47 Limnological Records in Past, Present, and Future Climates
Tuesday, 24 March 2015
3:30 PM - 5:30 PM
Reagan Room
WATERSHED CHARACTERISTICS, CLIMATE, AND IN-LAKE DYNAMICS IN RELATIONSHIP TO THE HISTORY OF GLOEOTRICHIA ECHINULATA
Paper number: 47-3
Program: Theme Sessions
Time: 4:10 PM – 4:30 PM
Authors
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Emil RydinUppsala University, Norrtälje, N/A
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Kathleen C. WeathersCary Institute of Ecosystem Studies, Millbrook, NY
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Kathryn L. CottinghamDartmouth College, Hanover, NH
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Peter R. LeavittUniv of Regina, Regina, SK
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Alyeska U. FiorilloBates College, Lewiston, ME
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John P. SowlesBates College, Lewiston, ME
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John E. MacKenzieBates College, Lewiston, ME
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Brian P. QuarrierBates College, Lewiston, ME
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Cayelan C. CareyVirginia Tech, Blacksburg, VA
Abstract
Paleorecords revealed different histories of watershed disturbance, lake eutrophication, and abundance of G. echinulata among lakes. In five lakes, G. echinulata was most abundant between 1750 and 1900, a time of both variable climate and agricultural activity in these watersheds. However, a sixth lake showed 20th century expansion of G. echinulata, and the seventh had exceedingly low concentrations of G. echinulata in the last 400 years and none in the half century preceding that. Thus, while land clearance and agricultural activity might be implicated as important drivers of G. echinulata abundances in some of the lakes, more eutrophic conditions were associated with lower populations in at least two lakes, perhaps because of light limitation. Despite apparently coincident modern increases in G. echinulata in lakes regionally, paleoecological analyses reveal that this species inhabited these lakes prior to European settlement. Further, no single mechanism can explain the historical patterns of abundance of G. echinulata, underscoring the importance of catchment differences in mediating regional influences such as climate.