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Climatic changes during the Plio-Pleistocene transition as recorded by the isotopic composition of pedogenic carbonates

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dc.creatorBeilinson, Elisa
dc.creatorRaigemborn, María Sol
dc.creatorSosa, Numa Nahuel
dc.date.issued2019
dc.description.abstractPlio-Pleistocene continental deposits in south-eastern Buenos Aires province (Argentina), correspond to fluvioalluvial deposits interbedded with palaeosols. The Pliocene units show little participation of carbonatic features in their palaeosols, which are classified as Argillisols. The late Pliocene-Pleistocene palaeosols show a much higher participation of pedogenic carbonates and are classified as Calcisols. Could this change from Argillisols to Calcisols be related to the global-scale climatic change during the Plio-Pleistocene boundary?
dc.identifierClimatic changes during the Plio-Pleistocene transition as recorded by the isotopic composition of pedogenic carbonates; 20th INQUA Congress; Dublin; Irlanda; 2019; 2731-2731
dc.identifierhttp://hdl.handle.net/11336/175227
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://naturalis.fcnym.unlp.edu.ar/handle/628872547/57350
dc.languageeng
dc.publisherIrish Quaternary Association
dc.relationinfo:eu-repo/semantics/altIdentifier/url/http://iqua.ie/wp-content/uploads/2020/02/INQUA-2019-Abstract-book.pdf
dc.relationinfo:eu-repo/semantics/altIdentifier/url/http://iqua.ie/inqua-2019-delegates/
dc.sourceAbstract Book for INQUA 2019
dc.subjectCLIMATE
dc.subjectISOTOPES
dc.subjectPLIO-PLEISTOCENE
dc.titleClimatic changes during the Plio-Pleistocene transition as recorded by the isotopic composition of pedogenic carbonates
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeinfo:eu-repo/semantics/conferenceObject
dc.typeinfo:ar-repo/semantics/documento de conferencia
dspace.entity.typePublication

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