ESR chronology of the fluvial sequence of Cueva del Silo (Sierra de Atapuerca,Spain) |
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| Institution: | 1. Centro Nacional de Investigación Sobre la Evolución Humana (CENIEH), Paseo Sierra de Atapuerca 3, Burgos, 09002, Spain;2. Fundación Atapuerca, Calle Crta. De Logroño 44, Ibeas de Juarros, Burgos, 09198, Spain;3. Institut Català de Paleoecologia Humana i Evolució Social (IPHES), Edificio W3, Campus Sescelades URV, Zona Educacional 4, Tarragona, 43007, Spain;4. Universitat Rovira i Virgili, Campus Sescelades URV, Zona Educacional 4, Tarragona, 43007, Spain |
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| Abstract: | The Cueva del Silo is part of the lower karst level of the Cueva Mayor-Cueva del Silo karst system (Sierra de Atapuerca, Burgos, Spain), whose evolution has preserved an impressive archeo-paleoanthropological sequence since the Early Pleistocene. Cueva del Silo is remarkable for the presence of fluvial deposits that record the entry of the Arlanzón River water in the cave system, providing a key sequence to investigate the fluvio-karstic relationships that give rise to this endokarst system. In order to provide a chronological framework to these fluvial deposits, six sediment samples were dated by Electron Spin Resonance and 16 samples by paleomagnetism, collected from two outcrops: Galería de las Arenas and Sala del Caos. Our results provide maximum mean age of around 1600 ka and a minimum age of 916 ± 136 ka for the deposits in Sala del Caos. The younger date from Sala del Caos might represent the last fluvial input from Arlanzón River in the lower karst level. In contrast, ESR ages estimates of 1268 ± 133 ka and 1262 ± 108 ka were obtained for Galería de las Arenas sequence, which could indicate re-sedimentation processes from the intermediate karst level where similar ages were published. The annual dose might be wrongly assessed due to the re-sedimentation processes inside the karst, hence, ESR ages for these facies should be treated with extreme caution. |
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| Keywords: | ESR dating Fluvial sediments Atapuerca karst Bleached quartz Pleistocene |
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