Titlebook: Marine Isotope Stage 3 in Southern South America, 60 KA B.P.-30 KA B.P.; Germán Mariano Gasparini,Jorge Rabassa,Eduardo Ped Book 2016 Spri

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Paleogeographic Evolution of the Atlantic Coast of South America During Marine Isotope Stage 3 (MISpproximate reconstruction of the paleogeographic evolution of the Atlantic coast of South America during the Marine Isotopic Stage 3 (MIS 3). To elaborate this digital model, the curve of global sea level variations as proposed by Lambeckand Chappell (.), for the last glacial cycle, was taken into c

Palpitation

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Marine Isotope Stage 3 (MIS 3) and Continental Beds from Northern Uruguay (Sopas Formation): Paleong the predominant taxa. Likely, relationships with the Last Interglacial Stage or with the Last Interstadial were proposed. The paleontological content of the Sopas Formation is updated, and the climatic and environmental signals provided by the fossil content are evaluated. Radiocarbon AMS dates ra

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Continental Vertebrates During the Marine Isotope Stage 3 (MIS 3) in Argentina,n. This situation is mainly due to the lack of absolute ages for Pleistocene fossil remains or their bearing sediments that would allow the verification of the chronology established for this interval. However, a few isolated evidences show that continental vertebrates responded to the abrupt temper

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Marine Isotope Stage 3 (MIS 3) Versus Marine Isotope Stage 5 (MIS 5) Fossiliferous Marine Deposits ethods. While .C datings suggest younger ages (related to Marine Isotope Stage 3—MIS 3), OSL, where available, indicate older times (related to Marine Isotope Stage 5—MIS 5). The analysis of the abundant molluscan fauna and the presence of extralimital warm water taxa points to a higher than present

Induction

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