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dc.contributor.authorBlain, Hugues-Alexandre
dc.contributor.authorCruz Silva, José Alberto
dc.contributor.authorJiménez Arenas, Juan Manuel
dc.contributor.authorMargari, Vasiliki
dc.contributor.authorRoucoux, Katherine
dc.date.accessioned2019-05-20T23:38:17Z
dc.date.available2019-05-20T23:38:17Z
dc.date.issued2018-07-01
dc.identifier.citationBlain , H-A , Cruz Silva , J A , Jiménez Arenas , J M , Margari , V & Roucoux , K 2018 , ' Towards a Middle Pleistocene terrestrial climate reconstruction based on herpetofaunal assemblages from the Iberian Peninsula : state of the art and perspectives ' , Quaternary Science Reviews , vol. 191 , pp. 167-188 . https://doi.org/10.1016/j.quascirev.2018.04.019en
dc.identifier.issn0277-3791
dc.identifier.otherPURE: 253147428
dc.identifier.otherPURE UUID: c692a833-b2c5-434c-bb45-26615c5e3de9
dc.identifier.otherRIS: urn:695710C79B441AF54376B355F92D75E6
dc.identifier.otherScopus: 85047148989
dc.identifier.otherWOS: 000437363000012
dc.identifier.urihttp://hdl.handle.net/10023/17733
dc.descriptionThis paper has been mainly funded by the University of Reading and also by projects CGL2016-80000-P (Spanish Ministry of Economy and Competitiveness) and 2017SGR-859 (Generalitat de Catalunya).en
dc.description.abstractThe pattern of the varying climatic conditions in southern Europe over the last million years is well known from isotope studies on deep-ocean sediment cores and the long pollen records that have been produced for lacustrine and marine sedimentary sequences from Greece, Italy and the Iberian margin. However, although relative glacial and interglacial intensities are well studied, there are still few proxies that permit quantitative terrestrial temperature and precipitation reconstruction. In this context, fauna-based climate reconstructions based on evidence preserved in archaeological or palaeontological sites are of great interest, even if they only document short windows of that climate variability, because (a) they provide a range of temperature and precipitation estimates that are understandable in comparison with present climate; (b) they may allow the testing of predicted temperature changes under scenarios of future climate change; and (c) quantitative temperature and precipitation estimates for past glacials and interglacials for specific regions/latitudes can help to understand their effects on flora, fauna and hominids, as they are directly associated with those cultural and/or biological events. Moreover such reconstructions can bring further arguments to the discussion about important climatic events like the Mid-Bruhnes Event, a climatic transition between moderate warmths and greater warmths during interglacials. In this paper we review a decade of amphibian- and reptile-based climate reconstructions carried out for the Iberian Peninsula using the Mutual Ecogeographic Range method in order to present a regional synthesis from MIS 22 to MIS 6, discuss the climate pattern in relation to the Mid-Bruhnes Event and the thermal amplitude suggested by these estimates and finally to identify the chronological gaps that have still to be investigated.
dc.format.extent22
dc.language.isoeng
dc.relation.ispartofQuaternary Science Reviewsen
dc.rights© 2018, Elsevier Ltd. This work has been made available online in accordance with the publisher’s policies. This is the author created accepted version manuscript following peer review and as such may differ slightly from the final published version. The final published version of this work is available at https://doi.org/10.1016/j.quascirev.2018.04.019en
dc.subjectVertebrates as climate proxyen
dc.subjectAmphibianen
dc.subjectReptileen
dc.subjectMutual Ecogeographic Rangeen
dc.subjectMiddle Pleistoceneen
dc.subjectSouth-Western Mediterraneanen
dc.subjectGE Environmental Sciencesen
dc.subjectG Geography (General)en
dc.subject.lccGEen
dc.subject.lccG1en
dc.titleTowards a Middle Pleistocene terrestrial climate reconstruction based on herpetofaunal assemblages from the Iberian Peninsula : state of the art and perspectivesen
dc.typeJournal itemen
dc.description.versionPostprinten
dc.contributor.institutionUniversity of St Andrews.School of Geography & Sustainable Developmenten
dc.identifier.doihttps://doi.org/10.1016/j.quascirev.2018.04.019
dc.description.statusPeer revieweden
dc.date.embargoedUntil2019-05-21


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