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An investigation of local scale human/landscape dynamics in the endorheic alluvial fan of the Murghab River, Turkmenistan

机译:土库曼斯坦穆尔加布河的内河冲积扇局部尺度的人类/景观动力学研究

摘要

Endorheic or inland deltas, commonly found across the deserts of Central Asia, represent unique anduddynamic ecotones that are still not fully understood. These regions of environmental and landscapeudtransition as well as social liminality straddle the line between fertile, sustainable environments and lessudproductive desertic regions less capable of sustaining significant human occupation. Because suchudboundary areas are dynamic and often unpredictable, they are excellent case studies through which toudstudy the complex processes that have characterized human/environmental relationships throughoutudthe late Holocene.udThis paper focuses on the local variability that characterizes these relationships in one such region, theudterminal fan of the Murghab River in Turkmenistan. Populated since at least the late 5th millennium BPudand likely earlier, the region has been variously described as an oasis environment in which deserticudprocesses have been more or less stagnant throughout the late Holocene, or, alternatively, as a fertile,udcontinuously occupied and heavily-cultivated alluvial fan in which desertification was a relatively lateudprocess, intensifying only in the mid 4th millennium BP. This paper presents geoarchaeological data fromuda series of test pits in the distal portion of the terminal fan to show that local-scale analysis indicates a farudmore complex interpretation, one shaped by the continuous and non-uniform interaction of aeolian andudalluvial depositional environments, and one that bears substantially on human/landscape dynamics inudthe region. The late Holocene development of the distal fan is examined using proxy data from granulometricudanalysis, Loss on Ignition (LoI) and geochemical analysis, as well as a series of new OSL datesudthat refines the depositional chronology of the region. Ultimately, we show that landscape changeudthroughout the Holocene has been characterized by pronounced variability at the local level not fullyuddescribed by regional scale approaches. While differential aeolian encroachment, non-uniform alluvialudprocesses, and climatic conditions bear significantly on the initial conditions for human occupation,udhuman/environmental processes are ultimately co-evolutionary in nature.
机译:在中亚的沙漠中普遍发现的内陆三角洲或内陆三角洲代表着独特而又动感十足的生态交错带,至今仍未完全了解。这些环境和景观过度过渡以及社会自由度的地区跨越了肥沃的,可持续的环境和生产力较低的低生产力的沙漠地区之间的界线,这些地区无法维持重要的人类占领。由于此类边界区域是动态的且常常是不可预测的,因此它们是出色的案例研究,可用于研究整个全新世晚期人与环境之间关系的复杂过程。 ud本文重点介绍表征这些关系的局部变异性。一个这样的地区,就是土库曼斯坦穆尔加布河的“末航母”。自从至少在5,000年晚期BP人口稠密,并且可能更早以来,该地区就被形容为一个绿洲环境,在整个绿洲环境中,整个全新世晚期的荒漠化过程或多或少停滞不前,或者是肥沃的,连续的荒漠化是一个相对较晚的过程,仅在第4个千年中期BP加剧。本文提供了来自末端风机远端部分测试坑的 uda系列的地球考古数据,以表明局部尺度分析显示了远 udmore复杂的解释,其解释是由风沙和 ualluvial的连续和非均匀相互作用相互作用形成的沉积环境,并且基本上取决于该地区的人类/景观动态。使用来自粒度分析/ udanalysis,灼烧失重(LoI)和地球化学分析以及一系列新的OSL日期/ ud的代理数据,检查了远端扇的全新世晚期发育,该数据可重新定义该地区的沉积年代。最终,我们表明,整个全新世的景观变化的特征是局部水平上的明显变化,而区域尺度方法并未完全描述。尽管不同的风成侵蚀,非均匀的冲积过程和气候条件在很大程度上取决于人类占领的初始条件,但是人类/环境过程最终在本质上是共同进化的。

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