Burial offerings in intramural tombs at Middle Bronze Age Megiddo

Tel Megiddo is a major type-site for the Middle Bronze in the Levant. During this period a new burial custom appeared in which the dead were interred beneath occupied houses. This tradition is well attested in Area K at the site. Area H, near the palatial complex, revealed a monumental masonry-constructed chamber tomb. This article presents the results of residue analysis conducted on ceramic vessels placed in these tombs as burial offerings. Hundreds of intramural Middle Bronze tombs with ceramic offerings were excavated in the Levant, but this is the first time the content of the vessels is revealed.     

A Persistent Place for Hunter-Gatherers During the Late Holocene: The Case of Burials in Pit on the Coast of Lángara Bay,Argentine Patagonia

In Argentine Patagonia, the type of archaeological burial “in pit” has been only identified on the coast of Lángara Bay. This modality is characterized by the presence of single and multiple primary burials. Studies on five human burials in pits are presented in this article. The aim is to compare the contexts of burials in pit at the site level and the spatial characteristics of their distribution in the Lángara Bay locality from a diachronic perspective. The approach focuses on mortuary practices and social relations of hunter-gatherer groups during the Late Holocene. A characterization of the burials, their chronologies, bioarchaeological determinations, stable isotope studies, and their spatial distribution are included. The results allow us to chronologically place the contexts between ca. 3000 and 2000 cal BP. A spatial pattern in the distribution of burials in the coastal landscape was identified. Finally, it is proposed that this part of the Patagonian coast was a persistent place of burials in pit.     

Hydrothermal dolomitization,mixing corrosion and deep burial porosity formation: numerical results from 1‐D reactive transport models

Major corrosion has been found at depth in carbonate hydrocarbon reservoirs from different geologic provinces. Fluid inclusion microthermometry and stable isotopic compositions of carbonate cements, predating major corrosion, constrain the interpretation of the evolution of parental fluids during progressive burial and prior to the major corrosion event. Post‐major corrosion mineral paragenesis includes pyrite (‐marcasite), anhydrite, kaolinite (dickite) and fluorite. Although the post‐corrosion mineral paragenesis represents minor volumes of rock, it may provide valuable insights into the post‐corrosion brine chemistry. Using reactive transport numerical models, the roles of cooling and/or mixing of brines on corrosion have been evaluated as controls for dolomitization, deep burial corrosion and precipitation of the post‐corrosion mineral paragenesis. Modelling results show that cooling of deep‐seated fluids moving upward along a fracture may cause minor calcite dissolution and porosity generation. Significant dolomitization along a fracture zone and nearby host‐rock only occurs when deep‐seated fluids have high salinities (4 mol Cl kg^?1 of solution) and Darcian flow rates are relatively high (1 m³ m^?2 year^?1). Only minor volumes of quartz and fluorite precipitate in the newly formed porosity. Moreover, modelling results cannot reproduce the authigenic precipitation of kaolinite (dickite at high temperatures) by cooling. As an alternative to cooling as a cause of corrosion, mixing between two brines of different compositions and salinities is represented by two main cases. One case consists of the flow up along a fracture of deep‐seated fluids with higher salinities than the fluid in the wall rock. Dolomite does not precipitate at a fracture zone. Nevertheless, minor volumes of dolomite are formed away from the fracture. The post‐corrosion mineral paragenesis can be partly reproduced, and the results are comparable to those obtained from cooling calculations. Minor volumes of quartz and fluorite are formed, and kaolinite‐dickite does not precipitate. The major outputs of this scenario are calcite dissolution and slight net increase in porosity. A second case corresponds to the mixing of low salinity deep‐seated fluids, flowing up along fractures, with high salinity brines within the wall rock. Calculations predict major dissolution of calcite and precipitation of dolomite. The post‐corrosion mineral paragenesis can be reproduced. High volumes of quartz, fluorite and kaolinite‐dickite precipitate and may even completely occlude newly formed porosity.     

郑州市南阳路家世界购物广场战国墓葬发掘简报

2003年10-12月,郑州市文物考古研究所配合基本建设,在郑州市南阳路家世界购物广场工程区发掘一批战国墓葬,出土大量随葬器物,以陶器为主,其年代为战国中、晚期。     

"虚拟"先人与十九世纪新加坡华人社会--兼论海外华人的"亲属"概念

在东南亚殖民地时代,"虚拟血缘"的组织原则对于华人移民社会的重组重建及其运作,具有重要的意义.本文以19世纪的新加坡为个案,考察华人移民如何透过埋葬先人的坟山组织建构"社群共祖"以整合华人社会,讨论东南亚华人虚拟的"先人"或"祖先"概念,进而思考海外华人的亲属研究问题.本文也讨论与比较了"虚拟血缘"组织原则在明代华南宗族"联宗"形态、台湾汉人社会发展早期的"合约式"宗族和东南亚华人坟山组织的不同运用.     

Agents in Inter-Action: Bruno Latour and Agency

This paper aims to describe Bruno Latour's contributions to the theory and methodology of agency in the Philosophy of Science and to apply them to the study of agency in archaeology. These contributions include an understanding of how artifacts or representations of the world emerge, what the best conditions to study them under are and how to understand the process of change they undergo. A case study using the Hopewell burial mounds of the Lower Illinois Valley will serve to demonstrate the application of this methodology.     

试论湖北地区的带龛楚墓

壁龛在各地楚墓中均有一定数量的发现,本通过综合分析湖北地区带龛楚墓的流行时期、分布区域、墓主身分、头向、随葬品及不同时期带龛楚墓的比例关系等,揭示湖北地区带龛楚墓的一般特征,并进而认为湖北地区带龛楚墓为庶民墓的埋葬形式之一,而非某一特定“族”的葬俗。     

论黄河流域先秦时期腰坑墓葬俗文化——兼说与长江流域同类墓葬俗的关系

腰坑墓流行于黄河流域中原地区的墓葬中,学者们多把对其研究的焦点集中在对这一葬俗文化起源问题的讨论上,并较一致地认为该葬俗最早起源于河南地区。本文对发现的有关材料进行梳理,围绕中原地区先秦时期腰坑墓的起源、用途、性质、发展演变等进行了分析,以澄清过去研究中存在的一些模糊认识。认为,腰坑墓的葬俗最早可以追溯到新石器时代,而其起源亦非河南地区。     

浅析广西西林县普驮铜鼓葬

广西西林县普驮发现的“铜鼓葬”是古句町一种较为特殊的葬俗,时代为西汉晚期至东汉初,其特殊的葬俗、独特而丰富的随葬品,暗示此类葬俗是专为某类特殊的人群使用。我们认为西林普驮铜鼓葬的主人身份是句町部落集合体中具有显赫权威的精神领袖－巫师。     

Mineral weathering in forest soils and its relevance to the preservation of the buried archaeological resource

There is more woodland in Britain now than for many centuries and considering many international climate change mitigation policies, woodland cover, both in Britain and internationally, is being promoted. However, neither the management of existing woodlands nor their expansion should be at the expense of important archaeological evidence. Due to the large number of known archaeological sites, the large areas of land with uninvestigated archaeological potential and the expanding woodland cover, suitable mitigation strategies need to be developed to allow preservation in situ of important sites. An understanding of how woodland soils and the buried archaeological resource interact is, therefore, essential. This paper utilises ongoing environmental research into the mineral weathering rates in forest soils and considers its application to artefact preservation. The study concludes that soil water pH, its movement, and the saturation of dissolved ions in the soil solution are major factors determining both mineral and artefact longevity. A simple guide to artefact longevity based on these properties is proposed and a geochemical model for predicting loss is tested. These tools could be applied to any soil or individual horizon irrespective of land-use.