首页> 外文期刊>Archaeometry >TAPHONOMIC OBSERVATIONS OF ARCHAEOLOGICAL WHEAT PHYTOLITHS FROM NEOLITHIC ATALH?YüK, TURKEY, AND THE USE OF CONJOINED PHYTOLITH SIZE AS AN INDICATOR OF WATER AVAILABILITY*
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TAPHONOMIC OBSERVATIONS OF ARCHAEOLOGICAL WHEAT PHYTOLITHS FROM NEOLITHIC ATALH?YüK, TURKEY, AND THE USE OF CONJOINED PHYTOLITH SIZE AS AN INDICATOR OF WATER AVAILABILITY*

机译:来自土耳其新谷类的考古小麦植株的定律观察以及结合的植株大小作为水利用率的指示*

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摘要

An investigation of wheat husk phytoliths from a midden deposit at Neolithic atalh?yük provided the opportunity to investigate the impact of taphonomic processes on conjoined phytolith size. Wheat husk phytoliths from a possible crop processing deposit were examined using three methods. The results indicate that the size of conjoined forms decreases significantly as a result of laboratory extraction and slide preparation. Observations of the phytolith layer in thin section show some of the depositional and post-depositional processes affecting phytolith size. These results indicate that these taphonomic factors need further investigation before conjoined phytolith size can be used to infer past water availability and agricultural practices.
机译:对新石器时代atalh?yük中部矿床的小麦壳植物石进行的调查提供了机会,研究了自发过程对联合植物石尺寸的影响。使用三种方法检查了可能的农作物加工沉积物中的小麦壳植硅石。结果表明,由于实验室提取和玻片制备,连体形式的大小显着减少。对薄壁植物石层的观察表明,一些沉积和沉积后过程会影响植物石的大小。这些结果表明,在结合植物石板的大小可用于推断过去的水供应和农业实践之前,需要对这些植物学因素进行进一步研究。

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