4.4 Article

Pliocene to middle Pleistocene in Uruguay: A model of climate evolution

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QUATERNARY INTERNATIONAL
卷 210, 期 -, 页码 37-43

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PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quaint.2009.08.011

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  1. Commission of Scientific Research (CSIC) of Uruguay

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The identification of sedimentary deposits containing probable Ensenadan Stage/Age (0.5-1.8 Ma) fossil remains in several points of the Rio de la Plata basin, Uruguay, allows positioning of some geological events in stratigraphic order. These events are indicators of important climate changes that occurred during the Late Pliocene, and Early and Middle Pleistocene. The dataset obtained in this research identifies the occurrence of and climate during the Early Pleistocene. At this time, the deposition of the loessic San Bautista Member (new name) of the Raigon Formation, containing Cardiatherium talicei, took place. The overlying Libertad Formation includes a sequence of paleosols developed on the loess sediments that formed in a climate much warmer and more humid than the present one. In comparison with the delta O-18 marine isotopic stage curve, the highest temperatures during the period were recorded at around 1.7 +/- 0.1 Ma. At this time, abundant Ensenadan vegetation and megafauna components occurred in the Rio de La Plata region, but disappeared towards 0.6 Ma, in coincidence with the significant glaciations that took place in the Southern Hemisphere. Several aspects of the revision of the Quaternary stratigraphy and paleoclimates in Uruguay are examined, using new criteria, field observations and global comparisons. (C) 2009 Elsevier Ltd and INQUA. All rights reserved.

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