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Title: Quaternary vegetation history of the Mississippi embayment

Journal Article · · Quat. Res. (N.Y.); (United States)

Nonconnah Creek, located in the loess-mantled Blufflands along the eastern wall of the Lower Mississippi Alluvial Valley in Tennessee displays a sedimentary sequence representing the Altonian Substage through the Woodfordian Substage of the Wisconsinan Stage. The site has a biostratigraphic record for the Altonian and Farmdalian Substages that documents warm-temperate upland oak-pine forest, prairie, and bottomland forest. At 23,000 y B.P., white spruce and larch migrated into the Nonconnah Creek watershed and along braided-stream surfaces in the Mississippi Valley as far as southeastern Louisiana. The pollen and plant-macrofossil record from Nonconnah Creek provides the first documentation of a full-glacial locality in eastern North America for beech, yellow poplar, oak, hickory, black walnut, and other mesic deciduous forest taxa. During the full and late glacial, the Mississippi Valley was a barrier to the migration of pine species, while the adjacent Blufflands provided a refuge for mesic deciduous forest taxa. Regional climatic amelioration, beginning about 16,500 y B.P., is reflected by increases in pollen percentages of cool-temperature deciduous trees at Nonconnah Creek. The demise of spruce and jack pine occurred 12,5000 y B.P. between 34/sup 0/ and 37/sup 0/N in eastern North America in response to postglacial warming.

OSTI ID:
5242535
Journal Information:
Quat. Res. (N.Y.); (United States), Vol. 13
Country of Publication:
United States
Language:
English