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New dates and palaeoenvironmental evidence for the Middle to Upper Palaeolithic occupation of Higueral de Valleja Cave, southern Spain

机译:西班牙南部Higueral de Valleja Cave中至上古石器时代占领的新日期和古环境证据

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A research programme has been set up at Higueral de Valleja Cave in southern Spain to investigate the late survival and eventual extinction of the southern Iberian Neanderthals and the arrival of modern humans. Of key interest in the first phase of research was to understand the depositional environment in the entrance chamber of the cave and to establish whether palaeoenvironmental and dating samples could be retrieved from the Middle and Upper Palaeolithic sequences. The outcome is a series of OSL, TL and radiocarbon dates showing that the cave was occupied by Neanderthal populations in Marine Isotope Stage (MIS) 3, if not earlier, and by modern human Solutrean populations during the last glacial maximum. Cave sediments provisionally indicate that the lower Middle Palaeolithic sequence (X-VIII) formed in warm and humid environments and the upper sequence (VIII-V) formed when the climate was cooler and drier. The presence of long grass phytoliths and of the small mammals Microtus duo-decimcostatus, Microtus brecciensis and Apodemus sylvaticus in the upper sequence indicates that a range of habitat types persisted near the cave including grassland, scrubby vegetation, patchy tree cover and ponds. This raises the possibility that environmental factors were key factors in the late survival of Neanderthal populations at the cave.
机译:西班牙南部的Higueral de Valleja Cave已建立了一项研究计划,以调查南部伊比利亚尼安德特人的晚期生存和最终灭绝以及现代人类的到来。在研究的第一阶段中,最重要的兴趣是了解洞穴入口室内的沉积环境,并确定是否可以从中旧石器时代的上层序列中检索出古环境和年代标本。结果是一系列的OSL,TL和放射性碳测年表明,该洞穴被海洋同位素阶段(MIS)3的尼安德特人种群(如果不是更早的话)所占据,而在最后一次冰川最大时期被现代人类Solutrean种群所占据。洞穴沉积物临时表明,在温暖和潮湿的环境中形成了较低的中古旧石器时代层序(X-VIII),而当气候凉爽干燥时,形成了较高的层序(VIII-V)。上部序列中存在长草植物石板和小型哺乳动物Microtus duo-decimcostatus,Microtus brecciensis和Apodemus sylvaticus,这表明该洞穴附近存在着多种生境类型,包括草地,灌木状植被,斑驳的树木覆盖物和池塘。这增加了环境因素是洞穴中尼安德特人种群晚期生存的关键因素的可能性。

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