In 2009, the Submerged New World team investigated several areas that have potential to contain deposits from the Late Pleistocene. This year the team will return to some of these ares to investigate them more thoroughly. C. Andrew Hemmings and Nicolas Alvarado dig a hole through old coral that covers the buried — and ancient — Suwannee River, about 75 miles offshore. Click image for larger view and image credit.
Mission Plan
J. M. Adovasio
C. Andrew Hemmings
Expedition Principal Investigators
Mercyhurst College
In our efforts to explore for the evidence of this Pleistocene landscape, and the people who once lived upon it, we will use a wide range of excavation tools and diving equipment. Scuba divers will use a suction dredge with a 100 foot long, six inch diameter tube to dig test excavation holes through the modern sandy seafloor and into the earlier layers we believe contain evidence of when people and Pleistocene animals roamed this area between 10,000 and 20,000 years ago. The dredge will send the sediments to a floating screen where we will collect bones, artifacts, and anything else of interest that we find. Our screen deck has graduated inserts, like giant screen doors, of ½, ¼, and 1/16th windowscreen, that we can use to collect even the tiniest scrap of evidence sent up from the deep.
As we collect representative samples of shells, coral, and other material on the screen we will be paying close attention for any shallow or nearshore species that indicate lowered sealevel. Below the sand and shell bottom we should start to see finer sediments with more black organic matter that might indicate shallow brackish water estuaries or lagoons like you often see today along the Gulf Coast. Below those layers we hope to recover evidence of both fresh water riverine sediments and even intact dry land sediments. Finding either of the last two kinds of sediment means we are in the right time period and if there is evidence of the Pleistocene people or fauna in our holes we would expect to find it in and below these levels.
Sea level rise since the last glacial episode. Click image for larger view and image credit.
You may find yourself wondering “but they go to all this effort, why would they do this?” There are a host of reasons to conduct this research but the overriding scientific imperative is fairly straightforward. Simply put, what we really know about the past is derived from the direct evidence we are able to collect in the field and analysis in the lab. Whether looking for information on long term climate change, sea level rise, the extinction of the Pleistocene megafauna, or how people first arrived and lived in the New World, the amount of direct evidence we have in hand is very small. Much of what we think we know about these topics is based on models and informed speculation. Directly probing the sequence of sediments discussed above will generate new data that can be used to give us a better understanding of the past, long term changes to the world, and how people and animals have adapted to the world in which they live.
Because our exploration is so far from the modern shore we hope to find artifacts and food remains of people living in the Americas that are both older than anything we have found elsewhere and based on a way of life related to living close to coastlines. If we find an early coastal culture we would expect to find both new species of plants and animals that were utilized, and new types of tools that we have never seen before as well. The greater age, distance from previously examined resource bases, and exploitation of different resource bases of these sites far from land today, are all expected to lead us to a culture unlike anything we have previously seen in the New World.
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