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

L. Benson; D. Currey; Y. Lao; S. Hostetler

doi:10.1016/0031-0182(92)90162-x

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

L. Benson·D. Currey·Y. Lao·S. Hostetler

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Abstract

Recessions of Lakes Lahontan and Bonneville that commenced ∼13,500 14 C yr B.P. were interrupted at ⪖11,500 14 C yr B.P. in the Lahontan basin and ∼12,200 14 C 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 14 C 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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Palaeogeography, Palaeoclimatology, Palaeoecology Article

Source-reported bounding extent: 35.539763811049966° to 41.93213402280034° latitude; -120.24126133487317° to -109.08190736391086° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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L. Benson, D. Currey, Y. Lao, S. Hostetler. 1992. Lake-size variations in the Lahontan and Bonneville basins between 13,000 and 9000 14C yr B.P. https://doi.org/10.1016/0031-0182(92)90162-x

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