000126988 001__ 126988
000126988 005__ 20241125101148.0
000126988 0247_ $$2doi$$a10.1016/j.quascirev.2023.108234
000126988 0248_ $$2sideral$$a134350
000126988 037__ $$aART-2023-134350
000126988 041__ $$aeng
000126988 100__ $$0(orcid)0000-0002-0041-0507$$aAlfaro-Ibáñez, M.P.$$uUniversidad de Zaragoza
000126988 245__ $$aImplications of population changes among the Arvicolinae (Rodentia, Mammalia) in El Mirón Cave (Cantabria, Spain) for the climate of the last c. 50,000 years
000126988 260__ $$c2023
000126988 5060_ $$aAccess copy available to the general public$$fUnrestricted
000126988 5203_ $$aThe El Mirón Cave site in Spain has one of the most complete archaeological and palaeontological records of the Late Pleistocene in the Iberian Peninsula, encompassing most of the last c. 50,000 years. Among other studies, the fossiliferous record has allowed the development of various interpretations of faunal and climatic changes during this period of time in the northern Atlantic region of the Iberian Peninsula. The addition of more radiocarbon dates from El Mirón Cave make it possible to revise some of the interpretations of the micromammal sequence carried out earlier for this major site. The record of small mammals is one of the most used tools to study the climate of the past, and among them the several Arvicolinae species are of great importance for the study of Quaternary climatic variations, due to their adaptations to a great diversity of habitats. New methodologies such as ancient DNA and geometric morphometric analyses now permit us to conduct a review of the Arvicolinae species previously described at this site and better to differentiate between species with similar morphologies, like Microtus arvalis and M. agrestis. We also identified the presence of a species not recorded before in El Mirón, Terricola pyrenaicus. With the study of the Arvicolinae species associations, we reaffirm the climate variations originally described in this deposit, indicating in detail how the successive changes in temperature and environment took place throughout the course of the late Last Glacial and early Postglacial periods (Marine Isotope Stages 3–1).
000126988 536__ $$9info:eu-repo/grantAgreement/ES/MCIU/FPU20-02031$$9info:eu-repo/grantAgreement/ES/MICINN-AEI-FEDER/PGC2018-093925-B-C33
000126988 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000126988 590__ $$a3.2$$b2023
000126988 592__ $$a1.558$$b2023
000126988 591__ $$aGEOGRAPHY, PHYSICAL$$b16 / 65 = 0.246$$c2023$$dQ1$$eT1
000126988 593__ $$aArcheology$$c2023$$dQ1
000126988 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b70 / 254 = 0.276$$c2023$$dQ2$$eT1
000126988 593__ $$aArcheology (arts and humanities)$$c2023$$dQ1
000126988 593__ $$aGlobal and Planetary Change$$c2023$$dQ1
000126988 593__ $$aGeology$$c2023$$dQ1
000126988 593__ $$aEcology, Evolution, Behavior and Systematics$$c2023$$dQ1
000126988 594__ $$a7.5$$b2023
000126988 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000126988 700__ $$0(orcid)0000-0001-5125-9651$$aCuenca-Bescós, G.$$uUniversidad de Zaragoza
000126988 700__ $$0(orcid)0000-0003-2942-2840$$aBover, P.
000126988 700__ $$aGonzález Morales, M.
000126988 700__ $$aStraus, L.G.
000126988 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000126988 773__ $$g315 (2023), 108234 [14 pp.]$$pQuat. sci. rev.$$tQUATERNARY SCIENCE REVIEWS$$x0277-3791
000126988 8564_ $$s11308849$$uhttps://zaguan.unizar.es/record/126988/files/texto_completo.pdf$$yVersión publicada
000126988 8564_ $$s2532554$$uhttps://zaguan.unizar.es/record/126988/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000126988 909CO $$ooai:zaguan.unizar.es:126988$$particulos$$pdriver
000126988 951__ $$a2024-11-22-12:05:12
000126988 980__ $$aARTICLE