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Unravelling the oxygen isotope signal (δ18O) of rodent teeth from northeastern Iberia, and implications for past climate reconstructions

dc.contributor.authorFernández-García, Mónica
dc.contributor.authorRoyer, Aurélien
dc.contributor.authorLópez-García, Juan
dc.contributor.authorBennàsar, Maria
dc.contributor.authorGoedert, Jean
dc.contributor.authorFourel, François
dc.contributor.authorJulien, Marie-Anne
dc.contributor.authorBañuls-Cardona, Sandra
dc.contributor.authorRodríguez-Hidalgo, Antonio
dc.contributor.authorVallverdú, Josep
dc.contributor.authorLécuyer, Christophe
dc.date.accessioned2020-04-23T08:41:48Z
dc.date.available2020-04-23T08:41:48Z
dc.date.issued2019
dc.description.abstractSmall mammals, especially rodents, constitute valuable proxies for continental Quaternary environments at a regional and local scale. Recent studies have demonstrated the relation between the stable oxygen isotope composition of the biogenic phosphate from rodent teeth (δ18Op), and the oxygen isotope composition of meteoric waters (δ18Omw), which is related to air temperatures at mid and high latitudes. This work explores the δ18Op of rodent tooth enamel (from Murinae and Arvicolinae subfamilies) to investigate the palaeoenvironmental conditions in northeastern Iberia during Marine Isotope Stage 3 (MIS 3; ca. 60-30 ka). Fourteen new δ18Op analyses from modern samples in conjunction with forty-six δ18Op analyses previously published are used to decipher the isotope record of present-day rodent teeth in this region. Two main factors should be considered in Iberian palaeoenvironmental reconstructions: the singular nature of Iberian δ18Omw records and the potential seasonality bias of small-mammal accumulation. Methodological proposals are made with a view to ensuring the correct interpretation of the δ18Op of small mammals in reconstructing past air temperatures. This methodology is applied to the MIS 3 sequence of the Cova dels Xaragalls site (Vimbodí-Poblet, Tarragona, Spain), where fifty-one δ18O analyses were performed on wood mouse (Apodemus sylvaticus) lower incisors. A spring-early summer accumulation of small mammals is suggested for the layers at Cova dels Xaragalls. In agreement with previous environmental studies of the site, variations in the δ18Op values suggest slight fluctuations in the climatic conditions throughout the sequence, which are consistent with the stadial-interstadial alternations that characterized MIS 3. Complementary palaeoenvironmental methods determine cooler conditions than nowadays, but within a globally stable climatic period.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationFernández-García, M., Royer, A., López-García, J. M., Bennàsar, M., Goedert, J., Fourel, F., . . . Lécuyer, C. (2019). Unravelling the oxygen isotope signal (δ18O) of rodent teeth from northeastern Iberia, and implications for past climate reconstructions. Quaternary Science Reviews, 218 107-121. doi: 10.1016/j.quascirev.2019.04.035pt_PT
dc.identifier.doi10.1016/j.quascirev.2019.04.035pt_PT
dc.identifier.issn0277-3791
dc.identifier.urihttp://hdl.handle.net/10451/43067
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherElsevierpt_PT
dc.relation.publisherversionhttps://www.sciencedirect.com/science/article/pii/S0277379118307224pt_PT
dc.subjectSmall mammalspt_PT
dc.subjectStable isotopespt_PT
dc.subjectGeochemistrypt_PT
dc.subjectPalaeoclimatologypt_PT
dc.subjectLate Pleistocenept_PT
dc.subjectWestern Europept_PT
dc.titleUnravelling the oxygen isotope signal (δ18O) of rodent teeth from northeastern Iberia, and implications for past climate reconstructionspt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage121pt_PT
oaire.citation.startPage107pt_PT
oaire.citation.titleQuaternary Science Reviewspt_PT
oaire.citation.volume218pt_PT
person.familyNameLópez-García
person.givenNameJuan Manuel
person.identifier.ciencia-id8A17-C512-C4C1
person.identifier.orcid0000-0003-1605-9763
rcaap.rightsclosedAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublication6c7b8a02-53c6-4523-a522-95a81d7cbc33
relation.isAuthorOfPublication.latestForDiscovery6c7b8a02-53c6-4523-a522-95a81d7cbc33

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