000088548 001__ 88548
000088548 005__ 20210902121632.0
000088548 0247_ $$2doi$$a10.1016/j.quascirev.2020.106239
000088548 0248_ $$2sideral$$a117186
000088548 037__ $$aART-2020-117186
000088548 041__ $$aeng
000088548 100__ $$aBaca, M.
000088548 245__ $$aDiverse responses of common vole (Microtus arvalis) populations to Late Glacial and Early Holocene climate changes – Evidence from ancient DNA
000088548 260__ $$c2020
000088548 5060_ $$aAccess copy available to the general public$$fUnrestricted
000088548 5203_ $$aThe harsh climatic conditions during the Last Glacial Maximum (LGM) period have been considered the cause of local extinctions and major faunal reorganizations that took place at the end of the Pleistocene. Recent studies have shown, however, that in addition many of these ecological events were associated with abrupt climate changes during the so-called Late Glacial and the Pleistocene/Holocene transition. Here we used ancient DNA to investigate the impact of those changes on European populations of temperate vole species (Microtus arvalis). The genetic diversity of modern populations and the fossil record suggests that the species may have survived cold episodes, like LGM, not only in the traditional Mediterranean glacial refugia but also at higher latitudes in cryptic northern refugia located in Central France, the northern Alps as well as the Carpathians. However, the details of the post-glacial recolonization and the impact of the Late Glacial and Early Holocene climate changes on the evolutionary history of the common vole remains unclear. To address this issue, we analysed mtDNA cytochrome b sequences from more than one hundred common vole specimens from 36 paleontological and archaeological sites scattered across Europe. Our data suggest that populations from the European mid- and high latitudes suffered a local population extinction and contraction as a result of Late Glacial and Early Holocene climate and environmental changes. The recolonization of earlier abandoned areas took place in the Mid- to Late Holocene. In contrast, at low latitudes, in Northern Spain there was a continuity of common vole populations. This indicates different responses of common vole populations to climate and environmental changes across Europe and corroborates the hypothesis that abrupt changes, like those associated with Younger Dryas and the Pleistocene/Holocene transition, had a significant impact on populations at the mid- and high latitudes of Europe.
000088548 536__ $$9info:eu-repo/grantAgreement/ES/MICINN/RYC-2016-19386$$9info:eu-repo/grantAgreement/ES/MINECO/HAR2017-82483-C3-1-P
000088548 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000088548 590__ $$a4.112$$b2020
000088548 591__ $$aGEOGRAPHY, PHYSICAL$$b13 / 50 = 0.26$$c2020$$dQ2$$eT1
000088548 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b47 / 198 = 0.237$$c2020$$dQ1$$eT1
000088548 592__ $$a1.883$$b2020
000088548 593__ $$aArcheology$$c2020$$dQ1
000088548 593__ $$aArcheology (arts and humanities)$$c2020$$dQ1
000088548 593__ $$aGlobal and Planetary Change$$c2020$$dQ1
000088548 593__ $$aGeology$$c2020$$dQ1
000088548 593__ $$aEcology, Evolution, Behavior and Systematics$$c2020$$dQ1
000088548 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000088548 700__ $$aPopovic, D.
000088548 700__ $$aBaca, K.
000088548 700__ $$aLemanik, A.
000088548 700__ $$aDoan, K.
000088548 700__ $$aHorácek, I.
000088548 700__ $$aLópez-García, J.M.
000088548 700__ $$aBañuls-Cardona, S.
000088548 700__ $$aPazonyi, P.
000088548 700__ $$aDesclaux, E.
000088548 700__ $$aCrégut-Bonnoure, E.
000088548 700__ $$aBerto, C.
000088548 700__ $$aLenardic, J.M.
000088548 700__ $$aMiekina, B.
000088548 700__ $$aMurelaga, X.
000088548 700__ $$0(orcid)0000-0001-5125-9651$$aCuenca-Bescós, G.$$uUniversidad de Zaragoza
000088548 700__ $$aKrajcarz, M.
000088548 700__ $$aMarkovic, Z.
000088548 700__ $$aPetculescu, A.
000088548 700__ $$aWilczynski, J.
000088548 700__ $$aKnul, M.V.
000088548 700__ $$aStewart, J.R.
000088548 700__ $$aNadachowski, A.
000088548 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000088548 773__ $$g233 (2020), 106239 1-13$$pQuat. sci. rev.$$tQuaternary Science Reviews$$x0277-3791
000088548 8564_ $$s1431588$$uhttps://zaguan.unizar.es/record/88548/files/texto_completo.pdf$$yVersión publicada
000088548 8564_ $$s49029$$uhttps://zaguan.unizar.es/record/88548/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000088548 909CO $$ooai:zaguan.unizar.es:88548$$particulos$$pdriver
000088548 951__ $$a2021-09-02-08:53:45
000088548 980__ $$aARTICLE