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- W2017865819 abstract "Spatially extensive paleoelevation records of the Altiplano plateau are critical to determining the geodynamic mechanisms that formed and support high elevations over a broad area. Prior stable isotope data reveal a climate history for the northern Bolivian Altiplano that has been interpreted to show rapid surface uplift of 2.5±1.0km between ∼10and6Ma. This study applies clumped isotope paleothermometry to paleosol carbonates formed at both a low-elevation site and temporally overlapping high-elevation sites in the southern Altiplano/Eastern Cordillera during the middle to late Miocene. Surface paleotemperature decreased by 14 °C in the southern Altiplano/Eastern Cordillera relative to stable low-elevation paleotemperatures, implying surface elevation increase of 1.9±0.7km between 16 and 13 Ma and an additional 0.7±0.6km between 13 and 9 Ma. Both the large magnitude of surface temperature decrease and earlier onset (7±4Myr) in the south as compared to the north suggest rapid elevation increase by piecemeal removal of lower lithosphere beneath the plateau and possible northward lower crustal flow." @default.
- W2017865819 created "2016-06-24" @default.
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- W2017865819 date "2014-05-01" @default.
- W2017865819 modified "2023-10-15" @default.
- W2017865819 title "Clumped isotope evidence for diachronous surface cooling of the Altiplano and pulsed surface uplift of the Central Andes" @default.
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- W2017865819 doi "https://doi.org/10.1016/j.epsl.2014.02.029" @default.
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