Nicolás Batalla, Mercedes Okumura, Casimiro S. Munita, Charles French, Astolfo G. M. Araujo
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引用次数: 0
Abstract
Geoarchaeological studies, particularly those incorporating micromorphology and associated techniques, have revealed the complex depositional and post-depositional history of mollusk shell-matrix archaeological sites, mostly in coastal areas where these sites are more widespread. But geoarchaeology can also be crucial to disentangle human and natural agencies in inland shell-rich settings, including caves and rock-shelters. In this paper, the site formation processes of the land snail-rich Maximiano Rockshelter, located in the karstic upper Ribeira de Iguape River valley of southern São Paulo state, Southeast of Brazil, are tackled. Embedded in the neotropical Atlantic Forest, the site contains lithics, bone artifacts, and faunal and human remains dating between ~11,165 and 1282 cal year B.P. Facies and microfacies were characterized in exposed stratigraphic profiles through micromorphology, particle size analysis, major, minor, and trace elements, and FTIR spectroscopy. Despite the strong humification affecting most of the site, results indicate deposits resulting from anthropic activities such as the dumping of land snail shells and other remains, the tossing of entire and fragmented shells in sub-horizontally distributed layers, primary combustion features, and dumping/sweeping of combustion-derived materials. Shell-bearing facies exhibit similarities with chronologically contemporaneous Ribeira de Iguape basin's riverine sambaquis.
地质考古研究,特别是结合微观形态学和相关技术的研究,揭示了软体动物壳基质考古遗址的复杂沉积和沉积后历史,这些遗址大多分布在沿海地区。但是,地质考古学对于理清内陆贝壳丰富的环境(包括洞穴和岩石避难所)中人类和自然的关系也至关重要。本文研究了位于巴西东南部圣保罗州南部Ribeira de Iguape河上游喀斯特河谷的富含陆生蜗牛的Maximiano Rockshelter的遗址形成过程。该遗址位于新热带大西洋森林中,包含距今11,165 ~ 1282 cal年的石器、骨制品、动物和人类遗骸。通过显微形貌、粒度分析、主、次、微量元素和FTIR光谱,在暴露的地层剖面中对相和微相进行了表征。尽管大部分地区受强烈的腐殖化作用影响,但结果表明,人类活动导致了沉积物的沉积,如倾倒陆地蜗牛壳和其他遗骸,在亚水平分布的层中抛掷完整和破碎的贝壳,初级燃烧特征以及燃烧衍生物质的倾倒/清扫。含壳相与同期Ribeira de Iguape盆地的河流sambaquis具有相似之处。
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.