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- W1803006936 abstract "We used carbonate clumped isotope thermometry toconstrain growth temperatures of paleosol carbonates andfossil unionid bivalves collected from the Big Horn Basin(Wyoming) from sections that span the Paleocene-Eoceneboundary. Long-term global warming of ~10°C occurred fromthe Late Paleocene to the Early Eocene. The Paleocene-Eocene Thermal Maximum (PETM) is an extreme thermalevent of short duration (< 200 ky) superimposed on the longtermwarming trend, and has been identified globally in theocean sediment record and on the continents in sedimentarybasins. The Big Horn Basin is one such basin that has beenextensively studied with multiple climatic and biotic proxiesin an attempt to characterize the PETM. Therefore, it is anideal case study for the new paleothermometry technique weuse here." @default.
- W1803006936 created "2016-06-24" @default.
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- W1803006936 date "2007-08-01" @default.
- W1803006936 modified "2023-10-15" @default.
- W1803006936 title "Continental temperatures from the Paleocene-Eocene boundary in the Big Horn Basin, WY from carbonate clumped isotope thermometry" @default.
- W1803006936 hasPublicationYear "2007" @default.
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