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RESEARCH PRODUCT

Amphibians and reptiles as palaeonvironmental proxies during the Late Pleistocene (MIS3): The case of Stratigraphic Unit V of El Salt, Alcoi, Spain

Ana FagoagaCristo M. HernándezCarolina MallolRafael Marquina-blascoFrancisco Javier Ruiz-sánchezFrancisco Javier Ruiz-sánchezBertila GalvánSalvador BailonVicente D. Crespo

subject

010506 paleontologyPleistocene[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory010502 geochemistry & geophysicsOceanography01 natural sciences//purl.org/becyt/ford/1 [https]HWMLATE PLEISTOCENE//purl.org/becyt/ford/1.5 [https]PALAEOCLIMATEZamenisLacertidaeCoronellaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyChalcides bedriagaiEcologyEpidalea calamitaIBERIAN PENINSULAPaleontology15. Life on landHERPETOFAUNAbiology.organism_classificationAridificationMERPaleoecologyGeology

description

The locality of El Salt (Alcoi, Spain) is a key site for understanding the extirpation of Neanderthals in the eastern part of Iberia. In this paper, we analyse an assemblage of amphibians and reptiles from Stratigraphic Unit V (45.2 ± 3.4 ka to 44.7 ± 3.4 ka), which corresponds to one of the last regional records of Neanderthals, to improve knowledge of the palaeoecology and palaeoclimate of this event. The assemblage comprises three anurans (Pelodytes sp., Alytes obstetricans, and Epidalea calamita), two lizards (Lacertidae indet. and Chalcides bedriagai), and five snakes (Colubridae indet., Coronella sp., Coronella sp./Zamenis sp., Natrix maura, and Vipera latastei). Palaeoclimatic reconstruction, based on the Mutual Ecogeographic Range method, indicates that climate was cooler and slightly wetter climate than the present day climate of the Alcoi area. Applying the Habitat Weighting Method, we infer that the area surrounding El Salt was dominated by open dry regions, alternating with rocky areas with scarce scrubs and forest patches that would have developed under mesomediterranean conditions. These results are not entirely consistent with those obtained with other proxies (charcoal and small mammal assemblages) from the same site, which suggest slightly warmer and drier conditions. We hypothesise that these divergences may be partly related to the current wide distribution of reptiles and amphibians across Iberia. A key finding is that the extirpation of the Neanderthals in Iberia coincided with aridification. Fil: Marquina Blasco, Rafael. Universidad de Valencia; España. Museu Valencià D’història Natural; España Fil: Fagoaga, Ana. Universidad de Valencia; España. Museu Valencià D’història Natural; España Fil: Crespo Roures, Vicente Daniel. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleontología Vertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Museo Paleontológico de Alpuente; España Fil: Bailon, Salvador. Centre National de la Recherche Scientifique; Francia. Histoire naturelle de l’Homme prehistorique; Francia Fil: Mallol, Carolina. Universidad de La Laguna; España Fil: Hernández, Cristo M.. Universidad de La Laguna; España Fil: Galván, Bertila. Universidad de La Laguna; España Fil: Ruiz Sánchez, Francisco Javier. Universidad de Valencia; España. Museu Valencià D’història Natural; España. Universidad Estatal Península de Santa Elena; Ecuador

10.1016/j.palaeo.2021.110372https://hal.archives-ouvertes.fr/hal-03232899