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首页> 外文期刊>Geoarchaeology >Holocene environment and settlement on the Carsamba alluvial fan, south-central Turkey: Integrating geoarchaeology and archaeological field survey
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Holocene environment and settlement on the Carsamba alluvial fan, south-central Turkey: Integrating geoarchaeology and archaeological field survey

机译：土耳其中南部，Carsamba冲积扇的全新世环境和沉积：地质考古和考古现场调查相结合

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The four-dimensional geomorphological history of the Carsamba fan in the Konya Basin, Turkey, has been reconstructed as part of integrated field research into the relations between Holocene environments and settlement history within a spatially well defined alluvial landscape, similar to 500 km(2) in extent. This has involved on- and offsite study of alluvial sequences linked to a systematic archaeological site survey of multiperiod settlement mounds and to excavations at the Neolithic-Chalcolithic site of Catalhoyuk. Two principal alluvial units lie above Late Pleistocene lake marls and have been characterized using particle size, magnetic susceptibility, organic and carbonate content, and color. Based on a combination of C-14, optically stimulated luminescence (OSL), and archaeological evidence, the lower unit dates primarily to the Neolithic-Chalcolithic, while the upper unit dates from Bronze Age to post-Byzantine times. Counterintuitively, alluvial landscape changes have not necessarily led to the systematic burial-and, therefore, "loss"-of those archaeological sites that are smaller or shallower, earlier (i.e., prehistoric), and located closer to the fan apex. As well as being important in interpreting settlement distributions, this geomorphological history of alluviation, pedogenesis, and erosion also provides data on changing flood regimes and soil and water availability that have affected the suitability of individual areas for human occupation. (c) 2006 Wiley Periodicals, Inc.
机译：作为整合野外研究的一部分，重建了土耳其科尼亚盆地卡桑巴扇的四维地貌史，作为对空间界定明确的冲积景观中全新世环境与沉降历史之间关系的研究的一部分，类似于500 km（2）在范围上。这涉及到冲积层序的实地和异地研究，这些研究与多期定居丘陵的系统考古现场调查以及Catalhoyuk的新石器时代-石器时代遗址的发掘有关。在晚更新世湖灰岩之上有两个主要的冲积单元，并利用粒径，磁化率，有机和碳酸盐含量以及颜色来表征。基于C-14，光学激发发光（OSL）和考古学证据的结合，较低的单位主要是新石器时代-胆石器时代，而较高的单位是青铜时代至拜占庭时代之后。与直觉相反，冲积景观的变化并不一定导致较早或较早（即史前）且位于扇形顶点附近的那些考古遗址的系统埋葬，从而造成“损失”。冲积作用，成岩作用和侵蚀的地貌史不仅在解释定居点分布方面很重要，而且还提供了有关洪水制度变化和土壤和水供应变化的数据，这些变化影响了各个地区对人类占领的适宜性。 （c）2006年Wiley Periodicals，Inc.

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