Age and paleoclimatic significance of late Holocene lakes in the Carson Sink, NV, USA

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• 作者：Adams ; Kenneth D.
• 关键词：Lake Lahontan ; Great Basin ; late Holocene ; Fallon Lakes ; paleoclimatology
• 刊名：Quaternary Research
• 出版年：2003
• 出版时间：November, 2003
• 年：2003
• 卷：60
• 期：3
• 页码：294-306
• 全文大小：1.31 M

文摘

New dating in the Carson Sink at the termini of the Humboldt and Carson rivers in the Great Basin of the western United States indicates that lakes reached elevations of 1204 and 1198 m between 915 and 652 and between 1519 and 1308 cal yr B.P., respectively. These dates confirm Morrison's original interpretation (Lake Lahontan: Geology of the Southern Carson Desert, Professional Paper 40, U.S. Geol. Survey, 1964) that these shorelines are late Holocene features, rather than late Pleistocene as interpreted by later researchers. Paleohydrologic modeling suggests that discharge into the Carson Sink must have been increased by a factor of about four, and maintained for decades, to account for the 1204-m lake stand. The hydrologic effects of diversions of the Walker River to the Carson Sink were probably not sufficient, by themselves, to account for the late Holocene lake-level rises. The decadal-long period of increased runoff represented by the 1204-m lake is also reflected in other lake records and in tree ring records from the western United States.