Younger Dryas to early Holocene (12.9 to 8.1 ka) limnological and hydrological change at Barley Lake, California (northern California Coast Range)

被引:4
作者
Leidelmeijer, Jenifer A. [1 ]
Kirby, Matthew E. C. [1 ]
MacDonald, Glen [2 ]
Carlin, Joseph A. [1 ]
Avila, Judith [3 ]
Han, Jiwoo [2 ]
Nauman, Benjamin [2 ]
Loyd, Sean [1 ]
Nichols, Kevin [4 ]
Ramezan, Reza [5 ]
机构
[1] Calif State Univ Fullerton, Dept Geol Sci, 800 North State Coll Blvd, Fullerton, CA 92834 USA
[2] Univ Calif Los Angeles, Dept Geog, 1255 Bunche Hall,Box 951524, Los Angeles, CA 90095 USA
[3] Univ Minnesota, Dept Geog Environm & Soc, 414 Social Sci Bldg, Minneapolis, MN 55455 USA
[4] Calif State Univ Fullerton, Dept Math, 800 North State Coll Blvd, Fullerton, CA 92834 USA
[5] Univ Waterloo, Dept Stat & Actuarial Sci, 200 Univ Ave West, Waterloo, ON N2L 3G1, Canada
基金
美国国家科学基金会;
关键词
California; Younger Dryas; Lakes; Sediment; Grain size; Holocene; Limnology; WESTERN UNITED-STATES; LAST GLACIAL MAXIMUM; SOUTHERN CALIFORNIA; CLIMATE-CHANGE; ORGANIC-MATTER; MAGNETIC-SUSCEPTIBILITY; ATMOSPHERIC RIVERS; KLAMATH MOUNTAINS; ROCKY-MOUNTAINS; POSTGLACIAL VEGETATION;
D O I
10.1017/qua.2021.9
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Paleoperspectives of climate provide important information for understanding future climate, particularly in arid regions such as California, where water availability is uncertain from year to year. Here, we present a record from Barley Lake, California, focusing on the interval spanning the Younger Dryas (YD) to the early Holocene (EH), a period of acute and rapid global climate change. Twelve radiocarbon dates constrain the timing between 12.9 and 8.1 ka. We combine a variety of sediment analyses to infer changes in lake productivity, relative lake level, and runoff dynamics. In general, the lake is characterized by two states separated by a <200-year transition: (1) a variably deep, lower-productivity YD lake; and (2) a two-part variably shallow, higher-productivity EH lake. Inferred EH winter-precipitation runoff reveals dynamic multidecadal-to-centennial-scale variability, in agreement with the EH lake-level data. The Barley Lake archive captures both hemispheric and regional signals of climate change across the transition, suggesting a role for both ocean-atmosphere and insolation forcing. Our paleoperspective emphasizes California's sensitivity to climate change and how that change can generate abrupt shifts in limnological regimes.
引用
收藏
页码:193 / 207
页数:15
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