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首页> 外文期刊>Quaternary International >Changing patterns of eastern Mediterranean shellfish exploitation in the Late Glacial and Early Holocene: Oxygen isotope evidence from gastropod in Epipaleolithic to Neolithic human occupation layers at the Haua Fteah cave, Libya
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Changing patterns of eastern Mediterranean shellfish exploitation in the Late Glacial and Early Holocene: Oxygen isotope evidence from gastropod in Epipaleolithic to Neolithic human occupation layers at the Haua Fteah cave, Libya

机译:冰川晚期和全新世早期地中海贝类开采方式的变化:利比亚Haua Fteah洞穴表新石器时代腹足动物到新石器时代人类占领层的氧同位素证据

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The seasonal pattern of shellfish foraging at the archaeological site of Haua Fteah in the Gebel Akhdar, Libya was investigated from the Epipaleolithic to the Neolithic via oxygen isotope (delta O-18) analyses of the topshell Phorcus (Osilinus) turbinatus. To validate this species as faithful year-round palaeoenvironmental recorder, the intra-annual variability of delta O-18 in modern shells and sea water was analysed and compared with measured sea surface temperature (SST). The shells were found to be good candidates for seasonal shellfish forging studies as they preserve nearly the complete annual SST cycle in their shell delta O-18 with minimal slowing or stoppage of growth. During the terminal Pleistocene Early Epipaleolithic (locally known as the Oranian, with modeled dates of 17.2-12.5 ka at 2 sigma probability, Douka et al., 2014), analysis of archaeological specimens indicates that shellfish were foraged year-round. This complements other evidence from the archaeological record that shows that the cave was more intensively occupied in this period than before or afterwards. This finding is significant as the period of the Oranian was the coldest and driest phase of the last glacial cycle in the Gebel Akhdar, adding weight to the theory that the Gebel Akhdar may have served as a refugium for humans in North Africa during times of global climatic extremes. Mollusc exploitation in the Latest Pleistocene and Early Holocene, during the Late Epipaleolithic (locally known as the Capsian, c. 12.7 to 9 ka) and the Neolithic (c. 8.5 to 5.4 ka), occurred predominantly during winter. Other evidence from these archaeological phases shows that hunting activities occurred during the warmer months. Therefore, the timing of Holocene shellfish exploitation in the Gebel Akhdar may have been influenced by the seasonal availability of other resources at these times and possibly shellfish were used as a dietary supplement when other foods were less abundant. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
机译:在利比亚的Gebel Akhdar的Haua Fteah考古遗址上,通过表层磷锅(Osilinus)turbinatus的氧同位素(δO-18)分析了从旧石器时代到新石器时代的贝类觅食的季节性模式。为了验证该物种是否为忠实的全年古环境记录仪,分析了现代贝壳和海水中O-18的年内变化并将其与测得的海面温度(SST)进行了比较。人们发现这些贝壳是季节性贝类锻造研究的理想候选者,因为它们在其贝壳三角洲O-18中几乎保留了完整的年度SST周期,而减缓或停止生长的可能性却很小。在更新世晚期的旧石器时代晚期(当地称为Oranian,以2σ的概率模拟日期为17.2-12.5 ka,Douka等人,2014),考古标本分析表明,贝类是全年觅食的。这与考古记录中的其他证据相辅相成,该证据表明该时期比以前或之后的时期都更加密集。这一发现意义重大,因为奥拉尼时期是格贝尔·阿赫达尔冰川最后一个冰期的最冷和最干燥的时期,这加重了这样的理论:即格贝尔·阿赫达尔可能是全球范围内北非人类的避难所。气候极端事件。在上新石器时代晚期(当地称为Capsian,约12.7至9 ka)和新石器时代(约8.5至5.4 ka)期间,在最新的更新世和全新世早期进行的软体动物剥削主要发生在冬季。这些考古阶段的其他证据表明,狩猎活动发生在较温暖的月份。因此,Gebel Akhdar全新世贝类的开采时间可能受到这些时间其他资源的季节性供应的影响,并且当其他食物较少时,贝类可能被用作膳食补充剂。 (C)2015 Elsevier Ltd和INQUA。版权所有。

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