Lake-size variations in the Lahontan and Bonneville basins between 13,000 and 9000 14C yr B.P

Palaeogeography, Palaeoclimatology, Palaeoecology
By: , and 

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Abstract

Recessions of Lakes Lahontan and Bonneville that commenced ∼13,500 14C yr B.P. were interrupted at ⪖11,500 14C yr B.P. in the Lahontan basin and ∼12,200 14C yr B.P. in the Bonneville basin by relatively large perturbations in lake level that persisted for ∼ 2000 years. Minor glacial readvances in the Sierra Nevada and White Mountains of California-Nevada occurred during the latter half of this interval (between 11,000 and 9700 14C yr B.P.). The hydrologic response of Lakes Lahontan and Bonneville and the mountain glacial advances were concurrent with the Allerød/Younger Dryas climatic intervals recorded in vegetational and glacial records of western and central Europe.

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Publication type Article
Publication Subtype Journal Article
Title Lake-size variations in the Lahontan and Bonneville basins between 13,000 and 9000 14C yr B.P
Series title Palaeogeography, Palaeoclimatology, Palaeoecology
DOI 10.1016/0031-0182(92)90162-X
Volume 95
Issue 1-2
Year Published 1992
Language English
Publisher Elsevier
Description 14 p.
First page 19
Last page 32
Country United States
State Nevada, Utah
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