A Paleolimnological Record from Lake George, New York

Wiltse B & Stager JC. 2017. A paleolimnological record from Lake George, NY. Adirondack Journal of Environmental Studies, 16(1): 1-7.

In this study a 30 centimeter (cm) sediment core taken from the north basin of Lake George was analyzed for changes in diatom community structure. The chronology of these sediments was established using radioisotopic dating methods. A unique and interesting sedimentary profile was observed while retrieving cores throughout the north basin of the lake. The nature of this sedimentary profile, along with supporting evidence from the diatom community, strongly suggests that a low stand occurred in the lake sometime between 200-350 before present (BP). The low stand likely predated heavy settlement of the watershed and would have resulted in a several meter drop in lake level. It is possible the lake was rebounding from this low stand as the watershed was being settled. Evidence of the recent onset of cultural eutrophication was also observed in the diatom community structure, and is probably related to development within the watershed. These findings highlight the importance of monitoring and predicting hydrological conditions in the Lake George watershed as human-driven climate change complicates the natural range of rainfall and drought variability in the region. They also provide a context for understanding the current state of the lake and understanding the degree of anthropogenic impacts on the watershed.

Brendan Wiltse

Brendan is a professional landscape, nature, and wildlife photographer with over 20 years of experience. He holds a Ph.D. in biology from Queen’s University and is an accomplished research scientist. His photography focuses on the conservation of the natural world. He is most well known for his work photographing the Adirondack Park in upstate New York but has worked across the eastern United States and Canada.

https://www.brendanwiltse.com
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Major shifts in diatom community structure suggest the influence of recent climate change on lakes in the boreal region of Canada.