VANDERBILT UNIVERSITY—Stone tools, cooked animal and plant remains and fire pits found at the Monte Verde site in southern Chile provide greater interdisciplinary evidence that the earliest known Americans—a nomadic people adapted to a cold, ice-age environment—were established deep in South America more than 15,000 years ago. The research, led by Tom Dillehay, Rebecca Webb Wilson University Distinguished Professor of Anthropology, appears in the Nov. 18 issue of PLOS ONE.
In 2013, at the request of Chile’s National Council of Monuments, Dillehay and an international team of archaeologists, geologists and botanists performed an archaeological and geological survey of Monte Verde to better define the depth and breadth of the site, which is protected by the Chilean government.
It is familiar ground for Dillehay, who has worked there since 1977, and it is there that Dillehay found evidence that fundamentally contributed to a new understanding of how and when humans first arrived in the Americas. His excavations have yielded a wide variety of scientific evidence of a small human settlement, using a different stone tool technology that predated the Clovis people, traditionally considered by many scholars as the earliest human culture in the Americas, by about 1,500 years at a site called MVII. Finds included hearths, the remains of local animals, wooden posts from approximately twelve huts, scraps of clothing made of hide, a portion of meat with preserved DNA of a mastodon, and even a human child’s footprint still preserved in clay. Archaeologists have estimated the population of the site at around 20-30 inhabitants. Dillehay also uncovered possible, though not conclusive, evidence of a much earlier human presence at a nearby site called MVI, dating back to possibly 30,000 years ago.
Dillehay’s findings were initially greeted with skepticism by the archaeological community, as it challenged the broadly accepted paradigm for human entry into the Americas. Until about 40 years ago, the prevailing understanding was that the Americas first began to be populated 13,000 years ago by big-game hunters from Asia who used a distinctive type of fluted stone projectile point called Clovis points. But subsequent excavations by other archaeologists at sites in both North and South America have also yielded evidence supporting an earlier human migration through the Americas.
On this visit, Dillehay’s team explored key areas around MVI and MVII. Though it was not intended to be a comprehensive reexamination of the sites, their findings did yield new insights. “We began to find what appeared to be small features—little heating pits, cooking pits associated with burned and unburned bone, and some stone tools scattered very widely across an area about 500 meters long by about 30 or 40 meters wide,” said Dillehay.
The stone tools discovered by the team were similar to what Dillehay had previously found at Monte Verde. Many were simple unifacial tools—meaning they were worked on only one side of the stone, to create a sharp edge—though some of the younger tools and projectile points indicate bifacial technologies. “One of the curious things about it is unlike what we found before—a significant percentage, about 34 percent, were from non-local materials. Most of them probably come from the coast but some of them probably come from the Andes and maybe even the other side of the Andes,” said Dillehay. Prior research had revealed evidence of Andean plants in the area, providing further support for a highly mobile population.
Terrain similar to what Monte Verde might have looked like during the late Pleistocene era. The ground is crisscrossed by shallow drainage features, while higher ground has patchy vegetation. Credit: Tom Dillehay
A very small faceted basalt wedge. Basalt is a local material. This tool, found at MVI, was made 15,000-16,000 years ago. It would have been used for woodworking. Credit: Tom Dillehay
A pebble tool with a bifacially knapped and retouched edge. The stone, called serpentine, is not a local material but likely comes from the coastal cordillera west of Monte Verde. It was found at the older site, MVI, and was made 17,000-19,000 years ago. Credit: Tom Dillehay
Stones, bones, plants and fires
The team recovered a total of 39 stone objects and 12 small fire pits associated with bones and some edible plant remains, including nuts and grasses. The bones tended to be small fragments, broken and scorched, indicating that the animals had been cooked. They often came from very large animals, like prehistoric llamas or mastodons, as well as smaller creatures like prehistoric deer and horses. The Monte Verde site was unlikely to have supported the kind of vegetation that those animals needed to eat, so they were likely killed and butchered elsewhere. The objects were radiocarbon dated and most were found to range in age from more than 14,000 to almost 19,000 years old.
The wide scattering suggests that the people who created these features were nomadic hunter-gatherers who might have camped for only a night or two before moving on. “Where they’re going, we don’t know, and where they’re coming from, we don’t know, but this would have been a passageway from the coast to the foothills of the Andes,” Dillehay said. Dillehay believes that they may have come through Monte Verde because the terrain was more walkable than the surrounding bogs and wetlands, and because it provided access to stone to make tools.
Rain, ice, soil and ash
A key goal during this visit was to better understand the geological and environmental context of the site. At the end of the last ice age, Monte Verde was a sandur plain—a runoff area situated about six kilometers away from a glacier, crisscrossed by a network of shallow streams and brooks fed by rain washing off the glacier, as well as melting snow. It was also a time marked by volcanic activity and a gradually warming climate, as the last glaciers began to retreat.
“It appears that these people were there in the summer months,” Dillehay said. “Each one of these [burned] features and the bones and stones associated with them is embedded in thin, oxidized tephra”—a type of geological layer formed by airborne ash particles from nearby volcanoes that only form in rainy, warmer temperatures. But though the glaciers had begun to retreat by 19,000 to 17,000 years ago, it was still an extremely challenging environment, Dillehay said. “We’re looking at people living in some really cold, harsh areas, even in the summer months.” Only later, around 15,000 years ago, did the climate warm enough to support the kind of longer-term settlement found at MVII.
Put together, these findings support the paradigm shift toward an earlier peopling of the Americas, although questions inevitably remain about how the hemisphere was settled. It also underscores the importance of long-term interdisciplinary research. “We now realize that the geology and the climate and the archaeology are much more complex than we ever calculated,” said Dillehay.
Source: Edited and adapted from the subject press release of Vanderbilt University.
This research was supported with grants from the National Geographic Society, the National Science Foundation, the Consejo de Monumentos Nacionales de Chile and Vanderbilt University.
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