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Origin: A Genetic History of the Americas

by Jennifer Raff

by Jennifer Raff

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to confirm that <strong>the</strong> stratigraphic layers containing <strong>the</strong> bison and stone tools<br />

were probably from <strong>the</strong> late Pleistocene (6).<br />

GEOARCHAEOLOGY<br />

Geoarchaeology is <strong>the</strong> application <strong>of</strong> geologic principles and<br />

methods to <strong>the</strong> solution <strong>of</strong> archaeological questions.<br />

Early geoarchaeologists in <strong>the</strong> <strong>Americas</strong> during <strong>the</strong> late 19th<br />

and early 20th centuries did much <strong>of</strong> <strong>the</strong> work to establish<br />

chronologies for archaeological sites before <strong>the</strong> advent <strong>of</strong><br />

radiocarbon dating by correlating stratigraphic layers with<br />

climatic events.<br />

Contemporary geoarchaeologists use sophisticated<br />

approaches to address complex questions in <strong>the</strong> research <strong>of</strong> a<br />

particular site. First, <strong>the</strong>y aim to understand <strong>the</strong> nature <strong>of</strong> <strong>the</strong><br />

landscape and environment during a site’s use. This<br />

environmental backdrop can tell us a lot about <strong>the</strong> ancient<br />

peoples’ priorities and choices. For example, geoarchaeologists<br />

ask why people might have chosen to live in a specific place.<br />

Was it close to water? Did it <strong>of</strong>fer access to (or control <strong>of</strong>)<br />

certain plants, tool stone, or animal resources? Were <strong>the</strong>re<br />

geological features that gave protection from <strong>the</strong> wea<strong>the</strong>r (or<br />

rival groups <strong>of</strong> people)?<br />

Ano<strong>the</strong>r goal <strong>of</strong> geoarchaeology is to reconstruct how a site<br />

was formed. To understand site formation processes,<br />

geoarchaeologists “read” <strong>the</strong> pr<strong>of</strong>iles <strong>of</strong> sedimentary deposits<br />

and soils—which toge<strong>the</strong>r make up <strong>the</strong> site’s stratigraphic<br />

sequence. They place this stratigraphic sequence in <strong>the</strong> context<br />

<strong>of</strong> surrounding regions and o<strong>the</strong>r sites. This context provides<br />

information for essential understanding <strong>of</strong> who was using <strong>the</strong><br />

site, when <strong>the</strong>y were using it, and <strong>the</strong>ir activities. For example,<br />

by reconstructing <strong>the</strong> formation processes at a particular site,<br />

geoarchaeologists could tell us not only that it was abandoned<br />

300 years after it was formed, <strong>the</strong>y could potentially tell us why<br />

it was abandoned. They might be able to correlate <strong>the</strong>

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