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To test the hypothesis of high elevations during the late Mesozoic, we used carbonate clumped isotope thermometry to determine the temperature contrast between Late Cretaceous to Paleocene carbonates atop the putative plateau in Nevada versus carbonates from relatively low paleoelevation central Utah site.
Lacustrine carbonates from the Nevada site preserve summer temperatures ∼13 °C cooler than summer temperatures from paleosol carbonates from the Utah site, after correcting for ∼1.2 °C of secular climatic cooling between the times of carbonate deposition at the two sites.
Our opinions are unbiased and unfiltered, and we never hold back. You will provide credit card and personal information only to CCBill's secure site.Your information is transmitted via encryption between you and payment system.Three strong, independent Israeli-Palestinian women try to square their liberated, hedonistic lifestyles with the stultifying restrictions of conservative family life, in Maysaloun Hamoud's charming and vital drama. We follow a rave DJ instigator rigging up decks in abandoned warehouses, a nosebleed 'techno tourist' who chases the hardcore around Europe and a girl addicted to... During the Late Cretaceous, central Nevada may have been a high elevation plateau, the Nevadaplano; some geodynamic models of the western US require thickened crust and high elevations during the Mesozoic to drive the subsequent tectonic events of the Cenozoic while other models do not.