Evidence of Late Quaternary Fires from Charcoal and Siliceous Aggregates in Lake Sediments in the Eastern U.S.A.
The late-glacial transition to the Holocene, 15,000–11,600 cal yr BP, is an enigmatic period of dynamic global changes and a major extinction event in North America. Fire is an agent of disturbance that transforms the environment physically and chemically, and affects plant community composition. To...
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TRACE: Tennessee Research and Creative Exchange
2015
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Online Access: | https://trace.tennessee.edu/utk_graddiss/3492 https://trace.tennessee.edu/cgi/viewcontent.cgi?article=4871&context=utk_graddiss |