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dc.contributor.authorAli, Guleed Ahmed Husseinen_US
dc.contributor.authorLin, Keen_US
dc.contributor.authorHemming, Sidney R.en_US
dc.contributor.authorCox, Stephen E.en_US
dc.contributor.authorRuprecht, Philippen_US
dc.contributor.authorZimmerman, Susan R. H.en_US
dc.contributor.authorStine, Scotten_US
dc.contributor.authorWang, Xianfengen_US
dc.identifier.citationAli, G. A. H., Lin, K., Hemming, S. R., Cox, S. E., Ruprecht, P., Zimmerman, S. R. H., Stine, S. & Wang, X. (2022). Emergence of wet conditions in the Mono Basin of the western USA coincident with inception of the Last Glaciation. GSA Bulletin, 134(9-10), 2267-2279.
dc.description.abstractAt present, the Basin and Range of the western USA is arid, but geologic studies show evidence of past wetness. The timing of these wetter conditions reveals a close association with glacial conditions. This association has led to the hypothesis of a causal link between glacial climate and regional wetness, but poor age control on the onset of regional wetness thwarts a test of this hypothesis. Here we determine the start of the most recent interval of persistent wetness in the Mono Basin, which is a hydrologically closed depression that sits at the west-central edge of the Basin and Range. The most recent emergence of persistent wetness in the Mono Basin is stratigraphically correlated with the depositional age of Ash 19—a rhyolitic ash bed that represents the oldest tephra of the Wilson Creek Formation and one of the earliest-known products of explosive volcanic activity from the Mono Craters. We constrain the depositional age of Ash 19 by using the U/Th disequilibrium dating method to date carbonates that are younger and older than Ash 19. Our U/Th dating results show that Ash 19 was deposited before the formation of a cross-cutting carbonate bed dated to 69.2 ± 0.3 ka but after an underlying carbonate tufa dated to 67.4 ± 3.5 ka, which suggests that the start of wetness in the Mono Basin was contemporary with the inception of the Last Glaciation—the beginning of Marine Isotope Stage 4—at ca. 70 ka. This finding corroborates the hypothesis of a link between glacial climate and regional wetness.en_US
dc.description.sponsorshipMinistry of Education (MOE)en_US
dc.relation.ispartofGSA Bulletinen_US
dc.rights© 2021 Geological Society of America. All rights reserved.en_US
dc.titleEmergence of wet conditions in the Mono Basin of the western USA coincident with inception of the Last Glaciationen_US
dc.typeJournal Articleen
dc.contributor.schoolAsian School of the Environmenten_US
dc.contributor.researchEarth Observatory of Singaporeen_US
dc.subject.keywordsNorth-Atlantic Climateen_US
dc.description.acknowledgementThis research was supported by the Gary Comer Science and Education Foundation and the Lamont-Doherty Earth Observatory Climate Center. Financial support from the Ford Foundation aided in the writing of this manuscript. X.W. acknowledges support from the Singapore Ministry of Education (grant nos. MOE2019-T2-1-1744 and RG13/20) and the Earth Observatory of Singapore.en_US
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