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Palaeo-environmental implications derived from lake and sabkha deposits of the southern Rub' al-Khali, Saudi Arabia and Oman

机译:古环境的影响源于鲁布哈利南部,沙特阿拉伯和阿曼的湖泊和萨布卡矿床

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Shallow lakes and sabkha deposits are evidence of past periods of higher groundwater table than today, and hence reflect increased humidity in the Rub' al-Khali, the large desert in the southern part of the Arabian Peninsula. Reported here are the observations made during four expeditions into this remote area in combination with luminescence dating constraining the age of the deposits. The results presented extend the spatial coverage of evidence and show that most of the deposits correlate to MIS 5 (ca. 130-70 ka) and the Early/Mid Holocene (ca. 11-5.5 ka). A single sample points towards potentially more humid conditions during the transition MIS 4/3 (ca. 65-55 ka). The presence of the mussel Unio in some of the deposits attributed to MIS 5 is indirect evidence for the presence of fish in the lakes, which must have supported a rich and diverse fauna (and probably also flora). Together with other evidence, this demonstrates that a number of small persistent lakes were spread across the Rub' al-Khali for at least some of the time. These lakes would not only have been a potential source of freshwater but could also have provided an additional and easy accessible food source via the fish for humans migrating through the area. The presented palaeoenvironmental data underlines that parts of MIS 5 represent a time window of opportunity for a potential expansion of modern humans across Arabia. (C) 2014 Elsevier Ltd and INQUA. All rights reserved.
机译:浅水湖泊和sabkha沉积物是过去地下水位高于今天的证据,因此反映出阿拉伯半岛南部的大沙漠Rub'al-Khali的湿度增加。此处报告的是在四次远距离考察中与发光测年相结合的观测结果,这些观测结果限制了矿床的年龄。提出的结果扩大了证据的空间覆盖范围,并表明大多数沉积物与MIS 5(约130-70 ka)和早期/中期全新世(约11-5.5 ka)相关。在过渡MIS 4/3(约65-55 ka)期间,单个样本指向可能更潮湿的条件。 MIS 5所致某些沉积物中存在贻贝乌尼奥,这是湖中鱼类的存在的间接证据,这些鱼类必定支持了丰富多样的动物(可能还有植物)。与其他证据一起,这表明至少在某些时候,许多小而持久的湖泊遍布Rub'al-Khali。这些湖泊不仅可能是淡水的潜在来源,而且还可以通过鱼类为人类在该地区的迁移提供额外的和容易获得的食物来源。提出的古环境数据强调,MIS 5的各个部分代表了现代人类在阿拉伯潜在扩展的机会之窗。 (C)2014 Elsevier Ltd和INQUA。版权所有。

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