墨西哥塞德罗斯岛Cerro Pedregoso遗址全新世早期人类活动的地质考古背景

IF 1.4 3区 地球科学 0 ARCHAEOLOGY
Loren G. Davis, Matthew R. Des Lauriers, Antonio Porcayo-Michelini, David B. Madsen, David Rhode
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引用次数: 0

摘要

在墨西哥下加利福尼亚州塞德罗斯岛的Cerro Pedregoso遗址的地质考古发掘中,发现了一个层状冲积扇沉积物,其中保存完好的证据表明,在距今约12,000至9600 cal BP之间的全新世早期,人类反复居住。我们使用来自多个挖掘单位的木材木炭和海洋贝壳的放射性碳定年法来建立这些早期沿海觅食者职业的安全年表。这些文化材料位于景观规模的沉积物3中,这是一个由冲积作用和风积作用共同形成的单元。在这个沉积物下面,一个以前未知的古土壤(S1),在第9单元的挖掘中暴露出来,表明存在更古老的沉积物,可能早于12,000 cal BP。虽然这个古土壤的考古内容很稀少,而且受到植物扰动的影响,但它为未来研究美洲最早的沿海活动提供了一个有希望的目标。因此,Cerro Pedregoso遗址提供了全新世早期人类活动的有价值的分层记录,并强调了在塞德罗斯岛的埋藏地貌中发现更早证据的可能性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Geoarchaeological Context of Early Holocene Human Occupation at the Cerro Pedregoso Site, Cedros Island, Mexico

Geoarchaeological excavations at the Cerro Pedregoso site on Cedros Island, Baja California, Mexico, uncovered a stratified alluvial fan deposit containing well-preserved evidence of repeated human occupation during the Early Holocene, between ~12,000 and 9600 cal BP. We used radiocarbon dating of wood charcoal and marine shell from multiple excavation units to establish a secure chronology for these early coastal forager occupations. These cultural materials lie within the landscape-scale Deposit 3, a unit formed by a combination of alluvial and aeolian processes. Beneath this deposit, a previously unknown paleosol (S1), exposed in excavation Unit 9, suggests the presence of even older sediments that may predate 12,000 cal BP. Although the archaeological content of this paleosol is sparse and affected by floralturbation, it offers a promising target for future investigations into the earliest coastal occupations of the Americas. The Cerro Pedregoso site thus provides a valuable stratified record of Early Holocene human activity and highlights the potential for even earlier evidence to be found in buried landforms on Cedros Island.

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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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