0000000000448405

AUTHOR

Christoph Burow

showing 2 related works from this author

Cueva Antón: A multi-proxy MIS 3 to MIS 5a paleoenvironmental record for SE Iberia

2016

Overlying a palustrine deposit of unknown age (complex FP), and protected from weathering and erosion inside a large cave/rock-shelter cavity, the sedimentary fill of Cueva Antón, a Middle Paleolithic site in SE Spain, corresponds in most part (sub-complexes AS2-to-AS5) to a ca.3 m-thick Upper Pleistocene terrace of the River Mula. Coupled with the constraints derived from the deposit’s paleoclimatic proxies, OSL dating places the accumulation of this terrace in MIS 5a, and radiocarbon dates from the overlying breccia cum alluvium (sub-complex AS1) fall in the middle part of MIS 3; the intervening hiatus relates to valley incision and attendant erosion. The two intervals represented remain …

Marine isotope stageRadiocarbon dating010506 paleontologyArcheology010504 meteorology & atmospheric sciencesPleistoceneMiddle PaleolithicLuminescence datingMarine isotope stage01 natural scienceslaw.inventionSedimentary depositional environmentPaleontologyCavelawMiddle PaleolithicGreenland interstadialMiddle PalaeolithicRadiocarbon datingEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryNeandertalesGeologyAleppo pineMurciaAlluviumGeologyNeandertal
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Luminescence Dating of Fluvial Deposits in the Rock Shelter of Cueva Antón, Spain

2015

Abstract The fluvial sediments at Cueva Antón, a Middle Palaeolithic rock shelter located in the valley of the River Mula (Southeast Spain), produced abundant lithic assemblages of Mousterian affinities. Radiocarbon dates are available for the upper part of the archaeological succession, while for the middle to lower parts chronometric data have been missing. Here we present luminescence dating results for these parts of the succession. Quartz OSL on small aliquots and single grain measurements yield ages ranging from 69 ± 7 ka to 82 ± 8 ka with a weighted mean of 72 ± 4 ka for sub-complexes AS2 to AS5. Equivalent dose estimates from large aliquots were highest and inconsistent with those f…

Thermoluminescence datingLuminescence datingFluvial sedimentGeochemistryFluvialMousterianEcological successionArqueologiaFeldsparlaw.inventionlawvisual_artEarth and Planetary Sciences (miscellaneous)visual_art.visual_art_mediumMiddle PalaeolithicRadiocarbon datingSingle grain datingPost-IR IRSLCueva AntónQuartzGeomorphologyRock shelterGeologyGeochronometria
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