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Proc Natl Acad Sci U S A. 2017 Jun 20;114(25):6474-6479. doi: 10.1073/pnas.1700327114. Epub 2017 Jun 12.

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

Author information

1
Geology Department, Middlebury College, Middlebury, VT 05753; wamidon@middlebury.edu.
2
Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78712.
3
Earth Research Institute, University of California, Santa Barbara, CA 93106.
4
Departamento de Ciencias Geológicas, Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires-Consejo Nacional de Investigaciones Científicas y Técnicas, Buenos Aires C1428EHA, Argentina.
5
Instituto Superior de Correlación Geológica, Universidad Nacional de Salta-Consejo Nacional de Investigaciones Científicas y Técnicas, 4400 Salta, Argentina.
6
Geology Department, Middlebury College, Middlebury, VT 05753.

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.

KEYWORDS:

M2; Messinian; Miocene; Pliocene; precipitation

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