2010
DOI: 10.1038/ngeo707
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Moisture variability in the southwestern United States linked to abrupt glacial climate change

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Cited by 211 publications
(223 citation statements)
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“…A warm and arid period began around 13,000 14 C yBP (15,000 cal BP), culminating in a severe drought that coincided with mammoth extinction and Clovis occupation of the SPV (10,900 14 C yBP or 12,800 cal BP) (18). Immediately thereafter, the Younger Dryas (YD) period brought a return to cool, wet conditions (19) and deposition of an organic-rich "black mat" over the Clovis-age landscape (18).…”
mentioning
confidence: 99%
“…A warm and arid period began around 13,000 14 C yBP (15,000 cal BP), culminating in a severe drought that coincided with mammoth extinction and Clovis occupation of the SPV (10,900 14 C yBP or 12,800 cal BP) (18). Immediately thereafter, the Younger Dryas (YD) period brought a return to cool, wet conditions (19) and deposition of an organic-rich "black mat" over the Clovis-age landscape (18).…”
mentioning
confidence: 99%
“…The additional paleoclimate records, used for comparison are found denoted by the black stars and circles. Data from previous studies includes a ΔP-ET proxy using ( 234 U/ 238 U) 0 for pedogenic carbonates from Wind River, Wyoming (WR) (Sharp et al, 2003), deep vadose zone opal from Yucca Mountain (YM) (Paces et al, 2010) and pedogenic opal from Diamond Valley, Nevada (DV), Newark Valley, Nevada (NV), Fish Lake Valley, Nevada (FLV) and Barstow, California (BA) (Maher et al, in prep); vein calcite from Devils Hole, Nevada (DH) (Winograd et al, 2006); speleothem from Cave of the Bells, Arizona (COB) (Wagner et al, 2010); and the timing of lake highstands at Lake Bonneville, Utah (Oviatt et al, 1992); Lake Lahontan, Nevada (Adams and Wesnousky, 1998); Lake Newark, Nevada (Kurth et al, 2011); Lake Diamond, Nevada (Tackman, 1993); Lake Jakes Lake, Nevada (Garcia and Stokes, 2006); Lake Manly, California (Ku et al, 1998) and Searles Lake, California (Lin et al, 1998).…”
Section: Late Pleistocene Pluvial Lakes In Western North Americamentioning
confidence: 99%
“…Many authors have postulated a southward deflection of the jet stream and westerly storm tracks with increasing growth of the Laurentide and Cordilleran ice sheets (Negrini, 2002;Benson et al, 1990;Adams and Wesnousky, 1998;Zic et al, 2002). Interpretations of several speleothem records, such as the Cave of the Bells record (Wagner et al, 2010) presented in Figure 10 have also invoked the shifting westerly winds as the atmospheric connection between increased rainfall and increased ice sheet extent (Oster et al, 2009;Asmeron et al, 2010). ka (Toggweiller et al, 2006;Lamy et al, 2007).…”
Section: Recordsmentioning
confidence: 99%
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