Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/2225
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dc.contributor.authorMirea, Ionuţ-Cornel-
dc.contributor.authorRobu, Marius-
dc.contributor.authorPetculescu, Alexandru-
dc.contributor.authorKenesz, Marius-
dc.contributor.authorFaur, Luchiana-
dc.contributor.authorArghir, Răzvan Adrian-
dc.contributor.authorTecsa, Viorica-
dc.contributor.authorTimar-Gabor, Alida-
dc.contributor.authorRoban, Relu Dumitru-
dc.contributor.authorPanaiotu, Cristian G.-
dc.contributor.authorSharifi, Arash-
dc.contributor.authorPourmand, Ali-
dc.contributor.authorCodrea, Vlad A‏.-
dc.contributor.authorConstantin, Silviu-
dc.date.accessioned2021-01-11T18:07:14Z-
dc.date.issued2021-01-
dc.identifier.citationPalaeogeography, Palaeoclimatology, Palaeoecology, 2021, 562, 110084es_ES
dc.identifier.issn0031-0182-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/2225-
dc.description.abstractCaves often hold valuable palaeoclimate archives including speleothems, fossil remains, and clastic sediments that complement each other. This paper presents a multi-archive interdisciplinary study of an extensive deposit of fossil mammals from the scientific reserve in the Muierilor Cave, Southern Carpathians, Romania. We present two new palaeontological excavations that indicate a high abundance and diversity of MIS 3–2 fossil mammals (carnivores, omnivores and herbivores) synchronous with the early modern humans known from this cave. Using geochronological and sedimentological methods, we present a general reconstruction of the cave evolution between ~120 kyr B.P. and the Holocene. The study is based on a combination of geochronological tools including OSL dating of sediments, U/Th dating of speleothems, and radiocarbon dating of fossil remains, with a total of 54 ages. Based on U/Th dating of speleothems from stratigraphically-relevant positions, we show that the MIS 3 assemblage of fossil mammals were massively reworked and deposited during the post-LGM deglaciation, slightly earlier than previously known for the Southern Carpathians. On the other hand, several young radiocarbon ages of cave bear samples suggest that the Southern Carpathians might have been functioning as a glacial refuge for this species as late as ~22 kyr B.P.es_ES
dc.description.sponsorshipThis research involved systematic excavation and research over the last seven years and therefore benefited from several sources of funding. It was initially supported through a National Geographic Grant (#964115) and further on through grants PCE 197/2016 (CARPATHEMS), and EEA 126/2018 (KARSTHIVES2), all to S. Constantin and RU-TE 2301/2014 (PALEOCLIM) to A. Petculescu. The support through grant PN-III-P4-ID-PCCF-2016-0016 (DARKFOOD, to O.T. Moldovan) is also acknowledged. We are grateful to Stelian Grigore, Cristinel Fofirică, Arthur Dăscălescu, Marius Iliescu (“Hades” Caving Club, Romania), the discoverers of the Hades Passage, for providing the base map of the cave and for insightful discussions.es_ES
dc.language.isoenes_ES
dc.publisherElsevieres_ES
dc.rightsinfo:eu-repo/semantics/embargoedAccesses_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectCave bearses_ES
dc.subjectCave genesises_ES
dc.subjectMIS 3–2 faunaes_ES
dc.subjectLGMes_ES
dc.subjectRomanian Carpathianses_ES
dc.titleLast deglaciation flooding events in the Southern Carpathians as revealed by the study of cave deposits from Muierilor Cave, Romaniaes_ES
dc.typeArticlees_ES
dc.identifier.doi10.1016/j.palaeo.2020.110084-
dc.relation.publisherversionhttps://doi.org/10.1016/j.palaeo.2020.110084es_ES
dc.date.available2021-01-11T18:07:14Z-
Appears in Collections:Geocronología y Geología



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