Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods
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 wit...
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00278424_v114_n25_p6475_Amidon http://hdl.handle.net/20.500.12110/paper_00278424_v114_n25_p6475_Amidon |
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paper:paper_00278424_v114_n25_p6475_Amidon2023-06-08T14:54:33Z Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods Ciccioli, Patricia Lucía M2 Messinian Miocene Pliocene Precipitation carbon water Article cold environmental erosion glacial period latitude mass extinction Miocene Pliocene precipitation priority journal salinity sea surface temperature South America Southern Hemisphere vegetation watershed 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:Ciccioli, P.L. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2017 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00278424_v114_n25_p6475_Amidon http://hdl.handle.net/20.500.12110/paper_00278424_v114_n25_p6475_Amidon |
| institution |
Universidad de Buenos Aires |
| institution_str |
I-28 |
| repository_str |
R-134 |
| collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
| topic |
M2 Messinian Miocene Pliocene Precipitation carbon water Article cold environmental erosion glacial period latitude mass extinction Miocene Pliocene precipitation priority journal salinity sea surface temperature South America Southern Hemisphere vegetation watershed |
| spellingShingle |
M2 Messinian Miocene Pliocene Precipitation carbon water Article cold environmental erosion glacial period latitude mass extinction Miocene Pliocene precipitation priority journal salinity sea surface temperature South America Southern Hemisphere vegetation watershed Ciccioli, Patricia Lucía Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods |
| topic_facet |
M2 Messinian Miocene Pliocene Precipitation carbon water Article cold environmental erosion glacial period latitude mass extinction Miocene Pliocene precipitation priority journal salinity sea surface temperature South America Southern Hemisphere vegetation watershed |
| description |
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. |
| author |
Ciccioli, Patricia Lucía |
| author_facet |
Ciccioli, Patricia Lucía |
| author_sort |
Ciccioli, Patricia Lucía |
| title |
Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods |
| title_short |
Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods |
| title_full |
Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods |
| title_fullStr |
Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods |
| title_full_unstemmed |
Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods |
| title_sort |
mio-pliocene aridity in the south-central andes associated with southern hemisphere cold periods |
| publishDate |
2017 |
| url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00278424_v114_n25_p6475_Amidon http://hdl.handle.net/20.500.12110/paper_00278424_v114_n25_p6475_Amidon |
| work_keys_str_mv |
AT cicciolipatricialucia miopliocenearidityinthesouthcentralandesassociatedwithsouthernhemispherecoldperiods |
| _version_ |
1768545962108649472 |