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- W563966581 abstract "A core from Osgood Swamp, California, which is located south of Lake Tahoe, in the Sierra Nevada, was analyzed every odd centimeter to a depth of 61 cm0 The Hypsithermal to Neoglacial transition occurs in the $1 to h9 cm interval, Pinus shows four distinct peaks and troughs, varying more than the other pollen types in the core. The Ericaceae show two distinct peaks accompanying the Pinus lows. Pollen analytical and ecological considerations indicate that bog heaths are the source of the Ericaceous record0 The Ericaceae peaks are believed to represent periods of moist coldness corresponding to Neoglacial events in the Sierra Nevadac Correlation of an ash layer at 180 cm, immediately above a radio carbon date of 6990 + 300 B.P. with an ash layer at 1 7 0 cm in my core, and other considerations, give an inferred sedimentation rate of about hi yr/cm in my core. This places the Ericaceae peaks at about 1 0 0 A J )0 and 1 6 3 0 A 0Do, and the Hypsithermal to Neoglacial transition in Osgood Swamp at about 2^00 B'„P0" @default.
- W563966581 created "2016-06-24" @default.
- W563966581 creator A5002909161 @default.
- W563966581 date "1973-01-01" @default.
- W563966581 modified "2023-09-27" @default.
- W563966581 title "A neoglacial pollen record from Osgood Swamp, California" @default.
- W563966581 hasPublicationYear "1973" @default.
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