Long-term Landscape, Environment and Climate Change Studies, from the Past through to Predictive Models for Future Developments

S. Smith, A. Allentuck, Louise Martin, Joe Roe, Matthew D. Jones, T. Richter, G. Rollefson, Hussam Hussein, Catherine Longford, K. Reynolds, Bernd Mller-Neuhof, R. Bewley, D. Kennedy, Rebecca Banks
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引用次数: 2

Abstract

The last glacial-interglacial transition (LGIT), between 20 and 10 ka BP, saw a global reorganization of climate, as ice caps melted, and a revolution in the way people lived, as agriculture developed. Understanding the spatial and temporal patterns of environmental change over this time period is therefore of interest to a range of disciplines. There are few long-term continuous records of environmental change from Jordan, or the natural archives where these may be found, and yet the eastern desert contains evidence of a long, and sometimes complex, occupation history, suggesting environments in the past were signifi cantly different to those of today. Such evidence indicates that a resource base was available for these communities to survive, or that ancient cultural economies were signifi cantly more advanced than we currently give them credit for. From a palaeoclimate perspective, spatial patterns of environmental change differ through the LGIT in regions north and west of Jordan compared to Arabia and North Africa so understanding where Jordan sits in this regional divide is important for understanding global climate structure through this transition.
长期景观、环境和气候变化研究,从过去到未来发展的预测模型
20 - 10 ka BP之间的最后一次冰期-间冰期过渡(LGIT)见证了全球气候的重组,冰盖融化;随着农业的发展,人类生活方式发生了革命。因此,了解这段时间内环境变化的时空格局是一系列学科的兴趣所在。约旦几乎没有长期连续的环境变化记录,也没有可能找到这些记录的自然档案,然而东部沙漠包含了长期的,有时甚至是复杂的占领历史的证据,这表明过去的环境与今天的环境有很大的不同。这些证据表明,这些社区的生存有资源基础,或者古代文化经济比我们现在所认为的要先进得多。从古气候的角度来看,与阿拉伯和北非相比,约旦北部和西部地区通过LGIT的环境变化空间格局有所不同,因此了解约旦在这一区域鸿沟中的位置对于通过这一转变了解全球气候结构非常重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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