globalchange  > 过去全球变化的重建
DOI: 10.1016/j.quascirev.2014.04.009
Scopus记录号: 2-s2.0-84899685681
论文题名:
Climate and environments during Marine Isotope Stage 11 in the central Iberian Peninsula: The herpetofaunal assemblage from the Acheulean site of Áridos-1, Madrid
作者: Blain H.-A.; Santonja M.; Pérez-González A.; Panera J.; Rubio-Jara S.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2014
卷: 94
起始页码: 7
结束页码: 21
语种: 英语
英文关键词: Acheulean ; Herpetofauna ; Marine isotope stage 11 ; Middle pleistocene ; Spain ; Western mediterranean
Scopus关键词: Climate change ; Ecosystems ; Mammals ; Precipitation (meteorology) ; Acheulean ; Herpetofauna ; Marine isotope stages ; Middle Pleistocene ; Spain ; Western Mediterranean ; Isotopes
英文摘要: The interglacial episodes of the Quaternary Period are currently the focus of a great deal of attention within the scientific community, primarily because they can help us to understand how the climate of the current interglacial may have evolved without human intervention and to assess the impact of these climate changes on ecological systems. In the central Iberian Peninsula, the archaeological site of Áridos-1 (Arganda, Madrid), with numeric dates of 379.7±45 ka obtained by AAR for the upper part of the sedimentological unit of Arganda I, in combination with the evolved state of the small mammals, has been chronologically attributed to Marine Isotope Stage (MIS) 11. Given the diversified faunal assemblages delivered by the 1976 excavations, Áridos-1 is probably one of the best terrestrial candidates for an understanding of the climatic and environmental conditions that prevailed in central Spain during the MIS 11 interglacial. In consequence, the fossil amphibians and squamate reptiles stored in the collections of the Museo Arqueológico Nacional of Madrid have been newly described and quantified in order to apply the mutual climatic range and habitat weighting methods for estimating quantitative data. The Mediterranean climate is shown to have been warmer and wetter than today in central Spain during MIS 11, with the mean annual temperature 1.7°C higher and mean annual precipitation 223.9mm higher than at present. The monthly climatic reconstruction shows differences in the distribution of precipitation over the course of the year, with more abundant precipitation during the winter months, at the beginning of spring and at the end of fall (from October to March) and less precipitation than today during the summer months and at the end of spring (from May to August), suggesting stronger rainfall seasonality between winter and summer than currently occurs. Such climate reconstruction is consistent with other European MIS 11 paleoclimatic records. The paleoenvironmental reconstruction based on the herpetofaunal assemblage suggests a patchy landscape with a large representation of dry meadows, scrubland and rocky habitats together with well-evidenced aquatic habitats. Such open environments during a warm and humid forestal period are seen to be connected with the location of the site in a large river valley, where open vegetation would have been partly initiated and certainly maintained by the grazing, browsing, trampling and tree-felling activities of large mammals. © 2014 Elsevier Ltd.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/60257
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作者单位: IPHES, Institut Català de Paleoecologia Humana i Evolució Social, c/ Marcelli Domingo s/n (Edifici W3), Campus Sescelades, 43007 Tarragona, Spain; Àrea de Prehistòria, Universitat Rovira i Virgili (URV), Avinguda de Catalunya 35, 43002 Tarragona, Spain; CENIEH, Centro Nacional de Investigación sobre la Evolución Humana, Paseo de la Sierra de Atapuerca s/n, 09004 Burgos, Spain; IDEA, Instituto de Evolución en África, Museo de los Orígenes, Plaza de San Andrés 2, 28005 Madrid, Spain

Recommended Citation:
Blain H.-A.,Santonja M.,Pérez-González A.,et al. Climate and environments during Marine Isotope Stage 11 in the central Iberian Peninsula: The herpetofaunal assemblage from the Acheulean site of Áridos-1, Madrid[J]. Quaternary Science Reviews,2014-01-01,94
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