中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Moisture availability and groundwater recharge paced by orbital forcing over the past 750,000 years in the southwestern USA

文献类型:期刊论文

作者Steidle, Simon D.4; Wendt, Kathleen A.3; Dublyansky, Yuri4; Edwards, R. Lawrence2; Li, Xianglei1,2; Mcclure, Gracelyn2; Moseley, Gina E.4; Spoetl, Christoph4
刊名COMMUNICATIONS EARTH & ENVIRONMENT
出版日期2024-07-14
卷号5期号:1页码:9
DOI10.1038/s43247-024-01550-0
通讯作者Steidle, Simon D.(simonsteidlescience@gmail.com)
英文摘要Quaternary climate changes are driven in part by variations in the distribution and strength of insolation due to orbital parameters. Continental climate variability is well documented for the most recent glacial-interglacial cycles, yet few records extend further back in time. Such records are critically needed to comprehensively assess the entire spectrum of natural climate variability against the backdrop of anthropogenic warming. Here, we apply uranium isotope geochronology to calcite deposits to date groundwater-table changes in Devils Hole cave, Nevada. The deposits record multi-meter groundwater-table fluctuations over the last 750,000 years, reflecting the long-term evolution of hydroclimate in this presently arid region. During periods between glacial or interglacial extremes, the water table responded sensitively to variations in 65 degrees N summer insolation, likely caused by the increasing extent of North American ice sheets during cold period, which steered moisture-laden trajectories towards the southwestern USA. These orbitally-driven hydroclimatic changes are superimposed on a tectonically-driven long-term decline in the regional groundwater table observed prior to 438,000 +/- 14,000 years ago. The paleo water table in the southwestern United States records global climatic shifts such as variations in the Northern Hemisphere summer insolation, shown by U-series and U-Th geochronology on calcite deposits in Nevada, USA.
WOS关键词LAST GLACIAL MAXIMUM ; NORTH-AMERICAN MONSOON ; DEVILS-HOLE ; CLIMATE RECORD ; CALCITE ; TH-230 ; NEVADA ; WATER ; AGES
资助项目Austrian Science Fund (Fonds zur Frderung der Wissenschaftlichen Forschung)[P263050] ; Austrian Science Fund (Fonds zur Frderung der Wissenschaftlichen Forschung)[P327510] ; Austrian Science Fund (Fonds zur Frderung der Wissenschaftlichen Forschung)[DEVA-2017-SCI-0002] ; Austrian Science Fund (Fonds zur Frderung der Wissenschaftlichen Forschung)[DEVA-2015-SCI-0006] ; Austrian Science Fund (FWF) ; Heising-Simons Foundation[2202913] ; NSF
WOS研究方向Environmental Sciences & Ecology ; Geology ; Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:001270859500001
出版者SPRINGERNATURE
资助机构Austrian Science Fund (Fonds zur Frderung der Wissenschaftlichen Forschung) ; Austrian Science Fund (FWF) ; Heising-Simons Foundation ; NSF
源URL[http://119.78.100.205/handle/311034/24000]  
专题中国科学院古脊椎动物与古人类研究所
通讯作者Steidle, Simon D.
作者单位1.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing, Peoples R China
2.Univ Minnesota, Sch Earth & Environm Sci, Minneapolis, MN USA
3.Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR USA
4.Univ Innsbruck, Inst Geol, Innsbruck, Austria
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GB/T 7714
Steidle, Simon D.,Wendt, Kathleen A.,Dublyansky, Yuri,et al. Moisture availability and groundwater recharge paced by orbital forcing over the past 750,000 years in the southwestern USA[J]. COMMUNICATIONS EARTH & ENVIRONMENT,2024,5(1):9.
APA Steidle, Simon D..,Wendt, Kathleen A..,Dublyansky, Yuri.,Edwards, R. Lawrence.,Li, Xianglei.,...&Spoetl, Christoph.(2024).Moisture availability and groundwater recharge paced by orbital forcing over the past 750,000 years in the southwestern USA.COMMUNICATIONS EARTH & ENVIRONMENT,5(1),9.
MLA Steidle, Simon D.,et al."Moisture availability and groundwater recharge paced by orbital forcing over the past 750,000 years in the southwestern USA".COMMUNICATIONS EARTH & ENVIRONMENT 5.1(2024):9.

入库方式: OAI收割

来源:古脊椎动物与古人类研究所

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