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Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods

Authors :
Douglas W. Burbank
Patricia Lucia Ciccioli
William H. Amidon
Ricardo N. Alonso
G. Burch Fisher
Perri H Silverhart
Michael S Christoffersen
Andrew L. Gorin
Andrew R.C. Kylander-Clark
Source :
Proceedings of the National Academy of Sciences of the United States of America, vol 114, iss 25, Amidon, WH; Fisher, GB; Burbank, DW; Ciccioli, PL; Alonso, RN; Gorin, AL; et al.(2017). Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 114(25), 6474-6479. doi: 10.1073/pnas.1700327114. UC Santa Barbara: Retrieved from: http://www.escholarship.org/uc/item/28687181, CONICET Digital (CONICET), Consejo Nacional de Investigaciones Científicas y Técnicas, instacron:CONICET
Publication Year :
2017
Publisher :
eScholarship, University of California, 2017.

Abstract

Although Earth's climate history is best known through marine records, the corresponding continental climatic conditions drive the evolution of terrestrial life. Continental conditions during the latest Miocene are of particular interest because global faunal turnover is roughly synchronous with a period of global glaciation from 6.2-5.5 Ma and with the Messinian Salinity Crisis from 6.0-5.3 Ma. Despite the climatic and ecological significance of this period, the continental climatic conditions associated with it remain unclear. We address this question using erosion rates of ancient watersheds to constrain Mio-Pliocene climatic conditions in the south-central Andes near 30° S. Our results show two slowdowns in erosion rate, one from 6.1-5.2 Ma and another from 3.6 to 3.3 Ma, which we attribute to periods of continental aridity. This view is supported by synchrony with other regional proxies for aridity and with the timing of glacial "cold" periods as recorded by marine proxies, such as the M2 isotope excursion. We thus conclude that aridity in the south-central Andes is associated with cold periods at high southern latitudes, perhaps due to a northward migration of the Southern Hemisphere westerlies, which disrupted the South American Low Level Jet that delivers moisture to southeastern South America. Colder glacial periods, and possibly associated reductions in atmospheric CO2, thus seem to be an important driver of Mio-Pliocene ecological transitions in the central Andes. Finally, this study demonstrates that paleo-erosion rates can be a powerful proxy for ancient continental climates that lie beyond the reach of most lacustrine and glacial archives. Fil: Amidon, William H.. Middlebury College; Estados Unidos Fil: Fisher, G. Burch. University of Texas at Austin; Estados Unidos. University of California; Estados Unidos Fil: Burbank, Douglas W.. University of California; Estados Unidos Fil: Ciccioli, Patricia Lucia. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Alonso, Ricardo Narciso. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Tucumán. Instituto Superior de Correlación Geológica. Grupo Vinculado al INSUGEO- Centro de Estudios Geologicos Andinos; Argentina Fil: Gorin, Andrew L.. Middlebury College; Estados Unidos Fil: Silverhart, Perri H.. Middlebury College; Estados Unidos Fil: Kylander Clark, Andrew R.C.. University of California; Estados Unidos Fil: Christoffersen, Michael S.. University of Texas at Austin; Estados Unidos

Details

Database :
OpenAIRE
Journal :
Proceedings of the National Academy of Sciences of the United States of America, vol 114, iss 25, Amidon, WH; Fisher, GB; Burbank, DW; Ciccioli, PL; Alonso, RN; Gorin, AL; et al.(2017). Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 114(25), 6474-6479. doi: 10.1073/pnas.1700327114. UC Santa Barbara: Retrieved from: http://www.escholarship.org/uc/item/28687181, CONICET Digital (CONICET), Consejo Nacional de Investigaciones Científicas y Técnicas, instacron:CONICET
Accession number :
edsair.doi.dedup.....c90468f24b2580737ae13792e7340bc7