Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods.
| Autor: | Amidon WH; Geology Department, Middlebury College, Middlebury, VT 05753; wamidon@middlebury.edu., Fisher GB; Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78712.; Earth Research Institute, University of California, Santa Barbara, CA 93106., Burbank DW; Earth Research Institute, University of California, Santa Barbara, CA 93106., Ciccioli PL; 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., Alonso RN; Instituto Superior de Correlación Geológica, Universidad Nacional de Salta-Consejo Nacional de Investigaciones Científicas y Técnicas, 4400 Salta, Argentina., Gorin AL; Geology Department, Middlebury College, Middlebury, VT 05753., Silverhart PH; Geology Department, Middlebury College, Middlebury, VT 05753., Kylander-Clark ARC; Earth Research Institute, University of California, Santa Barbara, CA 93106., Christoffersen MS; Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78712. |
|---|---|
| Jazyk: | angličtina |
| Zdroj: | Proceedings of the National Academy of Sciences of the United States of America [Proc Natl Acad Sci U S A] 2017 Jun 20; Vol. 114 (25), pp. 6474-6479. Date of Electronic Publication: 2017 Jun 12. |
| DOI: | 10.1073/pnas.1700327114 |
| Abstrakt: | 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 CO Competing Interests: The authors declare no conflict of interest. |
| Databáze: | MEDLINE |
| Externí odkaz: |
|