2015
DOI: 10.1016/j.jsames.2014.12.003
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Late Pleistocene lithostratigraphy and sequences in the southwestern Mesopotamia (Argentina): Evidences of the last interglacial stage

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Cited by 26 publications
(11 citation statements)
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References 54 publications
(78 reference statements)
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“…The holotype comes from the Talara Tar Seeps in Peru, from the Late Pleistocene, Mancora Tablazo terrace. Records of this taxon from Argentina correspond to those coming from the Late Pleistocene-Early Holocene, Salto Ander Egg Formation (following Brunetto et al, 2015) outcropping in Ensenada and Barrenechea rivers in Entre Ríos Province (Noriega & Areta, 2005); and also, from the left margin of Arroyo Chasicó, Pleistocene sensu lato, Buenos Aires Province (Tambussi & Noriega, 1999). Genus Buteo Lacépède, 1799 Type species.…”
Section: Geronogyps Reliquusmentioning
confidence: 82%
“…The holotype comes from the Talara Tar Seeps in Peru, from the Late Pleistocene, Mancora Tablazo terrace. Records of this taxon from Argentina correspond to those coming from the Late Pleistocene-Early Holocene, Salto Ander Egg Formation (following Brunetto et al, 2015) outcropping in Ensenada and Barrenechea rivers in Entre Ríos Province (Noriega & Areta, 2005); and also, from the left margin of Arroyo Chasicó, Pleistocene sensu lato, Buenos Aires Province (Tambussi & Noriega, 1999). Genus Buteo Lacépède, 1799 Type species.…”
Section: Geronogyps Reliquusmentioning
confidence: 82%
“…In these latitudes, high-stand sea levels correlate with humid periods typical of interglacial cycles. The stages characterized by higher sea levels can be correlated with the periods of accumulation of the fluvial deposits recorded on terraces in the tributaries of the distal area of the continental fluvial system Paraná-Río de la Plata (Brunetto et al, 2015). That is due to the fact that the sea level is the base level of M A N U S C R I P T…”
Section: Locality and Stratigraphical Provenancementioning
confidence: 88%
“…This is a reasonable criterion for establishing a chronological correlation of the fluvial sediments that compose the terraces located inside the fluvial valleys, with the Marine Isotopic Stages (Jouzel et al, 2007;Rohling et al, 2008). There are OSL datings (120 ka -ka) obtained from the higher fluvial terraces in neighbor areas, which indicate these levels were deposited over the Last Interglacial Stage (Brunetto et al, 2015;Ferrero et al, 2017).…”
Section: Locality and Stratigraphical Provenancementioning
confidence: 99%
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“…Within the valleys, the Tezanos Pinto Formation is represented by alluvial and fluvial facies. One OSL dating for the alluvial facies gave an age of 33,000 years (Ferrero 2009) and the fossil record is restricted to Smilodon populator (Ferrero 2013;Ferrero et al 2015;Brunetto et al 2015).…”
Section: Introductionmentioning
confidence: 99%