globalchange  > 气候减缓与适应
DOI: 10.1016/j.quascirev.2017.09.011
Scopus记录号: 2-s2.0-85030862648
论文题名:
Human responses and non-responses to climatic variations during the last Glacial-Interglacial transition in the eastern Mediterranean
作者: Roberts N.; Woodbridge J.; Bevan A.; Palmisano A.; Shennan S.; Asouti E.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2018
卷: 184
起始页码: 47
结束页码: 67
语种: 英语
英文关键词: Agricultural origins ; Charcoal ; Neolithic revolution ; Palaeo-demography ; Pollen ; Southwest Asia
Scopus关键词: Charcoal ; Climate change ; Glacial geology ; Plants (botany) ; Population dynamics ; Population statistics ; Vegetation ; Agricultural origins ; Neolithic revolution ; Palaeo-demography ; Pollen ; Southwest Asia ; Probability distributions ; agricultural change ; anthropogenic effect ; archaeological evidence ; charcoal ; climate change ; climate conditions ; climate variation ; demography ; glacial-interglacial cycle ; Neolithic ; paleoenvironment ; Paleolithic ; pollen ; vegetation dynamics ; vegetation type ; woody plant ; Younger Dryas ; Anatolia ; Asia ; France ; Hyeres Islands ; Levant Island ; Mediterranean Region ; Mediterranean Sea ; Mediterranean Sea (East) ; Provence-Alpes-Cote d'Azur ; Turkey ; Var ; Animalia
英文摘要: We review and evaluate human adaptations during the last glacial-interglacial climatic transition in southwest Asia. Stable isotope data imply that climatic change was synchronous across the region within the limits of dating uncertainty. Changes in vegetation, as indicated from pollen and charcoal, mirror step-wise shifts between cold-dry and warm-wet climatic conditions, but with lag effects for woody vegetation in some upland and interior areas. Palaeoenvironmental data can be set against regional archaeological evidence for human occupancy and economy from the later Epipalaeolithic to the aceramic Neolithic. Demographic change is evaluated from summed radiocarbon date probability distributions, which indicating contrasting – and in some cases opposite - population trajectories in different regions. Abrupt warming transitions at ∼14.5 and 11.7 ka BP may have acted as pacemakers for rapid cultural change in some areas, notably at the start of the Natufian and Pre-Pottery Neolithic cultures. However temporal synchroneity does not mean that climatic changes had the same environmental or societal consequences in different regions. During cold-dry time intervals, regions such as the Levant acted as refugia for plant and animal resources and human population. In areas where socio-ecological continuity was maintained through periods of adverse climate (e.g. Younger Dryas) human communities were able to respond rapidly to subsequent climatic improvement. By contrast, in areas where there was a break in settlement at these times (e.g. central Anatolia), populations were slower to react to the new opportunities provided by the interglacial world. © 2017 Elsevier Ltd
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/112273
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作者单位: School of Geography, Earth and Environmental Sciences, Plymouth UniversityPL4 8AA, United Kingdom; Institute of Archaeology, University College London, United Kingdom; Department of Archaeology, Classics and Egyptology, University of Liverpool, United Kingdom

Recommended Citation:
Roberts N.,Woodbridge J.,Bevan A.,et al. Human responses and non-responses to climatic variations during the last Glacial-Interglacial transition in the eastern Mediterranean[J]. Quaternary Science Reviews,2018-01-01,184
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