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量化沙特阿拉伯法萨尼群岛贝壳丘形成的空间变异性。

Quantifying spatial variability in shell midden formation in the Farasan Islands, Saudi Arabia.

机构信息

Max-Planck-Institute for the Science of Human History, Jena, Germany.

University of York, Heslington, United Kingdom.

出版信息

PLoS One. 2019 Jun 12;14(6):e0217596. doi: 10.1371/journal.pone.0217596. eCollection 2019.

Abstract

During the past decade, over 3000 shell middens or shell matrix deposits have been discovered on the Farasan Islands in the southern Red Sea, dating to the period c. 7,360 to 4,700 years ago. Many of the sites are distributed along a palaeoshoreline which is now 2-3 m above present sea level. Others form clusters with some sites on the shoreline and others located inland over distances of c. 30 m to 1 km. We refer to these inland sites as 'post-shore' sites. Following Meehan, who observed a similar spatial separation in shell deposition in her ethnographic study of Anbarra shellgathering in the Northern Territory of Australia, we hypothesise that the shoreline sites are specialised sites for the processing or immediate consumption of shell food, and the post-shore sites are habitation sites used for a variety of activities. We test this proposition through a systematic analysis of 55 radiocarbon dates and measurement of shell quantities from the excavation of 15 shell matrix sites in a variety of locations including shoreline and post-shore sites. Our results demonstrate large differences in rates of shell accumulation between these two types of sites and selective removal of shoreline sites by changes in sea level. We also discuss the wider implications for understanding the differential preservation and visibility of shell-matrix deposits in coastal settings in other parts of the world extending back into the later Pleistocene in association with periods of lowersea level. Our results highlight the importance of taphonomic factors of post-depositional degradation and destruction, rates of shell accumulation, the influence on site location of factors other than shell food supply, and the relative distance of deposits from their nearest palaeoshorelines as key variables in the interpretation of shell quantities. Failure to take these variables into account when investigating shells and shell-matrix deposits in late Pleistocene and early Holocene contexts is likely to compromise interpretations of the role and significance of shell food in human evolutionary and socio-cultural development.

摘要

在过去的十年中,在红海南部的法萨尼群岛上发现了 3000 多个贝壳丘或贝壳基质沉积物,其年代可追溯到公元前 7360 年至 4700 年。许多遗址分布在一条古海岸线沿线,该海岸线现在高出现在海平面 2-3 米。其他遗址形成集群,其中一些位于海岸线,另一些位于内陆,距离海岸线 30 米至 1 公里不等。我们将这些内陆遗址称为“后岸”遗址。继 Meehan 在她对澳大利亚北部 Anbarra 贝壳采集的民族志研究中观察到贝壳沉积的类似空间分离之后,我们假设海岸线遗址是专门用于处理或立即食用贝壳食物的场所,而后岸遗址是用于各种活动的居住场所。我们通过对 55 个放射性碳日期的系统分析以及对包括海岸线和后岸遗址在内的各种位置的 15 个贝壳基质遗址进行挖掘来测量贝壳数量,从而验证了这一假设。我们的研究结果表明,这两种类型的遗址之间贝壳积累率存在很大差异,并且由于海平面的变化,海岸线遗址被选择性地清除。我们还讨论了在世界其他地区与海平面较低时期相关的更广泛的意义,即理解沿海地区贝壳基质沉积物的差异保存和可见性的问题。我们的研究结果强调了后沉积退化和破坏、贝壳积累率、除贝壳食物供应以外的其他因素对遗址位置的影响以及沉积物与最近古海岸线的相对距离等埋藏因素在解释贝壳数量方面的重要性。如果在研究晚更新世和全新世早期的贝壳和贝壳基质沉积物时不考虑这些变量,那么对贝壳食物在人类进化和社会文化发展中的作用和意义的解释可能会受到影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/682f/6561681/09f42b0f1b01/pone.0217596.g001.jpg

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