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Paleoenvironment and paleoecology associated with the early phases of the Great American Biotic Interchange based on stable isotope analysis of fossil mammals and new U–Pb ages from the Pampas of Argentina

dc.contributor.authorSanz Pérez, Danae
dc.contributor.authorMontalvo, Claudia
dc.contributor.authorMehl, Adriana
dc.contributor.authorTomassini, Rodrigo
dc.contributor.authorHernández Fernández, Manuel
dc.contributor.authorDomingo Martínez, Laura
dc.date.accessioned2023-12-20T18:23:30Z
dc.date.available2023-12-20T18:23:30Z
dc.date.issued2024
dc.description.abstractThe analysis of stable isotopes in fossil mammals is useful for reconstructing paleoenvironmental and paleoecological conditions, but has been rarely applied to the Neogene of South America. In this study, we perform an integrative analysis (including U–Pb zircon dates and mammalian stable isotopes data) for the Late Miocene–Early Pliocene of central Argentina. We provide radioisotopic ages for some classic fossiliferous localities in this region, including an age of 9.7 ± 0.3 Ma for Arroyo Chasicó and 4.5 ± 0.2 Ma for Farola Monte Hermoso, and address the interval covering the Chasicoan (Late Miocene), Huayquerian (Late Miocene–Early Pliocene), and Montehermosan (Early Pliocene) stages/ages. In the Chasicoan Stage/Age, taxa with mixed C3–C4 diets are recorded, suggesting the existence of favorable conditions for the C4 photosynthetic pathway before its full expansion. However, taxa represented across most of the Huayquerian Stage/Age show a preference for C3–based diets, which changes in the latest Huayquerian–Montehermosan stages/ages when an increase in the percentage of C4 plants in the diet of notoungulates, rodents, and xenarthrans is recorded, coinciding with the global expansion of C4 plants. For the first time, the dietary behavior of two South American endemic sparassodont metatherians (Lycopsis and Thylacosmilus) has been evaluated from using stable isotope; analysis of these hypercarnivores show differences in δ13C values, suggesting prey partitioning, partly due to the difference in body size. The fossiliferous sites studied, and the new isotopic and chronological information obtained, provide more detailed paleoecological and paleoenvironmental contexts for the Argentine Pampas during the last stages of the isolation of South America and the first pulses of the Great Biotic American Interchange. In addition, the new ages allow to better adjust the arrival of the first Holarctic immigrants in the region.eng
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipMinisterio de Ciencia e Innovación (España)
dc.description.sponsorshipUniversidad Nacional de La Pampa (Argentina)
dc.description.sponsorshipUniversidad Nacional del Sur (Argentina)
dc.description.sponsorshipWaitt Foundation
dc.description.sponsorshipSantander Universidades
dc.description.sponsorshipUniversidad Complutense de Madrid
dc.description.statuspub
dc.identifier.citationSanz-Pérez, Dánae, et al. «Paleoenvironment and Paleoecology Associated with the Early Phases of the Great American Biotic Interchange Based on Stable Isotope Analysis of Fossil Mammals and New U–Pb Ages from the Pampas of Argentina». Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 634, enero de 2024, p. 111917. https://doi.org/10.1016/j.palaeo.2023.111917.
dc.identifier.doi10.1016/j.palaeo.2023.111917
dc.identifier.essn1872-616X
dc.identifier.issn0031-0182
dc.identifier.officialurlhttps://doi.org/10.1016/j.palaeo.2023.111917
dc.identifier.relatedurlhttps://www.sciencedirect.com/science/article/pii/S0031018223005357
dc.identifier.urihttps://hdl.handle.net/20.500.14352/91635
dc.issue.number111917
dc.journal.titlePalaeogeography, Palaeoclimatology, Palaeoecology
dc.language.isoeng
dc.publisherElsevier
dc.relation.projectIDinfo:eu-repo/grantAgreement/PGC2018–094955–A–I00
dc.relation.projectIDinfo:eu-repo/grantAgreement/PID2020-116220GB-I00
dc.relation.projectIDinfo:eu-repo/grantAgreement/PID2022-138275NB-I00
dc.relation.projectID13G, 21G projects
dc.relation.projectIDinfo:eu-repo/grantAgreement/PGI24H/154
dc.relation.projectIDinfo:eu-repo/grantAgreement/PRE2019–089848
dc.relation.projectIDinfo:eu-repo/grantAgreement/W467–16
dc.relation.projectIDinfo:eu-repo/grantAgreement/UCM-910607
dc.rightsAttribution-NonCommercial 4.0 Internationalen
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/
dc.subject.cdu56:574(82)
dc.subject.keywordCarbon
dc.subject.keywordOxygen
dc.subject.keywordRadiometric dating
dc.subject.keywordMiocene
dc.subject.keywordPliocene
dc.subject.keywordSouth America
dc.subject.ucmPaleontología
dc.subject.unesco2416.05 Paleontología de Los Vertebrados
dc.titlePaleoenvironment and paleoecology associated with the early phases of the Great American Biotic Interchange based on stable isotope analysis of fossil mammals and new U–Pb ages from the Pampas of Argentina
dc.typejournal article
dc.type.hasVersionVoR
dc.volume.number634
dspace.entity.typePublication
relation.isAuthorOfPublication7516423a-9940-471e-b25f-8da84bdc7b74
relation.isAuthorOfPublicationd7d8897f-0be5-4679-a9a1-87e0ef379cc1
relation.isAuthorOfPublication1c4f2451-bfbf-47b0-8493-e6d180dcba84
relation.isAuthorOfPublication.latestForDiscovery7516423a-9940-471e-b25f-8da84bdc7b74

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