New stratigraphically constrained palaeoenvironmental reconstructions for the first human settlement in Western Europe: The Early Pleistocene herpetofaunal assemblages from Barranco León and Fuente Nueva 3 (Granada, SE Spain)

• Published in: Quaternary science reviews 2020-09, Vol.243, p.106466, Article 106466
• Main Authors: Sánchez-Bandera, Christian, Oms, Oriol, Blain, Hugues-Alexandre, Lozano-Fernández, Iván, Bisbal-Chinesta, Josep Francesc, Agustí, Jordi, Saarinen, Juha, Fortelius, Mikael, Titton, Stefania, Serrano-Ramos, Alexia, Luzón, Carmen, Solano-García, José, Barsky, Deborah, Jiménez-Arenas, Juan Manuel
• Format: Article
• Language: English
• Subjects: Amphibia; Early Pleistocene; First human settlement in Europe; Habitat weighting; Iberian Peninsula; Squamata
• ISSN: 0277-3791; 1873-457X
• DOI: 10.1016/j.quascirev.2020.106466

The Early Pleistocene sites of Barranco León and Fuente Nueva 3 (Guadix-Baza Basin, SE Spain) have yielded abundant Oldowan lithic artifacts and one hominin tooth (Homo sp. in level D1 or D2 of Barranco León), today considered to be among the earliest evidence for a hominin presence in Western Europe, at ca. 1.4–1.2 Ma. Here, for the first time, the stratigraphic succession of these two sites are studied more precisely from a palaeoenvironmental point of view, taking into account the different levels of the depositional sequences to analyze the successive fossil assemblages of amphibians and reptiles. Palaeoenvironmental reconstructions are carried out by applying the “habitat weighting” method, which uses the modern distribution by habitat of amphibian and reptile species in order to interpret past landscapes. The successive herpetofaunal assemblages from Barranco León show a certain tendency towards more arid conditions from level D1 to level E, whereas in Fuente Nueva 3 environmental reconstructions reveal oscillating conditions, with a tendency towards more arid conditions in the basal part of the sequence, up to level 5, where the tendency shifts back to more humid conditions. Our results show that the layers included in this study with the highest density of anthropic evidence (such as level 5 in FN 3 and levels D1 and D2 in BL) are situated within the late Early Pleistocene climatic and environmental cyclicity, yielding different environmental conditions: a humid, wooded biotope for BL, and a more open and drier biotope in FN 3. This suggests that the hominins of the late Early Pleistocene, although conditioned to some extent by climatic factors, were able to cope with changing environmental conditions, both “interglacial” and “glacial”, in the southwestern extremity of the European continent. •Amphibians and reptiles are good proxies for the environmental reconstructions.•Paleoenvironmental conditions are reconstructed by stratigraphic levels.•The first hominins in Western Europe coped with changing environmental conditions.•The paleoenvironmental changes are in agreement with the climate oscillations.