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DOI10.1016/j.quascirev.2019.04.035
Unravelling the oxygen isotope signal (δ18O) of rodent teeth from northeastern Iberia; and implications for past climate reconstructions
Fernández-García M.; Royer A.; López-García J.M.; Bennàsar M.; Goedert J.; Fourel F.; Julien M.-A.; Bañuls-Cardona S.; Rodríguez-Hidalgo A.; Vallverdú J.; Lécuyer C.
发表日期2019
ISSN0277-3791
起始页码107
结束页码121
卷号218
英文摘要Small 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. © 2019 Elsevier Ltd
英文关键词Geochemistry; Late Pleistocene; Palaeoclimatology; Small mammals; Stable isotopes; Western Europe
语种英语
scopus关键词Atmospheric temperature; Geochemistry; Mammals; Oxygen; Repair; Signal reconstruction; Tooth enamel; Late Pleistocene; Palaeoclimatology; Small mammals; Stable isotopes; Western Europe; Isotopes; air temperature; geochemistry; interstadial; marine isotope stage; meteoric water; oxygen isotope; paleoclimate; paleoenvironment; paleotemperature; Pleistocene; proxy climate record; Quaternary; reconstruction; rodent; small mammal; stable isotope; tooth; Catalonia; Iberian Peninsula; Spain; Tarragona [Catalonia]; Apodemus sylvaticus; Arvicolinae; Mammalia; Murinae; Rodentia
来源期刊Quaternary Science Reviews
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/151857
作者单位Sezione di Scienze Preistoriche e Antropologiche, Dipartimento di Studi Umanistici, Università degli Studi di Ferrara (UNIFE), C/ so Ercole I d'Este 32, Ferrara, 44121, Italy; Histoire Naturelle de l'Homme Préhistorique (HNHP, UMR CNRS 7194), Muséum National d'Histoire Naturelle (MNHN), Sorbonne Universités, 1 rue René Panhard, Paris, 75013, France; Biogéosciences, UMR CNRS 6282, Université Bourgogne Franche-Comté, 6 Boulevard Gabriel, Dijon, 21000, France; Institut Català de Paleoecologia Humana i Evolució Social (IPHES), Zona Educacional 4, Campus Sescelades URV (Edifici W3), Tarragona, 43007, Spain; Àrea de Prehistòria, Universitat Rovira i Virgili (URV), Av. Catalunya 35, Tarragona, 43002, Spain; PACEA, UMR CNRS 5199, Université de Bordeaux, Bâtiment B18, Allée Geoffroy Saint-Hilaire, CS 50023, Pessac, 33615, France; Laboratoire d'Ecologie des Hydrosystèmes Naturels et Anthropisés (LEHNA), UMR CNRS 5023, ENTPE, Université Claude Bernard Lyon 1, Villeurbanne, 69622, France; Complutense University, Preh...
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Fernández-García M.,Royer A.,López-García J.M.,et al. Unravelling the oxygen isotope signal (δ18O) of rodent teeth from northeastern Iberia; and implications for past climate reconstructions[J],2019,218.
APA Fernández-García M..,Royer A..,López-García J.M..,Bennàsar M..,Goedert J..,...&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.
MLA Fernández-García M.,et al."Unravelling the oxygen isotope signal (δ18O) of rodent teeth from northeastern Iberia; and implications for past climate reconstructions".Quaternary Science Reviews 218(2019).
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