塞萨洛尼基湾东部的海岸变化和人类活动:通巴戈纳的地质考古调查

IF 1.4 3区 地球科学 0 ARCHAEOLOGY
Jakub Niebieszczański, Iwona Hildebrandt-Radke, Janusz Czebreszuk, Cezary Bahyrycz, Konstantinos Vouvalidis, Georgios Syrides, Panagiotis Tsourlos, Maria Pappa, Stylianos Andreou
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引用次数: 0

摘要

爱琴海地区全新世海侵对史前社会产生了重大影响。Toumba Gona是位于塞萨洛尼基湾以东的Anthemous河口的一个遗址。根据早期的研究,该遗址最多可以追溯到早期青铜器时代的晚期。然而,通过电阻率断层扫描、振动岩心、沉积学分析和放射性碳测年等地质考古研究表明,该遗址的直接邻近见证了公元前3000-2500年的最大海侵,以及公元前3000年之前的人类居住阶段,即海侵之前。由于三角洲的淤积,海岸线开始后退,这导致在通巴以南形成了广阔的沼泽。自公元前4世纪末以来,河流活动的增加与赞美斯河湾头三角洲的退化有关。在海侵之前和之后都记录了人类的活动,从而表明人类在海岸线环境中持续存在。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Coastal changes and human occupation in the eastern part of Thessaloniki Bay: Geoarchaeological investigations of Toumba Gona
The Holocene marine transgression in the Aegean Sea area has significantly impacted prehistoric societies. Toumba Gona is a tell site located at the mouth of the Anthemous River, east of Thessaloniki Bay. According to earlier research, the site should be dated at most to the late stage of the Early Bronze Age. Geoarchaeological research by means of electrical resistivity tomography, vibra‐coring, sedimentological analysis, and radiocarbon dating shows, however, that the direct proximity of the site witnessed the maximum marine transgression around 3000–2500 BC and the human habitation phase before the 3rd millennium BC, before the transgression. The coastline began to recede due to the delta progradation, which resulted in the formation of extensive marshes to the south of the Toumba. The increased fluvial activity since the end of the 4th millennium BC is relatable with the progradation of the Anthemous River's bay head delta. Human occupation was recorded before and after the marine transgression thus suggesting human persistence in the coastline environment.
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来源期刊
Geoarchaeology-An International Journal
Geoarchaeology-An International Journal 地学-地球科学综合
CiteScore
3.60
自引率
5.90%
发文量
51
审稿时长
>12 weeks
期刊介绍: Geoarchaeology is an interdisciplinary journal published six times per year (in January, March, May, July, September and November). It presents the results of original research at the methodological and theoretical interface between archaeology and the geosciences and includes within its scope: interdisciplinary work focusing on understanding archaeological sites, their environmental context, and particularly site formation processes and how the analysis of sedimentary records can enhance our understanding of human activity in Quaternary environments. Manuscripts should examine the interrelationship between archaeology and the various disciplines within Quaternary science and the Earth Sciences more generally, including, for example: geology, geography, geomorphology, pedology, climatology, oceanography, geochemistry, geochronology, and geophysics. We also welcome papers that deal with the biological record of past human activity through the analysis of faunal and botanical remains and palaeoecological reconstructions that shed light on past human-environment interactions. The journal also welcomes manuscripts concerning the examination and geological context of human fossil remains as well as papers that employ analytical techniques to advance understanding of the composition and origin or material culture such as, for example, ceramics, metals, lithics, building stones, plasters, and cements. Such composition and provenance studies should be strongly grounded in their geological context through, for example, the systematic analysis of potential source materials.
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