from Anatolia across the Mediterranean through the Dodecanese islands and Crete and across southern coastal routes.

Preistera Paschou and colleagues came to this conclusion after analyzing single nucleotide polymorphisms from a sample dataset of 32 populations, taken from the islands of Crete and the Dodecanese, Central Anatolia, Greece, Southern and Northern Europe, the Near East, and North Africa. They used a population genetics network approach that thye say determines the pathway of gene flow between populations.

Anthropologists and other scientists studying early Neolithic population migration have proposed three general routes that these early peoples may have taken to enter Europe. One was land-based to North-Eastern Anatolia and then through Bosporus and the Dardanelles and Thrace and into the Balkans; the second was maritime, from the Aegean Anatolian coast and across northern Mediterranean islands and along the coast of Southern Europe; and the third from the Levantine coastline across to the Aegean islands and into Greece. It is the second model that the recent genetic study most supports.

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neolithicexpansionMap of some earlier proposed theories related to Neolithic entry and expansion into Europe.

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“Our data support the Anatolian rather than the Levantine route because they consistently show the Aegean islands to be connected to the Near East through Anatolia,” write Paschou and colleagues in the research report*.

Genetics is not the only evidencial support cited for a maritime model. Archaeology has played its role. “Navigation across the Mediterranean was active during the Early Neolithic and Upper Paleolithic, as illustrated by the finding of obsidian from the island of Milos in Paleolithic sites of the Greek mainland and the early colonization of Sardinia, Corsica, and Cyprus,” add the authors………….”Archaeological evidence from Greek and Near Eastern and Anatolian Neolithic sites suggests that multiple waves of Neolithic migrants reached Greece and Southern Europe. Most likely multiple routes were used in these migrations but, as our data show, the maritime route and island hopping was prominent.”*

The detailed report is published in the Proceedings of the National Academy of Sciences (PNAS).

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*PNAS Article #13-20811: “Maritime route of colonization of Europe,” by Peristera Paschou et al. http://www.pnas.org/cgi/doi/10.1073/pnas.1320811111

Cover Photo, Top Left: Coast of Greece with sunset. Hedwig Storch, Wikimedia Commons

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Read about the most fascinating discoveries with a premium subscription to Popular Archaeology Magazine.  Find out what Popular Archaeology Magazine is all about.  AND MORE:

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discovery2014cover2

Popular Archaeology’s annual Discovery Edition eBook is a selection of the best stories published in Popular Archaeology Magazine in past issues, with an emphasis on some of the most significant, groundbreaking, or fascinating discoveries in the fields of archaeology and paleoanthropology and related fields. At least some of the articles have been updated or revised specifically for the Discovery edition.  We can confidently say that there is no other single issue of an archaeology-related magazine, paper print or online, that contains as much major feature article content as this one. The latest issue, volume 2, has just been released. Go to the Discovery edition page for more information.

 

  





 

 

 

 

 

Archaeologists of Historic Jamestown Release Native American Artifacts for Public View

Archaeologists with the Jamestown Rediscovery Project are now exhibiting a representative sampling of the thousands of Native American artifacts they have uncovered over the past 20 years in or near the site of the 1607 James Fort remains on Jamestown Island, the site of the first successful English colony in North America.

Under the rubric, “The World of Pocahontas Unearthed”, the artifacts can now be seen artfully displayed in their own section within the relatively new Voorhees Archaearium, a large one-story copper-sheathed building that rests on pilings designed to protect the seventeenth century-archaeological features and artifacts that lie beneath. 

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jamestown2View of the Archaearium on Jamestown Island. Ser Amantio di Nicolao, Wikimedia Commons

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“Over the past 20 years we have found thousands and thousands of Virginia Indian artifacts in the excavations………many of them date to the contact period which is, for us, about 1607 to about 1610. So for years, we have had a very elegant museum talking about the English equation or the English side of the story, and clearly there is another half — and that’s the indigenous, the Virginia Indian folks who were here,” says David Givens, a senior staff archaeologist with the Jamestown Rediscovery Project.

Artifacts exhibited include flaked stone projectile points, some of which were made of non-local materials and likely used for cultural exchange, as opposed to hunting and fighting purposes; Indian beads; examples of the 48,000 Indian pottery sherds thus far excavated; clay tobacco pipes that served as models for the English equivalent tobacco pipes; and even one clay pot that features an imprinted pattern of fiber from an Indian basket. 

“So when you come to see the exhibit, you can actually ‘see’ a Virginia Indian basket for the first time in over 400 years,” said Givens.

The James Fort site is unique in that it is considered to contain the richest recovered trove of Virginia Native American artifacts in the Chesapeake region, despite the fact that it is primarily an early English colonial site. This is because centuries of mechanized agriculture have disturbed or destroyed most of the Native American village footprints in the ground, while later colonial structures survived as they were set deeper into the soil than those, for example, of the Powhatan villages in the vicinity of the Jamestown settlement.

The Powhatan was a powerful Native American confederation of tribes in present-day Virginia when the Jamestown settlers first arrived. The confederation was led by Chief Powhatan, who was also referred to as “Emperor”. It is thought that there were possibly about 14,000–21,000 Powhatan people in the eastern part of Virginia in 1607 when the English first established James Fort. It was Chief Powhatan’s daughter, Pocahontas, who saved Captain John Smith’s life and later married colonist John Rolf. She bacame a symbol of the relationship that developed between the English Crown and the Native American people of southeastern Virginia.

“The World of Pocahontas Unearthed” can be seen at the Voorhees Archaearium on the grounds of Jamestown Island, not far from the restored colonial town of Williamsburg, Virginia, another major historical site. See the Jamestown Rediscovery website for more information about this and the ongoing excavations and programs related to James Fort and Jamestown.

Cover Image, Top Left: “The Coronation of Powhatan”, by John Cadsby Chapman, courtesy of the Greenville Museum of Art, Greenville, South Carolina

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The First Arabians

Winter in Saudi Arabia is nearly perfect for archaeological fieldwork—it is neither too hot nor too cold, and it is most always sunny, says Dr. Huw Groucutt, an archaeologist with the University of Oxford. Groucutt has been conducting archaeological research on the Arabian Peninsula for years, along with other senior colleagues such as Prof. Michael Petraglia, also of Oxford University, and Dr. Rémy Crassard, of the Centre National de la Recherche Scientifique (CNRS). They are prominent pioneers in the ongoing research of human prehistory in this region of the world, especially related to Paleolithic times. 

It has been something of an archaeological flurry. In recent years, Groucutt and his colleagues have been discovering sites across the Arabian Peninsula that bear on the entire time spectrum of human prehistory, beginning with the Lower Paleolithic (probably dating to more than one million years ago in some cases). No longer regarded as a cul-de-sac for studies on human evolution and dispersals, the area has quickly emerged as a major theater for exploration and scholarship in the evolving story of early humans and their dispersal across the globe.

Early on, while doing his PhD work, Groucutt began working with Petraglia to research the Arabian Middle Paleolithic in Saudi Arabia. Petraglia had already spent 10 years doing research in the country, and “things were ready for a big expansion in research,” according to Groucutt.

And expand it did.

“Over the last two years we have done two months of fieldwork a year, and the discoveries have been flowing in thick and fast,” he says.

Now with his Ph.D, Groucutt is referring here to the work that is being done in connection with the Palaeodeserts Project. Headed by Petraglia, it organizes the efforts of a multidisciplinary team of researchers to find answers to questions related to the effect environmental change has had on early humans and animals that have passed through and settled this desert subcontinent over the past 1+ million years. Along the way, they have uncovered a profusion of lithic (stone tool) assemblages left by humans at locations in Saudi Arabia. The finds testify to a human presence that dates back hundreds of thousands of years, researchers suggest, marking the trail and habitation zones of humans that followed and exploited green zones created by climatic humid or “wet periods” in an otherwise harsh, arid Arabian palaeoenvironmental history. Focusing for the purposes of this article on the mid-to-late Paleolithic period, the research could have profound implications in the debate on early human dispersal theories out of Africa, particularly those related to anatomically modern humans (AMH), and it is already making its mark in the scholarly world of human prehistory studies. 

The recent study reports on the topic have been pored over by scientists and academes alike. But they contain terms, concepts, and process descriptions that are familiar only to them. To elucidate the picture for a general readership in detail, Popular Archaeology interviewed Groucutt and Crassard, with additional input from Dr. Ash Parton, specialist on palaeoenvironmental change for the Palaeodeserts project. What follows is what they had to say:  

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Q: What have been the most significant Middle Paleolithic finds on the Arabian Peninsula that bear on the presence of anatomically modern human hunter-gatherers there?

Crassard:

To date, there has been no trace of fossilized hominin prior to the Holocene on the Arabian Peninsula. It is thus difficult to affirm with no doubt that AMHs (Anatomically Modern Humans) were present in Arabia during the Middle Paleolithic. This means that Neanderthals could have been there as well, as suggested in a paper we did on a site excavated in Yemen (Delagnes et al. JHE 2012: “Whether or not the Middle Paleolithic occupation of Wadi Surdud can be attributed to modern humans or to a human group related to the Neanderthals remains a totally open question. As no sound technological markers exist for distinguishing Neanderthals from early modern humans, neither of these alternatives can be ruled out”).

The stratified and thus dated sites are still very rare in the whole Peninsula for the Paleolithic period (most identified sites are surface scatters), and the only available data consists of stone tools. There is no evidence of symbolic activity, nor a robust faunal record, so the subsistence strategies are also unknown. One possibility for testing hypotheses relating to identifying the kinds of human species in Arabia during the Middle Paleolithic is to compare stone tools. Among several types of stone tools, bifacial tools, or hand axes, have been found at Jebel Faya in the United Arab Emirates, and they have been considered as a AMH production, dated to about 125,000 years. This interpretation is not always accepted by the scientific community, as they could have been produced by other human antecessors.

Another type of stone technology is interesting for tracing the demographic expansion of Homo sapiens. This is the Nubian technology. This kind of predetermined flake production on stone (chert, flint, quartzite…) was previously known only in northeastern Africa, until it was found in south Arabia (especially in the region of Dhofar (see Rose et al. Plos One 2011), in Oman, but also in Hadramawt in Yemen), and more recently in central Saudi Arabia, close to the modern city of Al-Kharj (Crassard & Hilbert, Plos One 2013). This technology is dated to more than 100,000 years in Arabia, a technology that seems to have only otherwise been produced by AMHs in Africa. Further research is needed, including new dates and stratified sites, to confirm these interpretations. 

Groucutt

Firstly, we must emphasize that interpretive caution is needed as no hominin fossils are known from before the Holocene (i.e. the last 12,000 years) in Arabia. So we are talking exclusively about lithic (‘stone tool’) technologies. Variation in lithic technologies reflects many factors, such as the influences of different types of raw materials (chert, quartzite, quartz, volcanic raw materials, etc.) used and other such ‘pragmatic’ factors, as well as the role ‘cultural’ variation may have played. Variants of Middle Palaeolithic technology are complicated and sophisticated, showing patterning in space and time. Such factors are important indications that we are dealing with learned (i.e. cultural) behaviors. As a result we should be able to look at how lithic technology varies in space and time and understand how populations moved through the landscape (i.e. dispersals) and how they responded to changes in their environment.

With that background, three major finds/groups of finds in Arabia have been argued to relate to the dispersal of anatomically modern humans (AMH). The first, published by Professor Simon Armitage, et al. (2011), in the journal Science, relates to the Jebel Faya rockshelter in the United Arab Emirates. This was the first site in Arabia for which absolute age estimates were published (using a technique called Optically Stimulated Luminescence or OSL dating, which allows us to date sites which are beyond the limits of radiocarbon dating). The excavators at Jebel Faya recovered several buried assemblages of lithics. They argue that the younger ones are unique and so represent a local population, perhaps isolated in this region. Attention has focused on the deeper (older) assemblage (‘Assemblage C’) which appears to have been been buried ~125 thousand years ago (the ‘Last Interglacial’). The discoverers argue that features of this assemblage demonstrate similarities to African ‘Middle Stone Age’ sites associated with early AMH. This is based on the combination of tool types found at the site – Levallois cores and flakes (flakes struck from specially prepared nodules of rock (cores) which result in flakes of a particular, predetermined shape), blades (long, thin flakes) and bifacial tools. Not much information has been published on the lithics yet, so it is difficult for other scholars to critically examine these claims. But arguably caution is needed and the position of Jebel Faya is still very much open to debate. For example, the discoverers reject connections with areas of the Levant as these are suggested to lack the tool types found at Jebel Faya. Yet sites such as Skhul in modern day Israel have bifaces, Levallois technology and blades.

The second major claim from Arabia comes from the discovery of a large number of archaeological sites which the discoverers describe as belonging to the ‘Nubian Complex’. Most of the sites in Arabia, published by Dr Jeff Rose and his colleagues, are in the Dhofar region of Oman, but before that similar technology had been found at lower frequencies in Yemen by Dr Rémy Crassard and others. More recently Dr Crassard and others have also found Nubian technology at Al Kharj in central Saudi Arabia. Nubian Levallois technology is a particular form of Levallois technology, where nodules of rock (‘cores’) are specially shaped. In this variant they are shaped in a way which produces pointed flakes (‘Levallois points’). Nubian technology was previously best known from northeast Africa (‘Nubia’), so a lot of people are very excited about its discovery in Arabia, seeing it as strong evidence that populations of AMH dispersed into Arabia more than 100 thousand years ago. This is again possible, but there have not yet been many detailed comparative studies. And with different types of Levallois technology we must always be wary of technologies being re-invented. Nubian or analogous technology is in fact known from Mauritania to India, and from central Saudi Arabia to Kenya. The presence of Nubian Levallois technology in Arabia is important, but it is not necessarily a smoking gun for dispersal out of Africa.

Finally, we on the Palaeodeserts Project (based at the University of Oxford but with collaborators at various international institutions), working in collaboration with the Saudi Commission for Tourism and Antiquities, have made a number of discoveries in Saudi Arabia. A basic point which must be made is that to understand movements out of Africa, we need to look at areas close to Africa. Jebel Faya, for instance, is about 2,000 km from Africa. Palaeodeserts Project fieldwork has identified dozens of new Middle Palaeolithic sites in Arabia, mostly associated with either ancient lakes and rivers, and/or with sources of raw material suitable for making lithics. We have worked in the Nefud desert of northern Arabia, central Arabia and southwestern Saudi Arabia. In these areas we have found Middle Palaeolithic sites of many ages and varieties. We are currently analyzing these discoveries and conducting laboratory assessments of sediments to understand the age of the sites and the nature of the environments, when occupied. What we are finding is that a lot of the sites date to what is called Marine Isotope Stage (MIS) 5, a climatic period which dates from around 130 to 75 thousand years ago. This time saw several periods of much warmer climate, which led to wetter conditions in Arabia. Lots of these MIS 5 sites share similar technology, particularly centripetal Levallois cores, which are flaked in a radial fashion around the edges of the core producing large numbers of flakes of predetermined shape. This is the standard way of producing flakes for much of the African Middle Stone Age, unlike more specific forms such as Nubian Levallois technology. We are also finding some particular tool types such as retouched points. These kinds of toolkits, both in terms of ‘core reduction strategies’ (types of Levallois technology) and of the tools then made are found in Africa for a long period associated with AMH, in the Levant with the earliest known AMH outside Africa (e.g. Skhul, Qafzeh) and at sites in India dating to more than 75 thousand years ago.

So what we really need to understand about the movement of AMH into Arabia is the demonstration of similarities with multiple constellations of technological features, not one feature or one tool type. Conclusions will be much more robust when this is done (we are currently doing this). But history shows that caution is needed. For example, a single site in Saudi Arabia had been suggested to share similarities with the ‘Aterian’ industry of North Africa (again MIS 5, and associated with AMH). A detailed reanalysis of the material by Dr. Eleanor Scerri (currently Université de Bordeaux and University of Oxford) however strongly suggested that the undated Saudi assemblage did not relate to the Aterian at all, but was a more-or-less similar form of technology that had been reinvented there in the last few thousand years. We think such findings are very important when making major claims based only on one aspect of technology. So aside from trying to identify repeated constellations of features it is also critical to have sites which are from secure contexts so that they can be dated. This is what the scientists with Palaeodeserts are doing at several sites in interior Saudi Arabia.

Finally, we must note that other claims for the dispersal of AMH out of Africa, such as the view of Professor Sir Paul Mellars that there was a single dispersal, around 60-50 ka, along the coastline out of Africa and around Arabia apparently associated with small and finely shaped ‘geometric microliths’, is not supported by any evidence in Arabia. Mellars’ model may indeed be true, and he has published his ideas in a number of the leading journals of the world, and he points to a rise in sea levels which would have covered the route taken by the earliest successful (i.e. ancestors of today, not dead-end populations) AMH to leave Africa. This is possible, but in many areas of southern Arabia there is a very steep coastal shelf so changing sea level hasn’t changed that much. Also in some areas tectonic uplift means that we have preserved sections of coastline. Given that extensive surveys have been conducted along the southern Arabian coastline, which have failed to produce any evidence at all for the kind of evidence predicted by Mellars’ model, we think this single dispersal model unlikely for now. 

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View of area being surveyed for archaeological sites in the western part of the Nefud desert. (credit: Eleanor Scerri/Palaeodeserts Project)

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Dr Huw Groucutt (University of Oxford) systematically collecting a dense scatter of artifacts on the shore of an ancient lake dating to around 85,000 years ago at Mundafan, southwestern Saudi Arabia. (credit: Richard Jennings/Palaeodeserts Project)

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 Excavation of a Middle Palaeolithic site at Jubbah (credit: Richard Jennings/Palaeodeserts Project)

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Q: What possible implications do the finds have within the context of current theories about the dispersal of anatomically modern humans out of Africa?

Crassard:

Arabia is regularly seen as a periphery to Africa. And this is logical, as it is the closest subcontinent to the region of emergence of the first AMHs. But the question of how this dispersal out of Africa was accomplished is really central to current debates. Two main hypotheses are being tested today through a very active (that is recent) research in Arabia: the coastal dispersal and the more inland, perhaps more complex dispersal into and within Arabia.

The international teams working today on these questions are placing a lot of emphasis on the relationship between human groups and climate evolution, as well as topography of the environment in general. Genetics studies are also important in these debates, as molecular geneticists have suggested that human populations have rapidly migrated to the East along the Indian Ocean coasts about 65,000 years ago; but recent discoveries may demonstrate a much earlier dispersal of AMH, or Homo sapiens.

The first results from the Jubbah and Mundafan paleolakes research (international team lead by Michael Petraglia (University of Oxford)) are very promising, as well as the research conducted along the Red Sea coasts by another international project lead by Geoff Bailey (University of York) and Geoffrey King (Institut de Physique du Globe, Paris). The Green Arabia conference, recently held in Oxford and organized by the Palaeodeserts team, featured presentations that very accurately elaborated on the state of the art relating to the actual debates in the region.

As mentioned before, the Nubian technology is an important discovery that needs more dating and more stratified sites; but the comparison with a very peculiar technology that was only known in Africa can really add a lot to this debate. This will be investigated by several teams working in Saudi Arabia (including my work and colleagues) and Oman (including the work of Jeffrey Rose and colleagues).

Groucutt:

As I mentioned, there are several theories about the dispersal of AMH out of Africa, and this in fact is one of the most exciting areas of research in hominin evolutionary studies. The differences between the theories concern a number of factors such as the causes of dispersal, the timing, the routes taken and the number of dispersals.

These different theories for dispersal out of Africa can be divided in many ways. There is a major split between those who think that dispersal at least began during the wetter climatic conditions of MIS 5, when either side of the Red Sea was a broadly similar environment, and those who think that successful dispersals out of Africa only occurred after MIS 5, around 60-50 thousand years ago. Within these different models, many different variants have been published and discussed. Aside from debates about the onset of dispersal, there are debates between those who think there were multiple dispersals out of Africa (a theory that seems likely me to) and those who argue there was only ever a single dispersal (based on some genetics ‘story telling’, discussed more below).

Each of these theories cites combined evidence from several disciplines (e.g. archaeology, the study of human fossils, genetic variability). Outside the small area of the Levant very little is known about archaeology in Asia before about 40 ka, with few well excavated and dated sites. Likewise, outside the Levant there are very few fossils of early modern humans. This may be because they were not there, but perhaps equally as likely it is just about limited research and poor preservation in some areas. As a result of these historical weaknesses in the archaeological and fossil record, patterns of genetic variability have become very important. And it can be argued that many theories really hang on the genetics, backfitting other evidence to this. Traditionally most genetic studies looked at ‘single loci’ such as mitochondrial DNA or the Y chromosome. These give useful information, but only reflect a very small component of our genetic makeup and are prone to over-interpretation. More recent studies looking at complete genomes are changing the picture and suggesting that genetic evidence is congruent with an earlier onset to dispersal than had been suggested by the single locus studies.

So what we are doing in Arabia is really testing these different models on the ground, and calling for scholars to keep an open mind on what is being found. Fossils would be great, but have so far been elusive. But we have found a very well preserved site in northern Saudi Arabia with lots of animal fossils. The fact that small animal bones, dating back hundreds of thousands of years, have been identified, clearly suggests that there is the great potential for hominin fossil material to be discovered. Great surprises may be in store. For instance, the discovery of a Neanderthal fossil in southern Arabia would be a remarkable finding. Likewise, we predict the discovery of AMH fossils in Arabia dating to MIS 5. This would show that these populations did not just expand into the Levant at this time (where according to scholars like Mellars they survived for a ‘brief’ few tens of thousands of years and then died out), but actually expanded an unknown distance into southern Asia. These small initial populations were then joined by further, later dispersals.

We think it is significant that virtually every archaeological team working on Middle Palaeolithic sites in Arabia supports an early onset to the dispersal of AMH out of Africa. This is in stark contrast to the views of other scholars who argue for a later AMH dispersal based solely on literature reviews. Different teams working in Arabia emphasize different sites and different forms of technology, but most are agreed that we are talking about dispersals starting in MIS 5 with Middle Palaeolithic technology and moving primarily by interior rather than coastal routes. Every new site being discovered in Arabia reveals remarkable new information which makes it a very exciting time to be working in the area. We are confident that over the next ten years we will make some major discoveries. We are also keen to see archaeological data emphasized when it seems that many archaeologists have been living in the shadow of genetics interpretations over recent years. Yet archaeological data is the only record of how humans were behaving in particular times and places, so we are trying to restore the balance to the subjects contributing to the story of modern human origins.

Q: What in your mind are the most important finds that suggest possible links to lithic technologies in Africa? 

Crassard:

As I mentioned before, this would definitely be the presence of the Nubian technology in Arabia, previously known only in northeastern Africa. This method of flint knapping, which archaeologists can understand through a rigorous use of technological and taxonomic analysis, is part of the greater family of the ‘Levallois’ concept known in many parts of the prehistoric Old World. The Nubian technology entails producing flakes with a predetermined shape, most of the time triangular. This discovery, finding such a technology in Arabia, thus has important implications related to questions of human dispersal and influences between Africa and Arabia. For reference, I co-authored a paper about this technology as it was discovered at the Al-Kharj site in Saudi Arabia, published in PLOS ONE in July of 2013*.

Groucutt: 

Again, we need to be cautious about linking individual types of technology when attempting to make the case about similarities with Africa. Our starting point should be rooted in biogeography. For example, we now know that in periods such as MIS 5 there were similar savannah environments on either side of the Red Sea, both dotted with lakes and rivers. AMH would therefore not have had to cross a significantly different ecological zone to disperse into Arabia, whilst Neanderthals to the north would have had to do so. This does not mean that it is impossible that Neanderthals were in Arabia, and indeed it is an exciting possibility that Arabia may have been an important frontier for archaic and modern human interactions.

So the point is that lithic similarities are more likely to be real when there are other reasons to think that similarity due to descent (‘homology’) is more likely than similarity due to convergent, independent evolution (‘analogy’). Middle Palaeolithic technology was sophisticated, but its users picked major characteristics from a relatively limited number of options. There are several reasons why we might think that particular forms would be re-invented. So we need to be careful. If we can demonstrate several, independent, measures of similarity between assemblages in Arabia and Africa which date to similar times then we think this provides good evidence for population connections. We do not think that there is a single ‘smoking gun’ which proves the ‘exodus’ out of Africa. We are using various techniques to understand lithic variability, particularly the development of multivariate statistical techniques rather than traditional typological approaches.

These factors said, we find it provocative that we are finding both similar core reduction strategies (particular methods of removing sharp flakes of rock from nodules of rock) and tools which were then made at several sites in interior Arabia, with areas such as East Africa, the possible homeland of Homo sapiens according to many specialists. We think that the discovery of several sites in the interior of Arabia with centripetal Levallois technology is very important, and as mentioned above its similarities with assemblages in Africa (where this kind of technology is found first, more than 200 thousand years ago), the Levant (around 120-80 thousand years ago) and India (around 80 thousand years ago) are something we think very significant. It is also key that similar technology was being used in different ecological zones, with different raw materials etc. This removes some of the ‘pragmatic’ factors, which can make lithics look similar or different, and suggests cultural connections.

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Figure 11

Distribution of main sites with Nubian cores in Eastern Africa and Arabian Peninsula. Illustrated cores do not represent actual size. 1. Al-Kharj 22; 2. Aybut Al Auwal; 3. Shabwa; 4. Hadramawt; 5. Aduma; 6. Gademotta; 7. Asfet; 8. Nazlet Khater 1; 9. Abydos. doi:10.1371/journal.pone.0069221.g011*

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Figure 6

 

Nubian preferential Levallois cores from Al-Kharj 22. Drawings by G. Devilder, CNRS. doi:10.1371/journal.pone.0069221.g006*

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An example of a Levallois core from southern Arabia. Note the large flake scar which has been shaped in a specific manner by preparatory flaking of the margins. (credit: Huw Groucutt)

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Q: What is the latest assessment based on the most recent evidence of the environment that existed during Middle Paleolithic times in parts of the Arabian Peninsula, specifically focusing on those areas that were suggested to be friendly to human habitation?

Crassard:

Several international teams are now working in the Arabian Peninsula, and environmental studies are key in understanding how and when it was more viable for human groups to colonize (and stay in) Arabia. These studies need to be combined with archaeological findings and genetics studies. It has been hypothesized from the first studies that human groups could have migrated to Arabia only during ‘windows of opportunity’, meaning only when climate was more humid, allowing better access to food (fauna and plants) and water (drinking water from springs, water resources and biotopes from lakes, for example). But new data gathered now suggest a more complex situation in Arabia, as a succession of contraction and expansion of population may have occurred, sometimes in direct relation to humidity increasing or decreasing, though not necessarily, as human groups could have gathered together in refugia at specific periods of time.  It is nevertheless very difficult to consider Arabia as a single region that would develop in a homogeneous way: Arabia is very diverse, topographically and in term of climates, even today. Palaeoenvironmental studies need to take this factor into account and need to focus more and more on regional and local studies, rather than on global studies considering Arabia as a whole.

Ash Parton (specialist on palaeoenvironmental change for the Palaeodeserts project):

The expansion of Middle Palaeolithic communities across Arabia is intrinsically linked to periods of increased rainfall when the land became green. In the present day, monsoon rains only reach the very south-southwestern edges of the peninsula; however, palaeoclimatic evidence suggests that over the past 130,000 years there have been several periods in which these rains extended all the way into the desert interior. Utilizing a technique that allows researchers to know when individual grains of sand were buried (optically stimulated luminescence dating), findings suggest that the ‘greening of Arabia’ occurred approximately every 22,000 years between around 130,000 and 50,000 years ago. During these times drainage systems became active, leading to the expansion of large meandering rivers and the development of vast freshwater lakes, some of which were up to 2000 km². Palaeoenvironmental evidence from relict lake beds in what are now the hyper-arid Nefud and Rub al Khali deserts of Saudi Arabia, also shows that these large lakes were fringed with grasslands and trees, and home to a wide variety of fauna. Additionally, advanced mapping techniques using satellite data in conjunction with ground-based landscape studies indicate that alongside the larger lakes were many, possibly thousands, of smaller water bodies. This dramatically different landscape would have proved critical to the early peopling of Arabia, and instrumental in determining the development of our species.

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firstarabians2

Sediments at the Jubbah site show environmental change through time. Young orange sand on the surface, white sediments represent a phase of lake formation around 125,000 years ago, the fine sands below this date to more than 200,000 thousand years ago and contain the oldest identified Middle Palaeolithic artifacts in Arabia. (credit: Huw Groucutt/Palaeodeserts Project)

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firstarabians3

Dr. Tom White (University of Oxford) samples ancient lake sediments dating to around 100 thousand years ago for molluscs and other indicators of ancient environmental conditions. (credit: Richard Jennings/Palaeodeserts Project)

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Q: What have been the challenges of doing work in those key areas of investigation?  

Crassard:

Challenges in the area were clearly linked to the lack of research in the last decades, comparing with better-known regions such as the Near East or Europe. It was always difficult at the beginning of my research to face with the lack of interest of some colleagues, sometimes seeing Arabia as a ‘cul-de-sac’ (where nothing could have really happened…). I am happy to see that this vision has totally changed today and that many teams are now working in the region which progressively became one of the ‘hot spots’ in the world for prehistoric research today. Other challenges are also due to the political instability of the region, as for example in Yemen that is today a difficult place to work in. I am though very optimistic for the future of Arabia, and it is now a great opportunity for international teams to work in close cooperation with local and professional teams.

Groucutt:

We have found Saudi Arabia to be an extremely welcoming country, and the Saudi Commission for Tourism and Antiquities have helped massively with our collaborative field efforts. Weather in the winter in Saudi Arabia has generally been close to optimum for fieldwork, not too hot or cold and generally sunny. Saying that, on occasion it has become extremely hot, making excavations difficult. Likewise, during times when the wind picks up, one is blasted by stinging sand which finds its way into any gap that is not covered. Driving poses a challenge in remote areas, and we travel in convoys of four-wheel drive vehicles. The Saudis are excellent off-road drivers, but we have had a few incidents of getting stuck in vast sand dunes! Some of the sites are very remote, so a lot of driving is involved.

Because Arabia is so unknown, the biggest challenge has been the lack of reference points. We are largely discovering things from scratch. This has been a challenge, but also allows us to approach the fieldwork with an open mind and not focus on one particular type of site. The academic freedom of working in such a poorly understood area is extremely liberating. When we find a site it is very exciting as whatever age it turns out to be is still an important discovery, unlike better-known areas where only finds of particular time periods are of much importance, as many sites are already known. So the lack of knowledge on Arabia is both a challenge and an opportunity.

Q: What is the focus of future efforts? 

Crassard: 

Future efforts are focused on the finding of more stratified sites. Most of the artifacts have been found on the surface, presenting difficulties in dating, and thus limiting our understanding of critical aspects such as chronology, dispersals, migration routes, and human species. The finding of human fossils is also a goal for every team working in Arabia, and this will definitely be a huge discovery. Multidisciplinary research is really the key to future work in Arabia and the teams working there have understood this. Arabia is today a fantastic laboratory to develop research on human origins — not only on its characteristics, but also in developing new methodologies (modeling, dating, surveying). We are experimenting in a very important moment in the development of prehistoric research in Arabia, and I hope this will continue in an exponential way.

Groucutt:

In terms of future archaeological fieldwork, a key aim is to increase the number of excavated and dated sites so that we can robustly compare findings. As almost every new site (or group of sites) reveals a different form of technology, often using different raw materials and dating to a different time, we still have a lot left to work out. The record seems to indicate repeated dispersals into Arabia, followed by local adaptation. In that sense researchers need to stop treating Arabia as just a passive receiver of dispersals from outside, or as a route to somewhere else, and see it as an area with its own complicated history.  Aside from the general ‘more digs, more dates’ aim, two key areas we in the Palaeodeserts project are working on are 1) developing landscape perspectives, i.e. not just looking at single sites, but trying to understand how hominins used and moved around landscapes, and 2) developing and applying multiple new techniques of lithic analysis, from biochemical analysis of residues found on lithics which can tell us what they were used for, through to sophisticated multivariate statistical approaches to objectively understand similarities and differences.

In environmental terms we are trying to understand more nuanced and sensitive archives. Much of the traditional picture of ancient climate change in Arabia has been built on speleothems (e.g. stalactites, etc.). These are important, but their formation tends to only reflect the very wettest times. We are studying records such as lake sediment records and alluvial fans, as these are more sensitive indicators of environmental and landscape change. Through these we are trying to move beyond simply saying Arabia was either ‘wet’ or ‘dry’. We are also working on developing our understanding of palaeoecology. For instance, another postdoc at Oxford working on the Palaeodeserts Project, Dr. Tom White, is an expert on ancient molluscs. These can provide very interesting information on the characteristics of ancient lakes (i.e. how salty the water was) and nuances such as the level of seasonality. This kind of information is much more valuable than simple dichotomies of wet and dry, and allows us to understand environmental variability at a scale closer to that of human lives.

Finally, the hunt for fossils of early humans continues. Arabia is full of ancient lake beds, caves and other places where fossil material can be preserved. I am confident that human fossils will be found in Arabia. It is just a matter of where and when.

 

About the Scientists

Rémy Crassard

crassard2

Rémy’s personal route to Arabia is due to a first experience in Oman in 1998, when he was a student of anthropology at La Sorbonne University in Paris. He discovered a region of the world that was totally unknown to him, as his original aim was to specialize in Mesoamerican archaeology. Gradually, through many meetings with researchers and scholars, he had the opportunity to work in Yemen where it was already difficult to go. After several experiences both in Europe and Arabia, he spent three years in Yemen to do PhD research and in the process became a specialist of the region. As his PhD was focused on doing a ‘panorama’ of the prehistory of Yemen, from the origins to the last productions of stone tools (at the beginning of the Common Era), he became involved in many international projects dealing with all kinds of artefacts and periods. Today, he finds himself in many places within the Arabian Peninsula, with the goal of developing his research through at least two very different perspectives: the Middle Paleolithic and the origins of the peopling by AMHs, and the rise of the Neolithic in Arabia and its specificities: Arabia being closed to ‘core areas’ of the Neolithic such as the Levant, although apparently developing in an isolated way. “I am very excited about the actual development of archaeological research in the Arabian Peninsula,” he says, “as researchers around the world have recently recognized the importance of Arabia that was for so many years an empty spot on the global archaeological map.” Rémy is considered a leading authority on the study of lithic industries of the Palaeolithic and Neolithic periods in the Arabian Peninsula and has co-authored major research papers related to the subject. (Photo courtesy Rémy Crassard and the Palaeodeserts Project)

Huw Groucutt

huw

While acquiring his Masters degree, Huw began to recognize that Arabia represented a large gap in scholarly understanding of the human prehistoric past. There was a prolific amount of research happening in areas at the edge of the Pleistocene world (South Africa, Europe) and small areas (the Levant), yet vast and central areas such as Arabia were all but unknown. He contacted Professor Michael Petraglia to determine if he would be interested in supervising his PhD research on the Arabian Middle Palaeolithic. He was very keen and we soon got to work. Mike had been working in Saudi Arabia for about ten years and all indications were that the region was ready for a major expansion in research. “When I started my PhD in 2009, not a single Middle Palaeolithic site in Arabia was dated,” says Groucutt. “That picture is rapidly changing. Mike and I and various collaborators started to do increasingly long field seasons in Saudi Arabia. I completed my PhD and Mike was awarded a large grant by the European Research Council for what is called the ‘Palaeodeserts’ project, which is run by Mike.” Huw has co-authored a number of recent research papers related to his work in Arabia and will continue to be a major player in developments in this area for years to come. (Photo courtesy Palaeodeserts Project)

Ash Parton

parton

Dr. Ash Parton, of the University of Oxford, is a specialist on palaeoenvironmental change for the Palaeodeserts project.  He focuses on researching the palaeoclimatic and palaeoenvironmental changes in Arabia throughout the Late Quaternary. In particular, his research investigates the nature and timing of humid phases from Marine Isotope Stage 7 to 3, through the development of geomatic and multiproxy palaeoenvironmental records.

The broader aim of this research is to establish how incursions of monsoon rainfall into Arabia facilitated the dispersal of hominin populations. (Photo courtesy Palaeodeserts Project)

 

Michael Petraglia

petraglia

Although not interviewed for this article, Michael Petraglia heads the Palaeodeserts Project. He is Professor of Human Evolution and Prehistory, Senior Research Fellow and the Co-Director of the Centre for Asian Archaeology, Art & Culture, School of Archaeology, University of Oxford. He is also a Senior Research Fellow, Linacre College (Oxford), and a member of the Human Origins Program, Smithsonian Institution, Washington, D.C.

His research work includes modern human origins, palaeolithic archaeology, lithic technology, evolution of cognition and out of Africa dispersals. His primary regions of research are the Arabian Peninsula, the Indian subcontinent and Eastern North America.

A special thanks goes to him for facilitating these interviews and directing the author to key resources related to the fieldwork being conducted on the Arabian Peninsula. (Photo courtesy Palaeodeserts Project)

(Did you like this article? Read more like it with a premium subscription to Popular Archaeology.)

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*Crassard R, Hilbert YH (2013) A Nubian Complex Site from Central Arabia: Implications for Levallois Taxonomy and Human Dispersals during the Upper Pleistocene. PLoS ONE 8(7): e69221. doi:10.1371/journal.pone.0069221

Other source documents for information about the research include:

Petraglia MD, Alsharekh A, Breeze P, Clarkson C, Crassard R, et al. (2012) Hominin Dispersal into the Nefud Desert and Middle Palaeolithic Settlement along the Jubbah Palaeolake, Northern Arabia. PLoS ONE 7(11): e49840. doi:10.1371/journal.pone.0049840 

Crassard R, Petraglia MD, Drake NA, Breeze P, Gratuze B, et al. (2013) Middle Palaeolithic and Neolithic Occupations around Mundafan Palaeolake, Saudi Arabia: Implications for Climate Change and Human Dispersals. PLoS ONE 8(7): e69665. doi:10.1371/journal.pone.0069665

Groucutt, Huw S., Petraglia, Michael D., The Prehistory of the Arabian Peninsula: Deserts, Dispersals, and Demography, Evolutionary Anthropology 21: 113-125 (2012)

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The Early Humans of Cueva Negra

Cueva Negra is 10 km south of Caravaca de la Cruz, lying at 740 m a.s.l. (metres above sea level) and 40 m above the R. Quípar where it flows northwards out of a gorge (“Estrecho”) below the hamlet of La Encarnación (Fig.1). The large rock-shelter contains a noteworthy depth of Pleistocene sediments cursorily explored in 1981 (Martínez-Andreu et al., 1989). It lies in Upper Miocene (Tortonian) sedimentary “biocalcarenite”1 rock on the right-hand side of the narrow gorge through which the R. Quípar Gorge descends before joining the R. Segura, which reaches the Mediterranean Sea 110 km east of the site that nevertheless is but 75 km north of the southern Murcian coast. Systematic excavation began in 1990 and 25 field seasons have taken place. For some years neither the chronology nor the complexity of the Pleistocene geology were understood correctly. Inaccuracies and mistaken interpretations in earlier publications were corrected in the 2013 revision (Walker et al., 2013) that supersedes them all, and significant aspects of it are summarized here (earlier publications cited here are preceded by ! indicating they contain some unreliable information, usually a chronological attribution that is too young, sometimes incorrect faunal assignation, or occasionally a geological error).  

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cuevanegra1Fig. 1: Cueva Negra and its surroundings

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The 5-m-deep Pleistocene sedimentary fill (Fig.2) is assigned by magnetostratigraphy2 to the Matuyama magnetochron2 >0.78 Ma (Scott and Gibert, 2009). Optically-stimulated sediment luminescence3 implies >0.5 Ma and mammalian biochronology indicates >0.7<1 Ma (Walker et al., 2013): e.g., extinct forms of Arvicolid rodents – i.e. voles, field-mice, water-rats, etc. – which became extinct around 0.7 Ma, such as Mimomys savini, Microtus (Iberomys/Terricola/Pitymys) huescarensis huescarensis, Pliomys episcopalism, Allophaiomys (Microtus/Euphaiomys) cf. chalinei, Stenocranius (Microtus) gregaloides; as well as extinct large mammals, among them the extinct Cervids Megaloceros aff. savini (a giant deer) and Dama cf. nestii vallonnetensis (an ancestral form of fallow deer); the extinct Rhinocerotid (i.e. rhino) Stephanorhinus cf. etruscus; the Equid Equus altidens (an extinct horse), etc.: all of them are well-known Pleistocene time-markers of mammalian evolution in western Europe. Sediment micromorphology4 shows the fill represents near-horizontal, gradual, intermittent fluviatile accumulation4 (Angelucci et al., 2013) with no significant horizontal or vertical discontinuities (pace Jiménez-Arias et al., 2011). Mammals, birds (including waterfowl), reptiles and amphibians corroborate pollen (! Carrión et al., 2003) typical of mild (MIS-21?5), damp, fluvio-lacustrine4 environments. Anne Eastham identified more than 60 bird species (! Walker et al., 1998) implying nearby biotopes6 of (1) lakes and rivers with temperate woodland, (2) open mixed woodland, (3) open grassland and heath, and (4) craggy mountainsides. That suggests the site was frequented owing to its well-favoured position in its surroundings with noteworthy biodiversity, though it may have been taken over by birds whenever flooding required mammals to abandon the cave, perhaps seasonally.

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cuevanegra2Fig. 2: Cueva Negra Plan and sections

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Cueva Negra “pre-Neanderthal” (Homo cf. heidelbergensis) teeth (Fig.3) give several measurements (Table 1) out with modern ranges; e.g. large antero-posterior measurement at the neck, or cervix, between crown and root (cervical vestibulo- or bucco-lingual dimension), typical in Neanderthals and archaic humans and often interpreted as a “buttressing” adaptation to using front teeth as a vise. Extreme tooth wear (attrition) of Cueva Negra front teeth, exposing dentine and the pulp- or root canal (rendering lingual crown height unreliable and uninformative) is also typical of Neanderthals and archaic humans, perhaps caused by using front teeth as a vise; in modern humans tooth wear and exposure of dentine occurs mostly on crowns of back teeth, only rarely on front teeth. One incisor tooth crown has a “shovel” form (a broad vertical scoop) on its internal (lingual) surface; “shoveling” is common on Neanderthal incisors. A canine tooth with occlusal attrition that exposed the pulp canal has a root that is much longer than in modern humans though comparable in length with some Neanderthal canines (e.g. from Grotte d’Hortus).

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cuevanegra3Fig. 3: Cueva Negra with hand-axe and teeth

 

Table 1

Cueva Negra fossil human teeth by type, metre-square, layer and spit (right), and measurements taken (below)

 

Left mandibular

permanent

lateral

incisor 

B1i (1)

left maxillary permanent lateral incisor

B2f (1-2)

left maxillary

permanent

canine

C3e(2c)

right

mandibular

permanent

anterior

premolar

C2e(3ñ)

Right

maxillary

permanent

anterior

premolar

C1a (1-2)

Anterior permanent

tooth root C4g(2c)

incisoapical height

23.0 mm

25.2 mm

27.2 mm

21.9 mm

22.9 mm

no crown

mesiodistal crown dimensión

 5.7 mm

 7.6 mm

 7.0 mm

11.8 mm

  6.2 mm

no crown

buccolingual crown dimensión

 7.9 mm

 9.6 mm

 7.8 mm

 8.0 mm

  7.6 mm

no crown

buccal crown height

 7.7 mm

 9.6 mm

 8.2 mm

 9.4 mm

10.4 mm

no crown

lingual crown height

 6.1 mm

 unreliable

unreliable

unreliable

Unreliable

no crown

buccal height of root

15.3 mm

 7.9 mm

19.0 mm

14.3 mm

14.6 mm

 22.5 mm

mesiodistal dimension at neck

 5.4 mm

 5.8 mm

 6.5 mm

 4.6 mm

  5.5 mm

  7.3 mm

buccolingual dimension at neck

 

 7.7 mm

 7.8 mm

 8.0 mm

 7.7 mm

  7.0 mm

  8.1 mm

maximal mesiodistal dimension of root

 5.0 mm

 5.3 mm

 5.3 mm

 3.7 mm

  5.0 mm

  5.5 mm

maximal buccolingual dimension of root

 8.3 mm

 8.7 mm

 8.0 mm

 6.5 mm

  6.9 mm

  7.6 mm

        Table 1

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The most important findings at Cueva Negra concern human activity. Two aspects are of especial interest. First, undoubted evidence of fire has been uncovered (Fig.4), sealed within a 4.5 m-deep layer of sediment 5 m back from the present entrance, perhaps still further back 0.8 Ma if rock overhanging the entrance has undergone erosion since then. Thin-section micromorphology suggests combustion of sediment (Angelucci et al., 2013) and recent geochemical analysis supports that. Since 2011 excavation has yielded both thermally-altered, lustreless chert, with pot-lid fractures and conjoined splintering caused by thermal shock to both nodules and artificially-struck flakes, and also charred burnt animal bone and white calcined fragments showing conjoined lengthwise long-bone spalling typical of circumferential shrinkage after thermal volatilization of organic components (Walker et al., 2013). Recent taphonomical analysis and electron microscopy of bone fragments attribute discolouration to burning, not to post-depositional mineral staining, and both Fourier Transform infrared spectroscopy and electron spin resonance analysis of chert and bone imply firing temperatures ca. 550ºC (Walker et al., in preparation).

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cuevanegra4Fig. 4: Cueva Negra deep layer with thermally altered remains

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A fire-place is not a hearth. The Cueva Negra humans could have brought glowing brands left by a forest fire into the cave to establish and tend a fire where rain or wind would not put it out. They may well have been less afraid of fire outside than other animals they saw fleeing from it (which could have led them to play with fire in order to drive animals towards natural death-traps, such as swamps, enabling dismemberment and roasting). This does not mean they could reproduce or control fire; there is a dearth of archaeological evidence for hearths or fire-pits before 0.5 Ma.

Nevertheless, fire at ca. 0.8 Ma supported hominin cognitive versatility, techno-manual dexterity, and palaeoeconomic extractive behaviour in long-vanished Western European palaeoecological and palaeobiogeographical contexts. Cueva Negra exemplifies those aspects; Palaeolithic finds imply resources were exploited as far away as 40 km downstream and 30 km upstream from the site (Zack et al., 2013). That range is unsurprising given that ≥1.3 Ma early humans had begun migrating into Western Europe from northern Africa or western Asia, and therefore they could not have been congenital stick-in-the-muds even though, plausibly, their preferred habitats were localities with abundant biodiversity at hand (cf. ! Walker et al., 2006).  

The excavated Palaeolithic assemblage includes a bifacially-flaked “Acheulian” limestone hand-axe, though it mostly consists of small chert, limestone or quartzite artifacts (<60 mm long), knapped on site, often by bipolar reduction or repetitive centripetal flaking of small discoidal (“Levallois”) cores, and often showing marginal retouch that is mainly steep-angle (>50º) and sometimes abrupt (“Mousteroid”), and very occasionally invasive or semi-invasive low-angle (<30º)  (from the hand-axe to very small chert flakes <30 mm long). Serrated, notched or denticulate edges occur, and pieces bearing one or two large notches are common. Some flakes and several flattish or laminar subrectangular fragments were knapped to give steep abrupt (“Mousteroid”) edge-retouch (Fig.5). Steep retouch on a piece of flattish laminar chert can transform its perpendicular edge to give an acute angle useful for cutting or scraping. It is plausible to see that as being very different indeed from abrupt retouch of “scrapers” in most Mousterian assemblages where steep retouch applied to thin feathered flakes could spare them from accidental breakage by snapping during use or may have been applied to resharpen a cutting tool. Well-formed feathered flakes with striking platforms and bulbs of percussion are fairly uncommon at Cueva Negra, whereas small fragments of laminar chert abound. Many of the small artifacts seem to have much in common with those from the penecontemporaneous Catalan site of Vallparadís (Martínez et al., 2010) and from the Italian site of Isernia La Pineta, rather than with assemblages ≥1 Ma from Atapuerca and Orce.

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cuevanegra5Fig. 5: Cueva Negra Palaeolithic artifacts

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From a descriptive viewpoint of stone-knapping techniques the assemblage may be called “Acheulo-Levalloiso-Mousteroid” (! Walker et al., 2006; Walker et al., 2013; Zack et al., 2013); this descriptive techno-methodological approach can be uncoupled, viewed epistemologically, from prescriptive ontological typologies influenced by relative chronological inferences drawn tautologically from conjectural “culture history” and pseudo-evolutionary conjectures about Palaeolithic technology.

           Once freed from the dead hand of traditional perspectives, other aspects of the assemblage come to the fore. Several small retouched artifacts seem to fall into overlapping groups, in contrast to some other Spanish Early Pleistocene assemblages that have been called “Oldowan” due to perceived similarity to African ones; the term is inappropriate at Cueva Negra because, unlike typically Oldowan artifacts in Africa, nearly all those excavated at Cueva Negra are <60 mm in size. Steep retouch is seen on many pointed pieces; some are flattish pieces and could be regarded as fine points, “awls”, or “perforators”, whereas others resemble thick “Tayac points” described often in Middle and early Late Pleistocene European assemblages. Pointed artifacts include “becs”, small chunks of chert from each of which there projects incongruously a delicate elongated tiny spur, or “beak” (fancifully bringing to mind a small bird head with its beak). There are also many steeply-keeled fragments; some resemble steep scrapers on short stumpy cores, whereas others, knapped into elongated keeled planoconvex shapes resembling garden slugs (“limaces”) may be called “proto-limaces”. Beaks and slugs could be interpreted as convergent steep scrapers, or where both ends are pointed they could be envisaged as thick double points. However, researchers at 0.7 Ma Isernia La Pineta argue that its beaks and slugs are what were left behind after their reduction by bipolar knapping to remove extremely small flakes used as unretouched tools, backing their argument up with microscopical use-wear analysis and experimental knapping (Crovetto, 1994; Crovetto et al., 1994; Peretto, 1994; Peretto et al., 2004).

Flakes produced by bipolar knapping occur at Cueva Negra, though they are yet to be quantified because quantification of bipolar elements depends on whether carinated pieces with notches, spurs (beaks) and planoconvex double-ended slug-shaped pieces, were outcomes, first and foremost, of bipolar core-reduction to remove usable flakes, or whether, instead, they were primarily fashioned intentionally for use as implements themselves. The two possibilities need not be mutually exclusive because comparable pieces have been interpreted as implements, sometimes supported by microscopical use-wear analysis; an extensive literature exists with references to “limaces”, “becs” and “microperforators” from Pleistocene and Holocene lithic assemblages in Europe, Africa, and North and South America.

         Most Cueva Negra artifacts are “expedient”, frequently of “informal” shape, implying “opportunistic” or “eclectic” technological behaviour. They bring to mind the different blades of a Swiss knife. It is perhaps unsurprising that retouch is seen as often on stone fragments as on well-made flakes struck from prepared discoidal cores by recurrent repetitive centripetal flaking, given that at 0.8 Ma secant-plane control of knapping was in its infancy worldwide. It should be borne in mind that such cores are known from 1.3 Ma in Africa (de la Torre et al., 2004) where hand-axes have even greater antiquity (1.7 Ma) and that both of these involved bifacial flaking albeit with different formal secant-plane implications (asymmetrical and symmetrical, respectively), though more eclectic informal (“Oldowan”) tool-making continued alongside them. Extraction of regular flakes by recurrent repetitive centripetal flaking of prepared discoidal cores is demanding in both cognitive and technical terms (Coolidge and Wynn, 2005); the putative flakes are, as it were, “hidden” from view (like the yolk inside a hen’s egg, so to speak), and “unimaginable” simply from looking at the external shape of the stone before the reduction sequence begins. Evidence at Cueva Negra of both bifacial hand-axe production and recurrent repetitive centripetal flaking of prepared discoidal cores, together with a diverse range of small artifacts, implies manual dexterity, technical aptitude and cognitive versatility.  

        This raises the question of how those who frequented Cueva Negra 0.8 Ma ago perceived and exploited their surroundings, particularly where they obtained raw materials for stone tools. Two different matters are relevant. First, how far were the different possibilities of different rocks perceived? Secondly, were outcrops available then that nowadays afford suitable stone?

         The hand–axe shows 30 fresh bifacial extractions on a flattish limestone cobble with some cortex still present and a similar cobble had 15 unifacial fresh extractions along one side. Both probably were obtained from fluvio-lacustrine gravels, though X-ray diffraction and petrography indicate that their grey-blue micritic limestone (94% calcite; 6% quartz) originated in Lower Jurassic (Lias) rocks (! Walker et al., 2006). An unworked cobble from Cueva Negra is a dismicrite containing 10% quartz, radiolarian fragments, and filamentous planctonic fragments, characteristic of Middle Jurassic (Dogger) strata. Lower and Middle Jurassic beds are exposed in mountainsides upstream from the site. Another unworked limestone cobble from the site lacks quartz, being oolitic sparite (oosparite). Two limestone cobbles from a small conglomerate outcrop 0.8 km east of the site also lack quartz, one being composed of cryptocrystalline limestone pellets of organic faecal origin, the other of sparite cement with microscopical fossils.

The aforementioned conglomerate outcrop is an Upper Miocene (Tortonian) marine conglomerate, containing complete Ostreid and Pectinid sea-shell fossils (i.e. oysters and scallops), that formed as an inshore deposit of Tethys Sea1 of cobbles and stones eroded out of the nearby mountainside and later cemented by CaC03 when intense Upper Pliocene and Early Pleistocene neotectonic activity lifted up the mountains and their erstwhile sea-shore to its present height of 750 m a.s.l. (the Tortonian strata dip strongly to the SW and 0.8 km away lie at 730 m a.s.l. below Cueva Negra; the steep dip was not taken into account in some early publications, leading to mistaken interpretations). The cemented cobbles and stones are of limestone, chert and quartzite; several were taken at Cueva Negra and at the outcrop Palaeolithic artifacts have been picked up similar to those of the rock-shelter, including a small prepared discoidal chert core. The chert raw material includes eroded frangible tabular nodules derived from chert blocks or slabs of sub-parallele-piped shape. They are best described as “fissible” (Stein, 1981: 537) because hammering on them often fails to elicit conchoidal fractures or produce feathered flakes with well-developed convex bulbs of percussion. If hammering does not simply shatter the chert blocks into very small chips and fragments, it may split them open along fissible flat planes defined by internal structure or impurities, and produce flattish sub-rectangular laminar fragments available for modifying as tools.

Loose chert cobbles and blocks (some upto 0.3 m across weighing 5 kg) abound <5 km south of Cueva Negra from 770 up to 890 m a.s.l. on the flanks of mountains from whose crags of Jurassic limestone chert was eroded. Massive continental lateral erosion took place in the Upper Pleistocene and initial Pleistocene, leaving high-altitude vestiges of an erstwhile vast gravel spread 100-120 m thick (“raña”; “glacis”) containing conglomerate bands, the base of which lies ca. 45 m above the river today (Walker et al., 2013; Zack et al., 2013). Later on, much of that ancient gravel was displaced both laterally and longitudinally and redeposited, owing to ongoing Early Pleistocene erosion induced by falling base level as uplift continued. The process gave rise, in two or perhaps three depositional cycles, to horizontally-bedded outcrops of gravels and fluvio-lacustrine conglomerate that abound at relative heights of 5-25 m above the river today. These outcrops often include noteworthy fossil vestiges of local lakes. The matter is complicated by unequal uplift of the sides of the active longitudinal shear fault along which the R. Quípar runs (unequal uplift saved the Cueva Negra sediments from riverine erosion), and by unequal spatiotemporal activity of those faults normal to it which probably determined development or drainage of hanging lakes upstream in the upper Quípar valley (where it is called the Rambla de Tarragoya). In short, there is a wealth of possible secondary or even tertiary sources of eroded Jurassic chert, but just which were available to Cueva Negra chert-knappers called out for forensic research.

There are also a few small primary chert outcrops. One is of radiolarite ca. 40 km downstream from the rock-shelter where a radiolarite scraper was found in 2013. Another is of light-brown tabular chert at Río Caramel, a tributary of the R. Guadalentín that joins the R. Segura near Murcia; the upper Quípar is separated by a watershed from the Guadalentín river system. It has not been possible yet to determine whether light-brown chert at Cueva Negra came from the outcrop. At high altitude on the watershed itself there is a very small outcrop of biogenic chert that probably formed in a freshwater Pliocene lake, which has the unusual frondose cactus-like form not unlike that of East African Lake Magadi flint; at least one flake at Cueva Negra may well have come from the outcrop. Primary chert outcrops seem not to have been exploited intensively.  

Most Cueva Negra chert originated in Jurassic rock strata, albeit obtained from secondary or even tertiary gravel or conglomerate accumulations. Which ones? Petrographically the cherts look much alike. Might help come from chemical finger-printing of chert? Thanks to collaboration with the University of Arizona help came from the laser-ablation inductively-coupled plasma mass-spectrometry of trace elements present in several of the Earth’s crustal rocks (Sc, V, Cr, Co, Zn, Ga, Ge, Rb, Sr, Y, Zr, Nb, Cs, Ba, La, Ce, Pr, Nd, Sm). Chert samples were taken from a number of outcrops for comparison with chert from Cueva Negra (Zack et al., 2013).

Multivariate factorial analysis of the data show most chert fragments analyzed from Cueva Negra resemble chert sampled at the Tortonian conglomerate 0.8 km to the east (Fig.6). A few Cueva Negra fragments more closely resemble samples from fluvio-lacustrine gravel outcrops upstream in the Rambla de Tarragoya as far as the headwaters of the valley (where we even picked up a “proto-limace”) ca. 25 km south of the site. Plausibly, variation in trace-element composition cherts that had formed at separate localities or times in the Jurassic is reflected in compositional differences between outcrops of gravels that received chert nodules eroded from the mountainsides nearest by. Some of those cherts were taken to Cueva Negra. Trace-element characterization indicates how far humans ranged.

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cuevanegra6Fig. 6: Upper Quipar Valley Cueva Negra CNERQ and chart outcrops sampled

 

 

Research at Cueva Negra throws new light, including fire-light, on the cognitive versatility, manual dexterity and technical aptitude of early humans ca. 0.8 Ma in S.E. Spain. They exploited their surroundings in a competent fashion that implies precise knowledge and accurate awareness of what was available for survival. Research continues both in the field and laboratory at this intriguing late Early Pleistocene site.          

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Acknowledgements:

We thank all research collaborators named in the text or references as well as palaeontologists Drs. A. Ruiz Bustos, J. van der Made, X. Murélaga Beirucua and archaeologists Drs. D.A. Roe and I. Martín-Lerma for their kind help.

 

Footnotes:

1. This biocalcarenite rock is an Upper Miocene (Tortonian) sedimentary rock that formed between 11 and 7.5 million years ago in the bed of the vast Tethys Sea that extended from the Atlantic Ocean to the Persian Gulf (the Mediterranean Sea is all that remains of it). The rock is called biocalcarenite because it contains sand-size grains and fragments of sea-shells and coral, all cemented by calcium carbonate. It forms the floor, walls, and roof of Cueva Nega though these lack the cobbles and large pebbles that are found in more deeply lying, slightly older, Tortonian strata at a conglomerate outcrop 0.8 km E of the cave which was exploited by its Palaeolithic occupants who took cobbles to the cave and broke them open to knap the chert that some of them contained.

2. Magnetostratigraphy is the use of “geomagnetic reversals to correlate rock strata that have been dated accurately by other means at some places. It relies on palaeomagnetic signatures of remanent magnetism in rocks, which may be based on metals (such as iron) in volcanic rocks, or on the orientation of magnetic minerals in grains in sedimentary deposits, which was the basis for the palaeomagnetic research into the Cueva Negra Pleistocene sediments. Some history is in order here. In 1906 the French geophysicist Bernard Brunhes drew attention to the phenomenon we call “geomagnetic reversal”, after finding that an ancient volcanic rock was magnetized in the opposite direction to the Earth’s present-day magnetic field. For that to have happened, he inferred that the magnetic North Pole would have to have been near to what we regard as the magnetic South Pole today, implying that our planet’s magnetic field had undergone a reversal. In 1929 the Japanese geophysicist Motonori Matuyama published findings that began to show that different reversals of the direction (“polarity”) of the Earth’s magnetic field characterize different parts of the geological stratigraphical record, and in particular that the part which we nowadays regard as the Early Pleistocene (formerly, Lower Pleistocene) was characterized by a reversal of the polarity of our planet’s magnetic field. We now know that this reversal lasted from 2.588 to 0.78 Ma: that period is called the Matuyama reverse polarity chron and it was followed by the Brunhes normal polarity chron from 0.78 Ma to the present day; the 0.78 Ma reversal is called the Matuyama-Brunhes boundary. The Matuyama chron was interrupted by a few normal polarity episodes (two important ones are named after geological beds at Olduvai and Jaramillo). The Gauss normal polarity chron mainly characterized the Upper Pliocene between 3.59 and 2.588 Ma (3.6-2.6 Ma for most intents and purposes). A few hundred reversals now are known to have taken place during the history of our planet. All of the Cueva Negra sediment corresponds to the end of the Matuyama chron, according to the results of a study of the palaeomagnetism of 11 samples taken from top to bottom of the 5 m depth of its sedimentary fill and a further 2 taken in the escarpment below the cave mouth where sediment is exposed by erosion.

3. Optically-stimulated luminscence (OSL) dating of sediment grains attempts to estimate the time elapsed since the grains were last exposed to heat (e.g. sunlight) that destabilized the chemical make-up of minerals (e.g. quartz), which over time, at a known rate, recovers part of the stability that was disturbed. If several mineral grains are used for OSL, there is a risk that some may have been exposed to light or heat at later times than others were, thereby underestimating the age of a sedimentary deposit, and this problem may have affected the OSL dates obtained on multiple-grain samples analyzed at Oxford University by Dr. Jean-Luc Schwenninger, who has made three visits to sample Cueva Negra sediments, which suggested an age of 0.3-0.4 Ma when the less reliable multiple-grain method was applied, and more recently an age of at least 0.5 Ma using single-grain analysis (Schwenninger, personal communication). Unfortunately, the time and cost involved in undertaking accelerator mass-spectrometry when single grains are used, and the obvious need to analyze several of these independently, hinder widespread application of this approach. The method is related to that of thermoluminescence, TL, that has been used to date pottery and even burnt flint for the past fifty years, often with considerable success. Dr. Schwenninger is trying to apply it to burnt chert from Cueva Negra. Put crudely, if the amount of recovery towards stability can be determined, and if also we have a fair idea of what the original firing temperature was likely to have been, then by refiring in the laboratory at that temperature a handmade prehistoric potsherd, the full degree of that ancient destabilization of physicochemical constituents of atoms in clay molecules can be reproduced, and hence, from the amount of energy we have applied in order to do so, it is possible to estimate how much time had elapsed since the original firing. Much is known about the effect on different clays caused by varying the temeprature of the potter’s kiln. The matter gets far more complicated, alas, where chert or flint underwent burning in a bonfire of unknown heat. Luckily, at Cueva Negra the burnt chert comes from a deeply-lying lens of burnt sediment containing white burnt animal bones that had undergone calcination (i.e. all organic matter in them had been burnt out), which implies heating at high temperature according to knowledge from Forensic Biology. A high temperature implies humans were tending fire in the cave, because, so far inside the cave, it is unlikely a passing bush fire could have produced it. Research into the temperature, using the method of Fourier Transform infrared spectrometry (FTIRS) on the calcined bone, is being undertaken now, with promising initial results, by geoarchaeologist Dr. Francesco Berna at Simon Fraser University, and also by Dr. Anne Skinner using electron spin resonance at Williams College at Williamstown. Their preliminary findings point to a temperature of around 550ºC.

4 Sediment micromorphology is a “geoarchaeological” technique which uses the microscope to study thin-sections of sediment samples that have been removed on site with accuracy and precision and then hardened with an impregnating agent. Microscopy can determine the size and shape of granules in the sediment, and may ascertain whether some were deposited by “fluviatile” processes, i.e. by flowing water in streams or rivers, by more sluggishly moving water in lakes or swamps (“fluvio-lacustrine”), by wind “aeolian” deposition, by volcanic ash, by organic disturbance by roots, worm-holes, or other animal activities, including human ones, etc.. It can also determine the nature of granules, whether the minerals themselves or inclusions such as small fossils, fragments of bones, shells, plants, flecks of charcoal, or even minute fragments of artifacts such as chert knapping smalls or tiny fragments of potsherds. The word “micromorphology” refers to the study of the structure or form of the sediment, which is particularly important because there may be vertical or horizontal gradations in the phenomena observed, or regular distributions may be interrupted by irregularities. Much, of course, is known about the structure of different soils and the processes underlying their formation today, but sediment micromorphology has to consider how sediments developed in long-vanished environments and climates, and knowledge of geology is fundamental in geoarchaeology.

 5 Biotope refers to an area of uniform environmental conditions providing a living place for a specific assemblage or community of plants and animals. (Greek: bios = life, topos = place).

6. MIS: In the 1960’s it was found that, as igneous rocks in the bed of the ocean floor spread out from volcanically active vents in central ridges beneath the Atlantic and Pacific Oceans, they may come to lie in the position of zonal bands, formed sequentially over time, that lie parallel to a ridge. They can offer us information about geomagnetic reversals in the polarity of the planet’s magnetic field at the time they were extruded from the Earth’s molten core. The atomic clock can be used to date many of them when they have been sampled by deep-sea cores. Furthermore, the cores shed light on the density of the sea-water around the time they were formed. This is because, by analyzing the proportion of 16O to 18O isotopes in the calcium-carbonate exoskeletons of marine foraminifers (which are protozoan life-forms), in marine sediments that formed over each new zonal band, it is possible to determine the extent to which sea-water was diluted by freshwater from melting ice-caps in warm interglacial periods, or concentrated during cold glacial periods when water with the lighter oxygen isotope was drawn up preferentially into the atmosphere and then deposited elsewhere as snow and ice, and the 40K-40A  or  40A-39A “atomic clocks” help to date the palaeoclimatic oscillations. Those scientific advances, together with isotopic studies of ice from cores through the Greenland and Antarctic ice sheets, have given increasingly accurate information about the number and timing of palaeoclimatic fluctuations during the Pleistocene, when they became both relatively frequent and increasingly intense when compared with the preceding geological epochs of the Pliocene and Miocene, though others had occurred several times in our planet’s more distant past. They are designated variously as MIS or OIS, standing respectively for marine or oxygen isotope stages. Working backwards from the present interglacial (MIS-1 or OIS-1), odd numbers are used for interglacials, and even numbers for ice ages, with the slightly awkward exception of the last ice age which for various reasons, including a possible climatic amelioration, comprises stages 2, 3 and 4; thus the last interglacial period, between 0.13 and 0.118 Ma, is MIS-5 or OIS-5 (not MIS-3 or OIS-3). Biochronology and pollen analysis at ancient Pleistocene sites can give a general idea about the prevailing climatic conditions, which were mild and moist when sediments accunmulated in Cueva Negra. They imply a warm interglacial period, perhaps one that occurred about 0.8 Ma (MIS-21 or OIS-21), the tenth before the present one we are living in today. Rodent biochronology at Cueva Negra implies a time later than the end, at 0.99 Ma, of the Jaramillo normal polarity episode (1.06-0.99 Ma), in the later part of the Matuyama chron, because rodent species known in southern Spain from before that episode are not present at our site.

 

Legends to figures:

Fig. 1 Cueva Negra del Estrecho del Río Quípar in its surroundings.

Fig. 2 Cueva Negra del Estrecho del Río Quípar: Plan and sections.

Fig. 3 Cueva Negra del Estrecho del Río Quípar: Hand-axe, human teeth.

Fig. 4 Cueva Negra del Estrecho del Río Quípar: Deep layer with thermally altered remains.

Fig. 5 Cueva Negra del Estrecho del Río Quípar: Palaeolithic artifacts.

Fig. 6 Cueva Negra del Estrecho del Río Quípar in the Upper Quipar Valley with chert outcrops shown.

 

References:

Walker, M.J., Angelucci, D., Anesin, D., Berna, F., Fernández-Jalvo, Y., Haber-Uriarte, M., López-Martínez, M., Rhodes, S.E., Rodríguez-Estrella, T., Schwenninger, J-L., and Skinner, A.R. Evidence of Early Palaeolthic fire at the late Early Pleistocene site of Cueva Negra del Estrecho del Río Quípar (Caravaca de la Cruz, Murcia, Spain). In preparation for Session B53 The Archaeology of Early Fire Use, XVII UISPP Congress, Burgos. September 1-7 2014.

Angelucci, D., Anesin, D., López-Martínez, M., Haber-Uriarte, M., Rodríguez-Estrella, T., Walker, M.J., 2013. Rethinking stratigraphy and site formation of the Pleistocene deposit at Cueva Negra del Estrecho del Río Quípar (Caravaca de la Cruz, Spain). Quaternary Science Reviews 80: 195-199.

! Carrión, J.S., Yll, E.I., Walker, M.J., Legaz, A.J., Chain, C., López, A., 2003. Glacial refugia of temperate, Mediterranean and Ibero-North African flora in south-eastern Spain: new evidence from cave pollen at two Neanderthal man sites. Global Ecology and Biogeography12: 119-129.

Coolidge, F.L. and Wynn, T., 2005. Working memory, its executive functions, and the emergence of modern thinking. Cambridge Archaeological Journal 15: 5-26.

Crovetto, C., 1994, Le industrie litiche, analisi tecnico-tipologica dei reperti di scavo, in Peretto, C. (Ed.), Le Industrie Litiche del Giacimento Paleolitico di Isernia La Pineta, la Tipologia, le Tracce di Utilizzazione, la Sperimentazione, Isernia, Cosmo Iannone, “Istituto Regionale per gli Studi Storici del Molise ‘V. Cuoco’”, pp. 183-353.      .

Crovetto, C., Ferrari, M., Peretto, C., Longo, L., Vianello, F., 1994. The carinated denticulates from the Palaeolithic site of Isernia La Pineta (Molise, Central Italy): tools or flaking waste? The results of the 1993 lithic experiments. Human Evolution 9: 175-207.

de la Torre, I., Mora, R., Domínguez-Rodrigo, M., de Luque, L., Alcalá, L., 2003. The Oldowan industry of Peninj and its bearing on the reconstruction of the technological skills of Lower Pleistocene hominids. Journal of Human Evolution 44: 203-224.

Jiménez-Arenas, J.M., Santonja, M., Botella, M., Palmqvist, P., 2011. The oldest handaxes in Europe: fact or artefact? Journal of Archaeological Science 38: 3340-3349.

Martínez, K., García, J., Carbonell, E., Agustí, J., Bahain, J.-J., Blain, H.-A., Burjachs, F., Cáceres, I., Duval, M., Falguères, C., Gómez, M., Huguet, R., 2010. A new Lower Pleistocene archaeological site in Europe (Vallparadís, Barcelona, Spain). Proceedings of the National Academy of Sciences 107: 5262-5267.

Martínez-Andreu, M., Montes-Bernárdez, R., San Nicolás-del Toro, M., 1989. Avance al estudio del yacimiento musteriense de la Cueva Negra de La Encarnación (Caravaca, Murcia), in Crónica XIX Congreso Nacional de Arqueología, Castellón de la Plana 1987, Ponencias y Comunicaciones Volumen I,  Saragossa, Universidad de Zaragoza, Seminario de Arqueología, Secretariado de los Congresos Arqueológicos Nacionales, “Congresos Arqueológicos Nacionales”, pp. 973-983.

Peretto, C. (Ed.), 1994, Le Industrie Litiche del Giacimento Paleolitico di Isernia La Pineta, la Tipologia, le Tracce di Utilizzazione, la Sperimentazione, Isernia, Cosmo Iannone, “Istituto Regionale per gli Studi Storici del Molise ‘V. Cuoco’”.

Peretto, C., Arzarello, M., Gallotti, R., Lembo, G., Minelli, A., Hohenstein, U.T., 2004. Middle Pleistocene behavioural strategies: the contribution of Isernia La Pineta (Molise, Italy), in Baquedano, E., Rubio Jara, S. (Eds.), Miscelánea en homenaje a Emiliano Aguirre Volumen IV Arqueología, Alcalá de Henares, Museo Arqueológico Regional, “Zona Arqueológica Número 4”, pp. 368-381.

Scott, G.R. and Gibert, L., 2009. The oldest hand-axes in Europe, Nature 461: 82-85.

Stein, J. (Ed.), 1981. Random House Dictionary of the English Language The Unabridged Edition, New York, Random House, p. 537.

Walker, M.J., Angelucci, D., Anesin, D., Berna, F., Fernández-Jalvo, Y., Haber-Uriarte, M., López-Martínez, M., Rhodes, S.E., Rodríguez-Estrella, T., Schwenninger, J-L., and Skinner, A.R. Evidence of Early Palaeolthic fire at the late Early Pleistocene site of Cueva Negra del Estrecho del Río Quípar (Caravaca de la Cruz, Murcia, Spain). In preparation for Session B53 The Archaeology of Early Fire Use, XVII UISPP Congress, Burgos. September 1-7 2014.

! Walker, M.J., Gibert, J., Sánchez, F., Lombardi, A.V., Serrano, I., Eastham, A., Ribot, F., Arribas, A., Sánchez-Cabeza, J-A., García-Orellana, J., Gibert, L., Albaladejo, S., Andreu, J.A., 1998. Two SE Spanish middle palaeolithic sites with Neanderthal remains: Sima de las Palomas del Cabezo Gordo and Cueva Negra del Estrecho del Río Quípar (Murcia province). Internet Archaeology5 (autumn/winter 1998) http://intarch.ac.uk/journal/issue5/walker_index.html

! Walker, M.J., Rodríguez-Estrella, T., Carrión García, J.S., Mancheño-Jiménez, M-A., Schwenninger, J-L., López-Martínez, M., López-Jiménez, A., San Nicolás-del Toro, M., Hills, M.D., Walkling, T., 2006. Cueva Negra del Estrecho del Río Quípar (Murcia, Southeast Spain): An Acheulian and Levalloiso-Mousteroid assemblage of Palaeolithic artifacts excavated in a Middle Pleistocene faunal context with hominin skeletal remains. Eurasian Prehistory 4: 3-43.

 Walker, M.J, López-Martínez, M.V., Carrión-García, J.S., Rodríguez-Estrella, T., San-Nicolás-del-Toro, M., Schwenninger, J-L., López-Jiménez, A., Ortega-Rodrigáñez, J., Haber-Uriarte, M., Polo-Camacho, J-L., García-Torres, J., Campillo-Boj, M., Avilés-Fernández, A., Zack, W., 2013. Cueva Negra del Estrecho del Río Quípar (Murcia, Spain): A late Early Pleistocene hominin site with an “Acheulo-Levalloiso-Mousteroid” Palaeolithic assemblage. Quaternary International 294: 135-159.

Zack, W., Andronikov, A., Rodríguez-Estrella, T., López-Martínez, M., Haber-Uriarte, M., Holliday, V., Lauretta, D., Walker, M.J., 2013. Stone procurement and transport at the late Early Pleistocene site of Cueva Negra del Estrecho del Río Quípar (Murcia, SE Spain). Quartär,  Internationales Jahrbuch zur Eiszeitalter- und Steinzeitforschung, International Yearbook for Ice Age and Stone Age Research  60: 7-28.

 

Michael Walker*, Mariano López-Martínez**, María Haber-Uriarte***

© All rights reserved.

*Department of Zoology and Physical Anthropology, Biology Faculty, Murcia University, Espinardo Campus Universitario Edificio 20, 30100 Murcia, Spain.

Email: [email protected]; [email protected]; “M.J.Walker” <[email protected]>  Tel: 34-620-267104

**Calle Pintor Joaquín 10-4º-I, 30009 Murcia, Spain.

Email: [email protected]  Tel: 34-630-408806

***Department of Prehistory, Archaeology, Ancient History, Mediaeval History and Historiographical Techniques and Science, Faculty of Letters, Murcia University, La Merced Campus, Calle Santo Cristo 1, 30001 Murcia, Spain.

Email: [email protected]; [email protected], “María Haber” <[email protected]> Tel: 629-756183

Directors of the excavation, Murcian Association for the Study of Palaeoanthropology and the Quaternary, MUPANTQUAT web-site http:www.mupantquat.com (Murcia Archaeological Museum, Avenida Alfonso X El Sabio 7, 30008 Murcia, Spain), all correspondence to MUPANTQUAT Secretary M.López Martínez <[email protected]>), and

Murcia University Experimental Sciences Research Group E005-11 “Quaternary Palaeoecology, Palaeoanthropology and Technology” (c/o Dr.J.S.Carrión García, Department of Plant Biology (Botany), Biology Faculty, Murcia University, Espinardo Campus Edificio 20, 30100 Murcia, Spain)

The Neanderthals of Sima de las Palomas

The Sima de las Palomas vertical cave system was formed by karst solution of a Triassic marble hill in present-day Spain overlooking the Mediterranean. In 1991, a speleologist descending the 18-m deep entrance shaft (Fig.1) extracted a fossil (designated SP1) which, once the cemented breccia was removed, comprised Neanderthal maxillae connected to the mandible, with almost all their adult teeth. Subsequent systematic excavation (Walker et al., 2012a) uncovered three undisturbed Neanderthal partial skeletons (SP96, SP92, and a child, SP97) with several skeletal parts in anatomical position (including cranio-mandibular articulation, femoro-pelvic articulation, elbow, rib-cage, vertebral column, shoulder girdle, foot bones, etc.), Mousterian Palaeolithic artifacts, and animal bones (some charred), all lying deeply in a cemented rock tumble within the upper part of an 18-m deep wall of brecciated sediments (Fig. 2) was left exposed by miners after they took out most of the shaft’s sedimentary fill ca. 1900. SP96 and SP97 have crania and mandibles (Figs. 3, 4), unlike SP92. Because SP1 had lain near SP92 it might be SP92’s head. Excavation uncovered SP96 lying with elbows flexed and hands touching the forehead. Computer-assisted tomography revealed hand-bones in breccia adhering to the forehead of the SP97, identified as a child (Walker et al., 2012b), which lay underneath SP96, an adult, perhaps its parent. The position of the upper extremities implies intentional arrangement before rigor mortis had set in; it is recorded at some other Mousterian sites (Defleur, 1993).

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palomas1Fig. 1: Sima de las Palomas del Cabezo Gordo: Main shaft.

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palomas2Fig. 2: Excavation area A: Mouth of Main Shaft. B: Excavation area C: Base of rock tumble that contained the three Neanderthal skeletons. D: Thin hard conglomerate band beneath which excavation is continuing in layers with Mousterian remains.

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palomas3Fig. 3: Neanderthal adult female skeleton SP96, “Paloma”

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palomas4Fig. 4: Neanderthal child skull SP97 (“Paloma’s child”)

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Individual articulated skeletons are very important indeed because they provide more precise and accurate estimates of body size and proportions than estimates derived from pooled statistical analyses of a given bone type (e.g. femur, tibia, or humerus) from an assemblage of bones from different people who may well not be identifiable individually. SP96 was a short Neanderthal woman (”Paloma”), less than 20 years old, with the typically female wide greater sciatic notch of the pelvic basin which underwent post mortem distortion (that “virtual” reconstruction will correct from tomographs). The skeleton is about 85% complete, which permits precise and accurate morphological measurements for estimating body proportions (e.g. crural index, etc.) which are undoubtedly Neanderthal and robust (“hyperpolar”). Remarkably, its stature is one of the shortest known for Neanderthal adults (Walker et al., 2011a).

The child skeleton, SP97, lay underneath “Paloma” (her child?). Also short in stature, SP92 was probably less than 25 years old (Walker et al., 2011b). Short, too, was the owner of SP77, a femoral head from looser sediment that had banked up against cemented rock tumble and contained scattered Neanderthal remains, including mandibular fragments of a baby, a child, and an adolescent female (Walker et al., 2010a; Walker et al., 2008); this sediment contained lenses with signs of burning. Fragments of three more Neanderthal mandibles were found while sieving rubble left by miners. The Neanderthal finds included many teeth and bone fragments.

In all, at least 9 Neanderthals are represented at the site. The excavated Neanderthal remains correspond to a time about 50,000 years ago; different scientific methods  give estimates implying >40,000-<60,000 (U-series, TL, 14C: for details, see Walker et al., 2012b). Palaeopalynology indicates cool moist conditions though with persistence of species ill-adapted to resist frost (Carrion et al., 2003).

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palomas5Fig. 5: Stratigraphical position of the three articulated Neanderthal skeletons and situations of dated materials and two other Neanderthal mandibles (for further information, see Walker et al., 2012a).

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      Excavated with the SP97 child were the only articulated bones of large animals found at the site so far, viz., two sets of horse ankles (calcaneum, talus, cuboid), one group, cemented by CaCO3 to SP97’s skull, had undergone burning, the other, unburnt, beneath SP97’s trunk, included additionally a distal tibial fragment, and a third horse talus lay underneath SP97. Two leopard metacarpal bones lay near SP97’s skull and two leopard hind-paws, with metatarsal and phalangeal bones in anatomical articulation, lay 0.5 m from SP97’s skull in a similar level. It is unlikely horse ankles and leopard paws were fortuitous accumulations, given absence around SP97 of other body parts of those species. A heavily burnt leopard temporal bone found in mine rubble implies Neanderthal intervention; a large premolar tooth implies presence of cave hyaenas. Flakes and spalls from flint-knapping lay close to SP97. The site has yielded some carefully prepared Levallois points on flat triangular flint flakes with finely-retouched margins, surely effective for hunting with thrusting spears. Flint outcrops are unknown on Cabezo Gordo. Some flint quite likely came from a hydrothermal outcrop inspected ca. 25 km to the south, though it is hardly the source of the bulk of the Palaeolithic assemblage. Despite lack of clear-cut signs of intentional interment, large stones might have been thrown over SP96, SP92 and SP97 to deter leopards and hyaenas from disturbing the corpses. This is a prosaic interpretation.

Rarely are Neanderthal skeletons uncovered in anatomical connection. When animals die their soft parts decompose quickly, aided and abetted by various organisms (carnivorous animals or birds, insects, saprophytic fungi, bacteria, etc.), after which skeletons come apart. Long before they can get buried by natural deposition of sediment, wind and rain may scatter bones where carnivorous animals and birds have failed (exceptionally, skeletons of creatures trapped in caves or swamps escape from being scattered). At Sima de las Palomas three articulated skeletons from 50,000 years ago lay close together. It raises a conjecture that behavioural or cultural impingement occurred, implicating individuals other than the three deceased. Maybe it is an instance of Neanderthals attending to their dead, albeit with a prosaic motive.

The three skeletons and the rock tumble over them lay on a thin bed of extraordinarily hard conglomerate, though it contained some Palaeolithic artifacts and charred bone fragments. Beneath it coarse sediment has been excavated to a depth of 2 m so far, containing many bones of red deer, horse and other herbivores, many of which are charred, as well as rabbits and other small animals, including mandibular fragments of two porcupines (Hystrix brachyura: Rhodes et al., 2013).Tortoise seems to have played a part in the diet (Morales-Pérez and Sanchis-Serra, 2009). Characteristically Mousterian flint artifacts are present. Several smooth rounded cobbles were undoubtedly brought by Neanderthals to the site from stream gravels in the plain below. Being larger than some hammer-stones from the site they might have been used to pound or grind minerals (perhaps haematite; the Cabezo Gordo marble contains veins of magnetite and other iron ores) or foodstuff. Vegetable food at Sima de las Palomas is suggested both by phytoliths discovered in calculus on some Neanderthal teeth (Salazar-García et al., 2013) and two examples of dental caries (Walker et al., 2010b).

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Acknowledgements:

We thank all our research collaborators named in the text or references, but above all Dr. E. Trinkaus for his tireless work. Among our many other collaborators we thank archaeologists Dr. D.A. Roe and I. Martín Lerma, palaeontologist Dr. X. Murélaga Bereicua, and anthracologist Dr. E. Badal García.  

 

Legends to figures:

Fig. 1  Sima de las Palomas del Cabezo Gordo: Main shaft.

Fig. 2 Sima de las Palomas del Cabezo Gordo: Excavation area. A Mouth of Main Shaft. B Excavation area. C Base of rock tumble that contained the three Neanderthal skeletons. D Thin hard conglomerate band beneath which excavation is continuing in layers with Mousterian remains.

Fig. 3 Sima de las Palomas del Cabezo Gordo: Neanderthal adult female skeleton SP96, “Paloma”. SP96 has parts of all skeletal units except feet. Open L (left) greater sciatic notch shows SP96 was female. Full occlusal eruption of L M3 and ventrally unfused sacral bodies, unfused proximal clavicular epiphysis, and partially fused iliac crest, imply death at ≤20 years. All sufficiently-preserved long-bone and manual epiphyses are fused. SP96 skull had undergone crushing with loss of mandibular corpus and posterior, inferior and most of L neurocranium. R (right) facial elements are undistorted, albeit broken and displaced, with 22 teeth cemented into them. Axial skeleton comprises partial lower cervical, upper thoracic, and lumbar vertebrae; 5 sacral bodies; and >6 R ribs cemented to R scapula and clavicle which are complete, as are all 6 upper limb long bones. Metacarpals and manual phalanges are mostly present in anatomical position (some carpals show erosion). Posterior ilum apart, all elements of ossa coxae are present on at least one side, albeit broken, displaced, and cemented. R and L femora and L tibia are almost complete. Only SP96 and La Ferrassie 1 afford reliable adult Neanderthal lengths of all 4 major limb segments, clavicular and scapular lengths, and weight-bearing articular dimensions. SP96 Neanderthal cranial features: lateral supraorbital torus; broad supratoral sulcus; large frontozygomatic suture with columnar frontal process of zygoma; little horizontal angulation of anterolateral zygoma; absent canine fossa; strongly bilevel nasal floor with sharply-angled inferior nasal aperture margin; nasal aperture breadth (30–32 mm) overlapping between Neanderthal and Upper Palaeolithic modern human values; mandible with high R coronoid process; mandibular notch with lowest point closer to condyle; prominent superior medial pterygoid tubercle on ramus; rounded L gonial angle; strongly shovelled I2 with marked labial convexity. Neanderthal postcranial features: strong dorsal sulcus of the right scapula; narrow medial humeral pillar; medially orientated radial tuberosity; subequal pollical phalangeal lengths; ulnar deviation of pollical distal phalanx; elongated superior pubic ramus with thinned ventral margin; absent femoral pilasteric development; rounded convex cross-section of tibial diaphysis; absence of distinct fibular diaphyseal sulci. Aspects of SP96 less common in Neanderthals: nontaurodont teeth; short I1 labial root length (SP19 and SP21 have Neanderthal values); absent opponens pollicis flange on metacarpal 1; manual terminal phalanges of digits 3 and 4 with apical tufts lacking the Neanderthal rounded curve (e.g. SP28) and distinct ungual spines.

Fig. 4  Sima de las Palomas del Cabezo Gordo: Neanderthal child skull SP97 (“Paloma’s child”).

Fig. 5 Sima de las Palomas del Cabezo Gordo: Stratigraphical position of the three articulated Neanderthal skeletons and situations of dated materials and two other Neanderthal mandibles (for further information, see Walker et al., 2012a).

Fig. 6  Sima de las Palomas del Cabezo Gordo: Exploded stratigraphical sections and site plan; the thin hard conglomerate band in Fig. 2D runs across the middle of the sections.

 

References:

Carrión, J.S., Yll, E.I., Walker, M.J., Legaz, A.J., Chain, C., López, A., 2003. Glacial refugia of temperate, Mediterranean and Ibero-North African flora in south-eastern Spain: new evidence from cave pollen at two Neanderthal man sites. Global Ecology and Biogeography12: 119-129.

Defleur, A., 1993. Les sépultures moustériennes, Paris, Éditions du Centre National de la Recherche Scientifique.

Morales-Pérez, J.V. and Sanchis-Serra, A., 2009. The Quaternary fossil record of the genus Testudo in the Iberian Peninsula. Archaeological implications and diachronic distribution in the western Mediterranean. Journal of Archaeological Science31: 1152-1162.

Rhodes, S.E., Walker, M.J., López-Martínez, M., Haber-Uriarte, M., López.Jiménez, A.,  Buitrago-López, A.T., Dewar, G., 2013. Analysis of Hystrix specimens recovered from Sima de las Palomas, Murcia, Spain, in Program with Abstracts, Canadian Association for Physical Anthropology, 41st Annual Meeting, October 17-20 2013 Scarborough, ON (University of Toronto, Scarborough).Scarborough, University of Toronto, and Canadian Association for Physical Anthropology, p. 47.

 

Salazar-García, D.C., Power, R.C., Sanchis Serra, A., Villaverde, V., Walker, M.J., Henry, A.G., 2013. Neanderthal diets in central and southeastern Mediterranean Iberia. Quaternary International318,3-18.

Walker, M.J., López Martínez, M., Ortega-Rodrigáñez, J., Haber-Uriarte, M., López-Jiménez, A., Avilés-Fernández, A., Polo-Camacho, J.L., Campillo-Boj, M., García-Torres, J., Carrión-García, J.S., San Nicolas-del Toro, M., Rodríguez-Estrella, T., 2012a. The excavation of the buried articulated Neanderthal skeletons at Sima de las Palomas (Murcia, SE Spain). Quaternary International 259: 7-21.

Walker, M., Ortega Rodrigáñez, J., Agut Giménez, A., Soler Laguía, M., Zollikofer, C.P.E., Ponce de León, M.S. 2012b. The Sima de las Palomas Neanderthal skeletons: First steps towards “virtual” reconstruction. Proceedings of the European Society for the Study of Human Evolution 1: 191 (special issue, J-J.Hublin, W.Roebroeks, M.Soressi, T.Terberger, F.Spoor, Eds., Proceedings of the 2nd Annual Meeting of the European Society for the Study of Human Evolution ESHE 21-22 September 2012 Bordeaux/France). Leipzig, Max-Planck Institute for Evolutionary Anthropology, Society for the Study of Human Evolution.

Walker, M.J., Ortega, J., Parmová, K., López, M., Trinkaus, E., 2011a. Morphology, body proportions, and postcranial hypertrophy of a female Neandertal from the Sima de las Palomas, southeastern Spain. Proceedings of the National Academy of Sciences USA 108:1008710091. 

Walker, M.J., Ortega Rodrigáñez, J., López Martínez, M., Parmová, K.,  Trinkaus, E., 2011b. Neandertal postcranial remains from the Sima de las Palomas del Cabezo Gordo, Murcia, southeastern Spain. American Journal of Physical Anthropology 144: 505-515.

Walker, M.J., Lombardi, A.V., Zapata, J., Trinkaus, E., 2010a. Neandertal mandibles from the Sima de las Palomas del Cabezo Gordo, Murcia, southeastern Spain. American Journal of Physical Anthropology 142: 261-272.

Walker, M.J., Zapata, J., Lombardi, A.V., Trinkaus, E., 2010b. New evidence of dental pathology in 40,000 year old Neandertals. Journal of Dental Research90: 428-432. 

Walker, M.J., Gibert, J., López Martínez, M., Lombardi, A.V., Pérez-Pérez, A., Zapata, J., Ortega, J., Higham, T., Pike, A., Schwenninger, J-L., Zilhão, J., Trinkaus, E., 2008. Late Neandertals in Southeastern Spain: Sima de las Palomas del Cabezo Gordo, Murcia, Spain. Proceedings of the National Academy of Sciences USA, 105: 20631-20636.

 

Michael Walker*, Mariano López-Martínez**, María Haber-Uriarte***

© All rights reserved.

*Department of Zoology and Physical Anthropology, Biology Faculty, Murcia University, Campus Universitario de Espinardo Edificio 20, 30100 Murcia, Spain.

Email: [email protected]  Tel: 34-620-267104

**Calle Pintor Joaquín 10-4º-I, 30009 Murcia, Spain.

Email: [email protected]  Tel: 34-630-408806

***Department of Prehistory, Archaeology, Ancient History, Mediaeval History and Historiographical Techniques and Science, Faculty of Letters, Murcia University, Campus Universitario de La Merced, Calle Santo Cristo 1, 30001 Murcia, Spain.

Email: [email protected] Tel: 629-756183

Directors of the excavation, Murcian Association for the Study of Palaeoanthropology and the Quaternary, MUPANTQUAT web-site http:www.mupantquat.com (Murcia Archaeological Museum, Avenida Alfonso X El Sabio 7, 30008 Murcia, Spain), all correspondence to MUPANTQUAT Secretary M.López Martínez <[email protected]>, and

Murcia University Experimental Sciences Research Group E005-11 “Quaternary Palaeoecology, Palaeoanthropology and Technology” (c/o Dr.J.S.Carrión García, Department of Plant Biology, Biology Faculty, Murcia University, Campus Universitario de Espinardo Edificio 20, 30100 Murcia, Spain)

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A Tale of Cities Lost and Found

Santiago Giraldo is currently Director of the Colombia Heritage Program with the Global Heritage Fund. He has an MA in Social Sciences and a PhD in Anthropology from the University of Chicago. He has worked for the Instituto Colombiano de Antropología e Historia (ICANH) as a research archaeologist, Coordinator for Archaeology, and Director-in-Charge of the Teyuna-Ciudad Perdida Archaeological Park, and has conducted extensive research and preservation at the archaeological sites of Pueblito and Teyuna-Ciudad Perdida over the past ten years. Today he is considered one of the world’s foremost authorities on the ancient Tairona people.

In 1881, after three years of travel throughout the Sierra Nevada de Santa Marta mountains in Colombia, South America, the British explorer, naturalist and geographer Frederic A.A. Simons published the first detailed map of the mountains in the Proceedings of the Royal Geographical Society of London. It included a brief description of the Sierra Nevada, its watershed, the indigenous population, and the surrounding towns. It was indeed the first relatively precise map of one of the highest coastal mountain systems in the world, which reaches heights over 19,000 feet above sea level within a scant 25 miles of the Caribbean coastline. Interestingly enough, the map included the supposed location of Posigueica, the fabled capital of the Tairona, the prehispanic peoples inhabiting the area when the Spanish first arrived in the first decades of the 16th century.

After the paper was read in an evening Royal Geographical Society meeting, there followed a question and answer session in which Sir Clements Robert Markham, president of the Society, asked Mr. Simons a question of enduring influence and consequence for all subsequent researchers. He asked “whether there was any trace of the Taironas, one of the most warlike tribes ever known in South America, who, after several battles, drove the Spaniards back to Santa Marta, or; whether they had been wholly exterminated.”1 Simons then answered that it seemed that they had been “completely exterminated and replaced by tribes coming in from the Orinoco”.

What, indeed, actually became of the Tairona? For all accounts and purposes, they had disappeared completely after the 16th century.

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perdida1The Simons map
Frederic Simons’ was the first relatively accurate map of the Sierra Nevada de Santa Marta up until 1939 when the Cabot Expedition for the American Geographical Society conducted a photogrammetric survey. It served as a basis for all maps of the Sierra Nevada up until WWII. The red lines index his travels throughout the massif. (The map appears in Simons 1879 article for the Royal Geographical Society. This is a composite image created by the author.)

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perdida2Map showing the Sierra Nevada de Santa Marta region within its geographic context in northern Colombia. Credit Santiago Giraldo

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perdida3The Sierra Nevada de Santa Marta showing very general limits to what is considered to be the area inhabited by the Tairona up until the end of the 16th century, in relationship to the present-day nearby geographic areas and town/archaeological sites. Credit Santiago Giraldo

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The Discovery

Our knowledge about these fabled and little known polities who held sway over the northern and western reaches of the Sierra Nevada de Santa Marta has slowly improved over the past 100 years. Known primarily for their intricate gold work exhibited at the Bogotá Museo del Oro (Gold Museum) and other museums in North America and Europe, the Tairona built large towns and urban centers up and down the numerous rivers flowing downwards from the snow covered peaks.2 They were prolific artisans, and though less known, their stone beadwork, bone and wood carvings, and pottery are also outstanding. Their featherwork and textiles, though described as fabulously ornate and beautiful by the Spanish conquistadors, have not survived.

Up until the 1970s, only five archaeologists had actually worked in the area around Santa Marta: John Alden Mason with the Field Museum of Natural History in Chicago in 1922-23, Gregory Mason for his dissertation at the University of Southern California in 1936, Gerardo Reichel-Dolmatoff and his wife Alicia Dussán between 1946 and 1949, and Henning Bischof in the 1960s.3 Their work concentrated on coastal sites currently located within Tairona Natural Park (Parque Nacional Natural Tairona), and it was Alden Mason’s research that led to the initial discovery of Pueblito, a large Tairona town where he excavated most of the objects currently on display at the Field Museum of Natural History in Chicago.  Subsequent investigations by Reichel-Dolmatoff and Dussán, and Bischof made it the best-known Tairona town until the discovery of Teyuna-Ciudad Perdida. Despite their work, little was known about the extent of Tairona settlements in the general area, and there was next to no information on towns and sites located higher up on the mountain slopes. 19th century travelers such as Simons and Elisée Reclus, the French anarchist geographer, mentioned in their writings that they had seen and walked upon long staircases and stone-paved paths that wound their way up the mountain, so it was highly probable that Tairona towns and settlements were not confined to the coast. Yet no archaeologist had explored the upper slopes of the mountain. Covered in tropical forest, with a broken topography that makes movement and exploration incredibly difficult, it was not until the 1970s that the extent of Tairona settlements on the northern and western sides of the mountain became clear.

Beginning in 1973 and up until 1976, the Instituto Colombiano de Antropología-ICAN (Colombian Institute of Anthropology) began an ambitious project led by two of its archaeologists, Luisa Fernanda Herrera and Gilberto Cadavid, whose objective was to systematically survey as many river basins as possible on the western and northern sides of the mountain, locating Tairona settlements throughout the area.4  Around the same time (1973), Paul Bahn, Richard Luckyn, and Patrick Jacquelin, who were then students at Cambridge University, organized an expedition to survey the Mendihuaca, Buritaca, and Don Diego rivers on the northern side of the mountain.5 Jack Wynn, a U.S. archaeologist, was also conducting fieldwork for his dissertation in the lower Buritaca River. All things considered, either one of the three projects/expeditions could have found Teyuna-Ciudad Perdida. It was simply a question of time, timing, and a bit of luck. When Paul Bahn and I met in 2009 in New York for lunch and he kindly gave me his copy of their expedition’s report, he expressed that not finding Ciudad Perdida had been a sore disappointment. In fact, the disappointment is shared by many of us, for no archaeologist discovered Teyuna-Ciudad Perdida. By the beginning of 1976 however, Herrera and Cadavid had located 199 Tairona villages and towns that spread from the western to the northern side of the mountain.6 The extent and density of the settlements was a surprise, and served to show that the 16th century Spanish documents describing the Sierra Nevada as “full of peoples and towns” were not an exaggeration.

As the story was narrated to Luisa by the guides during the trip, it was in fact Julio César Sepúlveda, the son of a professional looter by the name of Florentino Sepúlveda living nearby on the Guachaca River, who happened to find the city during a hunting trip, some time around 1975.7 A bird he shot fell on an exposed stone step of the staircase that led up to the site. At that time, the Sierra Nevada de Santa Marta was literally crawling with looters in search of Tairona gold, and over 5,000 of them were employed by various patrons who funded their looting expeditions. The Sepúlveda family began to quietly and systematically loot the town, but other “guaqueros” (looters) soon got wind of the fabulous gold objects they were finding and tracked them up the Buritaca River. As usually happens in this line of business, the rival crews worked out who had “rights” over the area with shotguns and rifles. In the ensuing firefight, Julio César was killed, and the word spread like wildfire among the looters that a fabulous Tairona city in the Buritaca had been found and that “guaqueros” were killing each other over the gold. In the aftermath, one of the patrons, a man by the name of Jorge Barón who had funded the looting expeditions to the site, unexpectedly contacted the director of the Gold Museum in Bogotá and proposed a “joint venture”, wherein they would share the profits of the finds. Utterly perplexed by this strange offer, the director of the Gold Museum alerted the director of ICAN, who in turn called upon Louisa and Gilberto to set up an expedition to this place out in the middle of nowhere – a place that guaqueros were calling “el infierno” (hell) due to its remoteness and isolation.

Reaching Teyuna-Ciudad Perdida by foot today usually takes visitors 4 to 6 days round trip, with plenty of strenuous hiking along a 16 mile trail. At that time, however, there were no open trails, outfitters or guides, and the upper sections of the Guachaca and Buritaca rivers were completely uninhabited. Faint hunting tracks criss-cross the forest, and it is very easy to get lost or disoriented. A few homesteaders lived further down river and indigenous Kogi families had just begun colonizing the upper sections of the watersheds, which were completely covered in tropical montane forest and had been completely uninhabited for almost 400 years. No one, apart from the “guaqueros” actually knew how to get there.

The archaeologists traveled to Santa Marta and spoke with Jaime Barón, who introduced them to two of the looters who had been “working” the site and had agreed to guide them. Bernardo Valderrama, an architect, and Lucía Rojas, another archaeologist working for ICAN, had also joined the team by then. Given the difficulties of reaching the site on foot, an army helicopter was chartered, and the looters were able to lead them up the river canyon up to a narrow hill overlooking the Buritaca River at an elevation of 3300 feet above sea level. The hilltop was completely covered in dense forest; with towering Tagua palm trees over 120 feet high that made it impossible to land. The pilot suggested they lower themselves by rope, but without knowing how far below the canopy they would find solid ground, the idea was extremely risky and reckless, so they rapidly abandoned it after some discussion. The team was forced to go back to the military base and approach the site on foot, crossing the Guachaca River basin and then slowly moving up the Buritaca River until they reached the partially exposed staircase the looters were using to climb up to the site.

It took the team five grueling days to reach “el infierno”, sleeping under a plastic tarp and palm leaf shelters in the forest to protect themselves from the nightly downpours. Along the way, Lucía Rojas had to stay at a homesteader’s farm because her feet, according to Luisa, had become a single large blister that made it impossible for her to walk. The guides insisted that “no woman” had ever made it to “el infierno”. Rivers and streams were crossed several times and they were constantly wet and cold beneath the rainforest. The idea of turning back reared up its ugly head a few times, but according to Luisa, she was willing to head up to the site accompanied by a single guide if need be. In the end, Luisa, Gilberto, and Bernardo reached the site with their two guides,  “El Negro” Rodríguez and Franky Rey. (Franky later on became the first foreman and site administrator for Teyuna-Ciudad Perdida Park). What they found soon became Colombia’s most important archaeological find in the 20th century and an iconic archaeological park for Colombia in general.*

The team camped out at the site for three days under a palm frond shelter, rationing their meager supplies that were attacked on a nightly basis by opossums and rats. Wet and bedraggled from the constant rain, mud, and the evening fog that completely covered the hilltop, they began clearing out bits and pieces of the site. As they explored the forest-covered town, they could see the lunar-like landscape left by the looters: scores of holes and broken potsherds littering the forest floor. But by lightly clearing some areas they also became aware of the stone masonry walls, staircases, and flagstone paved terraces that were everywhere. The more they cleared the more they found, and as Luisa has often told me when we discuss that moment, the visible remains of stone structures simply kept going on and on along the ridgeline and slopes of the hill top. After three days, their food ran out and they were forced to head back to the trailhead and from there on to Santa Marta. Back in Bogotá, they tried to explain to ICAN’s director, Álvaro Soto, the significance of what they had seen.

By June of 1976, ICAN set up a major research and conservation project that spanned 5 years, opening Teyuna Ciudad Archaeological Park to the public in 1981. Officially, Louisa and Gilberto named the site “Buritaca 200”, given that it was the 200th Tairona site they had found and it was located on the Buritaca River basin. Bernardo Valderrama, the architect who was with them, is responsible for the name “Ciudad Perdida”, The Lost City. Much sexier than “B-200”, the moniker stuck and by the mid 2000s the name of the park officially became Teyuna-Ciudad Perdida Archaeological Park. Additional work between 1981 and 1986 led to the discovery of another 26 Tairona villages and towns of varying sizes located in the surrounding area. Since the park was opened, ICAN (now ICANH, Colombian Institute for Anthropology and History) has been in charge of research, conservation, and management.8 Two structures, a nuhue and a huitema, ceremonial houses used by kogi men and women respectively, were built in 1999 to accommodate the periodic rituals carried out by the indigenous community that now lives in the area.9

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perdida5The team arrives on the third day at the farm of a homesteader by the name of Gertrudis. Lucia Rojas had to remain here due to blistered feet. (L to R) “El Negro” Rodríguez, Louisa, Bernardo, Gilberto, Franky. Courtesy Louisa Fernanda Herrera

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perdida7The team resting on a fallen log after a four-hour climb to the top of “amansa guapos” (man tamer) hill on the way to Ciudad Perdida. Note the dense forest fog surrounding them. (L to R) Franky, Gilberto, Luisa and Rodríguez. Courtesy Luisa Fernanda Herrera

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perdida6Franky Rey, the looter who would go on to become Ciudad Perdida’s first administrator, standing atop a vegetation covered staircase. Courtesy Luisa Fernanda Herrera

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perdida8Left to right, Bernardo, Lucia, Gilberto, Frank, Luisa, and “El Negro” Rodriguez resting after the expedition to Ciudad Perdida. Courtesy Luisa Fernanda Herrera

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Research and Conservation from 1977-2014

What visitors see today when they reach Teyuna-Ciudad Perdida is the product of 37 years of research and conservation work. The areas of the town, or city if you will, that are currently open to the public extend over 80 acres, but the protected area comprises over 400 acres and includes three additional sites that are not open to the public: Garage 1 and 2, and B-201, which are currently under research. During the initial phase of the ICAN project, 85% of the town was cleared and restored, with excavation work concentrating on domestic structures. When the archaeologists arrived in June of 1976, it became apparent that looter crews had returned and practically destroyed some of the more important structures in their hurry to find whatever gold they could before the site was closed to them by ICAN. Much conservation work in those years entailed fixing this damage, but the town is large enough that numerous structures went untouched. Unfortunately, the looters did get away with many of the most spectacular finds, which were gold and pottery objects associated with single burials located within the rammed earth and stone masonry terraces. None of these objects, all acquired by private buyers, have been recovered.

Teyuna-Ciudad Perdida was laid out over the hilltop in such a fashion that its administrative and political center covers a narrow ridgeline, with residential wards located towards the slopes. The ridgeline and slopes were leveled out using a combination of rammed earth and masonry terraces, and round buildings with stone foundations were set upon them. A 10,000 square foot terrace, for example, has multiple round or oval buildings and is connected to adjacent terraces via paved walkways or staircases. At this point, less than 10% of the town has been excavated, but more importantly, for the first time archaeologists were able to understand what a Tairona town actually looked like. It has been fully mapped and surveyed twice, the first time by Guillermo Rodriguez and Margarita Serje in 1980, and the second time by an ICANH-Global Heritage Fund archaeological and topographic survey crew in 2011.  

One of the more striking features of Tairona architecture and settlement layout (that became apparent as the site was slowly uncovered), is its apparently informal, curvilinear, low-density, and spacious quality, with residential wards and ceremonial/feasting areas spread out over extremely broken, mountainous terrain. In contradistinction to most other early towns and cities studied by archaeologists in the Americas, where square or rectangular rooms along with masonry walls, corridors and doorways are used to parse out, divide, subdivide, and restrict built space, Tairona settlements make use of open terracing without walled divisions and emphasize roundness in built structures. For most visitors, this makes it quite difficult to understand what was used for what purposes, since most everything looks exactly the same and functional differences between structures have to be teased out through excavation.

The open architecture that is a characteristic of Tairona towns makes it very difficult to know what constitutes private or public space. In a town such as Ciudad Perdida that by A.D. 1500 would have had 2500 to 3000 inhabitants, everyone would have been on view to everyone all the time as they moved about or worked in the open spaces and patios. Circulation and movement throughout the town would have been completely unrestricted, with multiple paths available for reaching different areas. In other words, unlike our own circulation pattern, which enforces movement along prescribed pathways using walls and corridors, Tairona societies emphasized unrestricted flow and movement. As such, the network of paved pathways connecting structures to one another at Ciudad Perdida allows a visitor to move about in various ways between different parts of the town. Finding your way within the town actually requires creating a mental map of pathways and circulation patterns that can then be followed in different combinations depending on where you want to go. These are in fact hub and spoke arrangements, with a terrace and residential building working as a hub that is connected to other terraces and residential areas via multiple paths (spokes). In a town such as this one where everyone is on view to everyone and movement is unrestricted, day to day interaction would probably have followed a number of sociocultural norms and clues regarding who can or cannot enter certain spaces, and who can or cannot use specific pathways. This radically different way of conceiving and conceptualizing built space is also what makes studying the Tairona so fascinating.

Research carried out for my dissertation between 2005 and 2010 also concentrated on understanding the deeper history of places such as Teyuna-Ciudad Perdida and Pueblito.10 The radiocarbon dates secured during the 1980s suggested that Ciudad Perdida dated to the 11th century A.D., but there were no dates for Pueblito, which made it hard to understand whether places such as these had followed common or divergent trajectories. We knew that they had been abandoned sometime around the 1600s due to a combination of diseases brought in by the Spanish and cyclical warfare with them, but we knew very little about what had happened before that. In the 1960s, Henning Bischof found a particular type of pottery that differed significantly from the Tairona wares that we already knew. The people who had produced the pottery appeared to be from an earlier time period that he called Neguanje. He assigned a tentative range of A.D. 500-750 to this time period, but had no radiocarbon dates to support his hypothesis. A few years later, Wynn found these types of pottery in his own research but like Bischof was unable to date them. Subsequent research along the coast found some burials from this period but no habitation sites. It was assumed that these particular people were the predecessors of the Tairona but the data was still insufficient to establish a direct and unequivocal relationship.

Ironically but unsurprisingly, while we were carrying out the architectural and topographic survey of Pueblito near the coast we were able to locate Neguanje period structures buried deep below Tairona terraces and structures on view to visitors and archaeologists alike. They had been, so to speak, underneath our noses all this time but had gone unnoticed by previous projects. Two overlapping Neguanje period dwellings, for example, were found almost 9 feet below the surface of a Tairona period terrace at Pueblito. In subsequent excavations at Teyuna-Ciudad Perdida we found the same pattern: earlier occupations and structures buried below structures that had been on view to everyone. When I discussed these findings in 2010 with Alicia Dussán, she indicated that it was quite clear that they had not been found because of the clean and very thick layers of fill separating the occupation levels. This had led them to assume only sterile layers of fill were to be found below Tairona household floors.

This finding has allowed us to better understand the construction sequence of these places in a more nuanced and subtle fashion. Radiocarbon dates from buried occupations at both sites suggest that they were initially settled some time between A.D. 500 and A.D. 700, and grew relatively slowly up until A.D. 1100, reaching a size of about 30 acres. Core area plazas, terracing, and structures were then rapidly built some time between A.D. 1100 and A.D. 1200 and remained unchanged until A.D. 1600. That is, these areas were used and reused continuously but saw no major changes in their architectural layout. Yet both towns continued to expand after this time period, with growth concentrating mainly in residential areas. It is now clear that the Neguanje period peoples were directly related to the Tairona, and that there is a deeper time frame to the inhabitation and transformation of the northern and western side of the Sierra Nevada de Santa Marta. As exciting as this new information is, further research on these buried occupations faces serious challenges. To be able to excavate them properly we would have to dig through Tairona structures, dismounting paved floors, house foundation rings, retaining walls, and staircases. This of course is a very prickly issue because both Teyuna-Ciudad Perdida and all other archaeological sites in the Sierra Nevada de Santa Marta are considered national heritage. For the indigenous peoples of the Sierra Nevada (Ijku, Kankuamo, Kogi, and Wiwa communities), the site is a sacred place that should not be disturbed by research activities. For these reasons, further investigation of this particular time period and its relationship to how these towns grew and developed requires rethinking research design and excavation methods. With the Colombian Institute of Anthropology and History and Teyuna-Ciudad Perdida’s conservation team, we are currently assessing the use of minimally intrusive methodologies such as Ground Penetrating Radar, magnetometry and other such sub-surface mapping techniques.

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perdida14Tairona circulation patterns emphasize free flowing movement. The central area terraces have numerous internal paths and adjacent, integrated sidewalks such as these that would have allowed people to move about freely between the different parts of the town. Credit Santiago Giraldo

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perdida16The “piedras” (stones) sector of the town has many beautifully built structures, but its main characteristic is the use of large boulders as foundation for terraces and rings. Much of the stone used to build Ciudad Perdida was quarried in this area, where laminar schist boulders such as the one on the right in the photograph can be found strewn about the slopes of the hill. Credit Santiago Giraldo

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perdida15In higher status dwellings, perfect circles of cut and dressed stone elevated above the terrace are achieved by using trapezoidal-shaped cut blocks with a curved edge. Notice also the two entrances. Masons had to work in situ to be able to assemble these rings. Credit Santiago Giraldo

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perdida13Spanish documents from the 16th century mention that Tairona family structure was polygamous. An extended family at Ciudad Perdida would have inhabited one or more interconnected terraces with various dwellings and structures such as these. This is a large terrace with two stone foundation rings. Credit Santiago Giraldo

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perdida9Excavations all along Ciudad Perdida’s central sector in 2006 showed that this part of the town was built in a single push between A.D. 1100-1200. Credit Santiago Giraldo

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perdida10As part of the Master Management Plan and as a way of correcting a number of errors found in the 1980 map of the town, we surveyed and mapped Ciudad Perdida using total stations and set in brass benchmarks linked to Colombia’s geodetic grid. February 2011. Credit Santiago Giraldo

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perdida4Map showing the distribution of Tairona sites located to date in the northern and western faces of the Sierra Nevada de Santa Marta. Blank areas have not been surveyed, but we know they hold numerous sites that still need to be mapped. Credit Santiago Giraldo

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Current Projects

In recent years (2010-2014) and in my capacity as Colombia Program Director for the Global Heritage Fund, our efforts at Teyuna-Ciudad Perdida have concentrated on solving a great number of issues and problems that emerged in the past 30 years that threatened the park’s future. In alliance with the Colombian Institute of Anthropology and History, the Colombian Park Service, the outfitters and guides, and the indigenous and peasant councils of the Buritaca Basin we have developed a number of heritage conservation, environmental, and community development projects that will hopefully ensure sustainable visitation in the foreseeable future. 11

Up until 2007, due to Colombia’s internal conflict, conservation work at the park came to a standstill. The general area was under the control of paramilitary groups and most peasant families lived off of coca production, which meant that developing any sort of project in the area was a risky endeavor. To make matters even worse, and though tourists trickled into the park even under these conditions, a kidnapping in 2003 of 8 tourists by the ELN insurgent group (Ejército de Liberación Nacional) placed the site on every country’s travel warning list. This also forced ICANH to bring down all park rangers, which made basic maintenance work a nightmare. Facilities deteriorated completely, sections of the site were overgrown with vegetation, and it was impossible to control visitation. After the 2007 demobilization agreements between the Colombian government and the paramilitary groups the situation was quite desperate and there was next to no funding available for the park. In 2009, GHF and ICANH designed a six-year project aimed at setting the park back on its feet, involving a three-pronged strategy focusing on improving management and conservation activities at the park and carrying out a number of much needed community development projects between the trailhead town and the park itself.

Between 2010 and 2012, GHF and ICANH concentrated on designing a management and conservation plan for Teyuna-Ciudad Perdida, a crucial factor that had gone unresolved since the park opened in 1981. Without the management plan, it was extremely difficult for ICANH personnel unfamiliar with the park and its history to understand long-standing problems and difficulties and thus envision strategies to resolve them. Hence, a multiplicity of projects have been developed, either to provide much needed data required for decision-making purposes or to set in motion activities suggested by the management plan. For example, the town was surveyed and mapped once again in 2011. This corrected a number of inaccuracies present in the 1980 map and gave us a Digital Elevation Model or DEM, to work with for setting up visitation circuits, buffer zones, and delimiting a protected area. Satellite imagery for the whole basin from various remote sensors was acquired, maps were updated, and we began to groundtruth the 26 sites in the vicinity of Teyuna-Ciudad Perdida. We have also begun to slowly add new sites missed during the 1980s. Each one of the structures within the area open to the public was assessed for damages and a comprehensive conservation plan was designed and set in motion. Since 2010, and for the first time since it opened to the public, conservation teams have worked every year. As I mentioned previously, research, mapping and survey work continued during 2013 at Garage 1 and 2, and B-201, sites located within the protected area delimited by the management plan.

In turn, community development projects have encompassed a wide range of activities. These have included designing new curricular materials for the trailhead school aimed at heritage and environmental conservation, wilderness first aid training for all guides, providing rescue equipment at key lodges, setting up gray and black water treatment systems for lodges, building a 90-foot-long suspension bridge at a particularly dangerous ford in the river, and building a new health post at the indigenous village of Mutanzhi. In 2012, a team of researchers from SELVA and Panthera-Colombia carried out a much needed biodiversity evaluation, aided by members of the indigenous and peasant communities. This project provided basic data needed to assess visitor impact on wildlife along the trail, thus providing baseline data allowing us to fine tune the carrying capacity assessment. Researchers also collected data on large felines with camera traps. We were able to find out that at least five puma and two jaguars, along with a healthy population of ocelots, are permanent residents along the trail. SELVA researchers also taught several workshops on bird identification and a wildlife guide for the trail was printed out and distributed at all lodges so that visitors could also learn about the incredible range of fauna along the trail.

From 2014 to 2016 we will be concentrating on expanding our mapping and survey work a bit further upriver to include a site by the name of “Tigres”. Located approximately 2.3 miles upriver, Tigres (also known as B-203 in the literature) was located in 1978 and initially mapped and investigated between 1980 and 1981. Even though it is a relatively small site of approximately 8-12 acres with some 50-60 structures, for many years now, looters have systematically targeted the site A rumor among the looters gave it its name, since a few of them claimed to have found jaguar figurines made out of gold.12 During a visit in 2010 we became aware that looters continued to “work” the site and so it was decided with ICANH that we should try and recover as much information as possible before the site was completely lost.

At Teyuna-Ciudad Perdida, Conservation activities will continue to be developed on a yearly basis according to the management plan, as well as detailed architectural mapping of each structure intervened by the team. Because the only available landing area for army helicopters to bring in provisions for soldiers stationed at the site is the 1100-1200 A.D. central platform, we would also like to be able to install vibration sensors. This will give us hard data on how landing and takeoff affect the structure. New personnel facilities are also in the process of being designed, and we hope to increase the number of park rangers from four to seven.

In sum, though much has been gained in the past four years and everyone has pitched in to solve issues and problems going back more than three decades, we still have much to do. Then again, there is still much to be learned about the Tairona. 

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perdida11Due to the extremely heavy rainfall in and around Ciudad Perdida (over 157 inches per year), as well as tourist visitation, the staircase leading in to the site needed to be restored early this year. All conservation activities are part of a Master Conservation Plan designed by Ciudad Perdida’s head conservator, Ms. Catalina Bateman. The basic crew is headed by Walter Hinojosa, conservation supervisor. January 2014. Credit Santiago Giraldo

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perdida12Community development in the area encompasses a wide range of activities that I co-design with indigenous and peasant leaders after extensive discussions. In late 2012 we agreed with the indigenous authorities that a new Health Post was needed at the Kogi village of Mutanzhi, on the trail to Ciudad Perdida. Throughout 2013 Global Heritage Fund raised funds from various sources, and construction began in March of 2014. The health center is being built using superadobe, a stabilized soil building technique that minimizes the use of cement and brick and provides great formal flexibility. The indigenous community has provided labor and materials such as wood, sand, stone, and soil. Here we can see the indigenous crew taking a break after hauling sand. May 2014. Credit Santiago Giraldo

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Individuals interested in learning more about Ciudad Perdida and/or contributing to the efforts at the site may go to the Global Heritage Fund website for more details.

*The park currently receives about 8500 visitors per year. Any good guidebook to South America has instructions on how to get to the site and contact information for the different outfitters. Also, the 2009 English edition of the Teyuna-Ciudad Perdida Guidebook is freely available at ICANH’s website.

References and relevant bibliography

Bahn, Paul, Richard Luckyn, and Patrick Jacquelin. 1973. “Cambridge Expedition to Santa Marta, Colombia  Summer 1973.” Unpublished expedition report. Cambridge.

 

Bischof, Henning. 1961. News Report from Bischof: Colombia. In Katunob 2(3):41-45 Magnolia

—–1969a. Contribuciones a la cronología de la cultura Tairona Sierra Nevada de Santa Marta. In Proceedings of the 38th International Congress of Americanists. pp.259-269.

—–1969b. La Cultura Tairona en el Area Intermedio. In Proceedings of the 38th International Congress of Americanists. pp. 271-280.

 

Cadavid, Gilberto, and Luisa F. Herrera. 1985. “Manifestaciones Culturales En El Area Tairona.” Informes Antropológicos 1: 5–54. Bogota: Instituto Colombiano de Antropología

 

Dever, Alejandro. 2007. Social and Economic Development of a Specialized Community in Chengue, Parque Tairona, Colombia. Unpublished PhD dissertation, University of Pittsburgh

 

Giraldo, Santiago. 2010. “Lords of the Snowy Ranges: Politics, Place, and Landscape Transformation in Two Tairona Towns in the Sierra Nevada de Santa Marta, Colombia”. Unpublished PhD dissertation. Chicago: University of Chicago.

—–2009. Teyuna-Ciudad Perdida Guidebook. Bogotá: Instituto Colombiano de Antropología e Historia.

 

Groot de Mahecha, Ana María. 1985. Arqueología y Conservación de la localidad precolombina de Buritaca 200 en la Sierra Nevada de Santa Marta.  Informes Antropológicos 1. 55-102. Bogotá: Instituto Colombiano de Antropología.

 

Herrera, Luisa Fernanda. 2013. “El Hallazgo de Ciudad Perdida.” Unpublished document

—–1984a. “Agricultural Activity in the Sierra Nevada de Santa Marta (Colombia): Historical Perspective.” In La Sierra Nevada de Santa Marta (Colombia) Transecto Buritaca la Cumbre, Thomas van der Hammen and Pedro M. Ruiz, Eds, 501–30. Berlin-Stuttgart: J.Cramer.

—–1984b. “Buritaca 200: Survey of the Archaeology and a Palynological Investigation.” In La Sierra Nevada de Santa Marta (Colombia) Transecto Buritaca la Cumbre, Thomas van der Hammen and Pedro M. Ruiz, Eds, 531–46. Berlin and Stuttgart: J.Cramer.

 

Mason, John Alden. 1931. Archaeology of Santa Marta, Colombia: The Tairona Culture: Marshall Field Archaeological Expedition to Colombia, 1922-23. Field Museum of Natural History. Anthropological Series 304, 358, 446. Vol. XX, no. 1-3. Chicago.

 

Mason, Gregory. 1938. “The Culture of the Taironas”. Unpublished Dissertation, University of Southern California.

 

Reichel-Dolmatoff, Gerardo. 1951. Datos historico-culturales sobre las tribus de la antigua Gobernación de Santa Marta. Santafé de Bogotá: Imprenta del Banco de la República.

—–1953. Contactos y cambios culturales en la Sierra Nevada de Santa Marta. In Revista Colombiana de Antropología, 1 (1): 15-122.

—–1954a. Investigaciones Arqueológicas en la Sierra Nevada de Santa . Marta. Partes 1-2. Revista Colombiana de Antropología 2(2): 147-106.

1954b. Investigaciones Arqueológicas en la Sierra Nevada de Santa  Marta. Parte 3. Revista Colombiana de Antropología 3: 141-170.

—–1954c. A Preliminary Study of Space and Time Perspective in Northern Colombia. American Antiquity, 4: 352-66.

 

Simons, F.A.A. 1879. Notes on the Topography of the Sierra Nevada de Santa Marta. Proceedings of the Royal Geographical Society and Monthly Record of Geography 1, 11 (Nov): 689-694.

_____. 1881. On the Sierra Nevada de Santa Marta and Its Watershed (State of Magdalena, U.S. of Colombia). Proceedings of the Royal Geographical Society and Monthly Record of Geography 3, 12 (Dec): 705-723.

 

Soto, Alvaro. 1988. La Ciudad Perdida de Los Tayrona. Bogotá: Neotrópico.

 

Wynn, Jack. 1974. Buritaca Ceramic Chronology: a seriation from the Tairona Area, Colombia. Unpublished PhD Dissertation, University of Missouri.

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Footnotes 

[1] Simons 1881, 722.

[2] A simple web search for Tairona gold work will throw thousands of images. Almost a full third of the Gold Museum´s collection (34,000 pieces) is comprised of Tairona gold artifacts.

[3] Mason, John Alden. 1931. Archaeology of Santa Marta, Colombia: The Tairona Culture: Marshall Field Archaeological Expedition to Colombia, 1922-23. Field Museum of Natural History. Anthropological Series 304, 358, 446. Vol. XX, no. 1-3. Chicago.;

Mason, Gregory. 1938. “The Culture of the Taironas”. Unpublished Dissertation, University of Southern California.

Reichel-Dolmatoff, Gerardo. 1951. Datos historico-culturales sobre las tribus de la antigua Gobernación de Santa Marta. Santafé de Bogotá: Imprenta del Banco de la República.; 1951. Contactos y cambios culturales en la Sierra Nevada de Santa Marta. In Revista Colombiana de Antropología, 1 (1): 15-122. ; 1954a. Investigaciones Arqueológicas en la Sierra Nevada de Santa . Marta. Partes 1-2. Revista Colombiana de Antropología 2(2): 147-106. ; 1954b. Investigaciones Arqueológicas en la Sierra Nevada de Santa  Marta. Parte 3. Revista Colombiana de Antropología 3: 141-170. 1954c. A Preliminary Study of Space and Time Perspective in Northern Colombia. American Antiquity, 4: 352-66.

Bischof, Henning. 1961. News Report from Bischof: Colombia. In Katunob 2(3):41-45 Magnolia

1969a. Contribuciones a la cronología de la cultura Tairona Sierra Nevada de Santa Marta. In Proceedings of the 38th International Congress of Americanists. pp.259-269. 1969b. La Cultura Tairona en el Area Intermedio. In Proceedings of the 38th International Congress of Americanists. pp. 271-280.

[4] Cadavid, Gilberto, and Luisa F. Herrera. 1985. “Manifestaciones Culturales En El Area Tairona.” Informes Antropológicos 1: 5–54.

[5] Bahn, Paul, Richard Luckyn, and Patrick Jacquelin. 1973. “Cambridge Expedition to Santa Marta, Colombia  Summer 1973.”

[6] Based on further archaeological evidence from river basins east of the Buritaca and other unexplored areas, both Luisa and I agree that there are more than the 260 Tairona sites located to date. If the same settlement densities hold for the other basins, the total number of Tairona towns and villages probably exceeds 500.

[7] Herrera, Luisa Fernanda. 2013. “El Hallazgo de Ciudad Perdida.” Unpublished document.

[8] An account of the Ciudad Perdida project can be found in Soto Holguín, Alvaro. 1988. La ciudad perdida de los tayrona. Bogotá: Neotrópico. About 98% of the academic literature on Ciudad Perdida is in Spanish. All unpublished excavation reports can be found at ICANH’s library in Bogotá.

[9] The upper section of the Buritaca River was completely uninhabited up until about the early 1960s when homesteaders slowly began moving up the river and indigenous Kogi families moved in from the Don Diego River towards the east. The Kogi village of Mutanzhi, which lies on the trail to Teyuna-Ciudad Perdida, is actually quite recent and dates to 1986.

[10] Giraldo, Santiago. 2010. “Lords of the Snowy Ranges: Politics, Place, and Landscape Transformation in Two Tairona Towns in the Sierra Nevada de Santa Marta, Colombia”. Chicago: University of Chicago.

[11] The project has been successful thanks to the generous support of a great many donors and agencies such as CitiFoundation, Morgan Family Foundation, Fondo Patrimonio Natural (Colombia)- USAID Conservation Landscapes Program, Fundación Bolívar-Davivienda (Colombia), and private donors in Colombia, the United States, and Europe. Allied foundations such as OPePA (Colombia), SELVA (Colombia), Panthera-Colombia, and Fundación Puentes de la Esperanza (Colombia) have all contributed with expertise and in-kind support as well. Without the unwavering commitment of the guides, Kogi indigenous community of Mutanzhi, and the campesino community, none of these activities would have been possible. ICANH has consistently sought to increase the park’s budget in the past four years and provided substantial conservation co-funding.

[12] In the Sierra, jaguars are usually called “tigres” (tigers) by the indigenous and peasant population rather than jaguares.