000145348 001__ 145348
000145348 005__ 20250923084445.0
000145348 0247_ $$2doi$$a10.1016/j.palaeo.2024.112532
000145348 0248_ $$2sideral$$a140242
000145348 037__ $$aART-2024-140242
000145348 041__ $$aeng
000145348 100__ $$0(orcid)0000-0003-1762-6328$$aDomínguez-García, Ángel C.
000145348 245__ $$aPalaeoclimatic analysis of Quaternary terrestrial small mammal assemblages from the Sierra de Atapuerca (Burgos, Spain)
000145348 260__ $$c2024
000145348 5060_ $$aAccess copy available to the general public$$fUnrestricted
000145348 5203_ $$aUnderstanding past climatic changes is one of the central challenges in palaeontological research. The Bioclimatic Model (BM) enables the reconstruction of qualitative and quantitative climatic conditions using the fossil record of rodents and eulipotyphlans. Here, we applied this model to the rich and well-documented fossil record from the localities of the Sierra de Atapuerca karst complex, including six archaeological and palaeontological sites spanning nearly continuously from the Early Pleistocene to the Late Holocene ∼1.2 Ma - 3.1 ka. A typical temperate climate was inferred for most of the sequence, with variations between Mediterranean and temperate climates, and the influence of boreal climates during the Late Pleistocene cold climatic oscillations recorded in El Portalón and El Mirador assemblages. The record from the base of the sequence of Sima del Elefante (TELRU, TE7-TE14) indicates relatively warmer conditions than the current climate, and a trend of thermal increase was observed from the end of Calabrian and Chibanian based on the Gran Dolina levels TD6 and TD8. Additionally, we obtained a thermotype classification reflecting regional-scale climatic changes linked to shifts in altitudinal belts boundaries. This work constitutes the first, diachronic, bioclimatic analysis of the entire biostratigraphic sequence of the Atapuerca site complex, providing an updated synthesis of long-term climatic reconstruction over more than one million years.
000145348 536__ $$9info:eu-repo/grantAgreement/ES/DGA/E18-23R$$9info:eu-repo/grantAgreement/ES/MCINN/PID2021-122533NB-I00$$9info:eu-repo/grantAgreement/ES/MSC/CT18-22
000145348 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000145348 590__ $$a2.7$$b2024
000145348 592__ $$a0.997$$b2024
000145348 591__ $$aPALEONTOLOGY$$b3 / 56 = 0.054$$c2024$$dQ1$$eT1
000145348 593__ $$aEarth-Surface Processes$$c2024$$dQ1
000145348 591__ $$aGEOGRAPHY, PHYSICAL$$b27 / 67 = 0.403$$c2024$$dQ2$$eT2
000145348 593__ $$aPaleontology$$c2024$$dQ1
000145348 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b99 / 258 = 0.384$$c2024$$dQ2$$eT2
000145348 593__ $$aOceanography$$c2024$$dQ1
000145348 593__ $$aEcology, Evolution, Behavior and Systematics$$c2024$$dQ1
000145348 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000145348 700__ $$aLópez-García, Juan Manuel
000145348 700__ $$aNúñez-Lahuerta, Carmen
000145348 700__ $$aGalán, Julia
000145348 700__ $$0(orcid)0000-0001-5125-9651$$aCuenca-Bescós, Gloria$$uUniversidad de Zaragoza
000145348 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000145348 773__ $$g655 (2024), 112532 [13 pp.]$$pPalaeogeogr. palaeoclimatol. palaeoecol.$$tPALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY$$x0031-0182
000145348 8564_ $$s1382933$$uhttps://zaguan.unizar.es/record/145348/files/texto_completo.pdf$$yVersión publicada
000145348 8564_ $$s2585562$$uhttps://zaguan.unizar.es/record/145348/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000145348 909CO $$ooai:zaguan.unizar.es:145348$$particulos$$pdriver
000145348 951__ $$a2025-09-22-14:53:49
000145348 980__ $$aARTICLE