西汉早期柿园墓四神云气图壁画保护研究（一）——历史与现状调查

壁画保护研究,多集中在正面的保护以及揭取方法和材料的选用。对壁画揭取选用材料性能的系统研究甚少。而对已揭取壁画的破坏与保护的研究更少。已揭取壁画的破坏包含壁画原有的破坏和揭取所用材料蜕变引发的破坏。已揭取壁画具有结构体系的复杂性和破坏类型的多样性,其破坏类型往往是交织在一起的。对此类壁画的保护修复应建立在全面调查、系统研究的理论框架上。其研究内容涉及多学科以及多类型材料和方法的综合运用,其调查内容,也须从壁画制作工艺、材料、环境、破坏类型、原有保护材料以及材料相互作用等方面界定。本工作对西汉早期柿园墓四神云气图壁画的历史状况和现状进行了全面调查。调查结果无疑对后续的研究、对认识壁画的破坏形式和性质具有重要的作用,更有助于实施对古代壁画的科学保护和修复。     

大兴新城北区12号地唐代墓葬发掘简报

2008年12月,北京市文物研究所在大兴新城北区12号地发掘唐代墓葬7座,出土各类文物15件,为研究本地区墓葬考古和历史文化提供了新的资料。     

北京大兴区杨各庄墓地发掘简报

2004年10月20日～11月7日,北京市文物研究所对北京大兴区青云店镇杨各庄墓地进行了考古发掘,清理辽代墓葬7座,出土器物37件,对研究辽代墓葬形制、葬俗以及社会经济状况具有较重要的意义。     

Reclip:more Kleinr?umige Klimaszenarien für ?sterreich

Der letzte Bericht des Intergovernmental Panel on Climate Change (IPCC 2007) erl?utert die weltweiten Auswirkungen des Klimawandels deutlich – allerdings aus globaler Sicht. Um zu kl?ren wie sich das regionale Klima in ?sterreich ver?ndern wird, wurde mit dem Projekt „reclip:more“ (Research for Climate Protection: Model Run Evaluation) eine erste kleinr?umige Datenbasis für Klimaschutz und Klimafolgenforschung für ?sterreich generiert. Klimaszenarien wurden mittels regionaler Klimamodelle (RCMs) für die Alpen als 10 × 10-Kilometer-Raster und mit anschlie?endem Downscaling für ?sterreich mit einer Zielaufl?sung 1 km entwickelt. Die RCMs wurden mit ERA-40 Reanalyse-Daten der Vergangenheit und Daten eines Zukunftsszenarios des globalen Klimamodells (GCM) ECHAM5 angetrieben, um retrospektive (1981 bis 1990) und künftige (2041 bis 2050) Klimadatens?tze für die Alpen zu berechnen und M?glichkeiten und Unsicherheiten der Modelle und Downscaling-Methoden für die Alpen zu evaluieren. Die nun vorliegenden Datens?tze und weitere, die im Folgeprojekt „reclip:century“ für alternative Treibhausgasszenarien bis 2100 berechnet werden, dienen dazu als Basis für Aussagen über ?kologische und sozio?konomische Entwicklungen im Hinblick auf den Klimawandel.     

Where East Meets West: The Formative in Mexico’s Central Highlands

Mexico’s Central Highlands form one of Mesoamerica’s fundamental cultural seams, a point of overlap between two traditions, one to the east and the other to the west. Although this area is usually included in the west, it can be more productively viewed as an interface, the physical space where people, goods, and ideas passed from one side to the other, and thus it holds many keys for our understanding of emerging social complexity in Mesoamerica. In reviewing the last two decades of Formative period (1500 BC–AD 100) research in this crucial territory, we focus on themes that reveal the variation and dynamism of interregional interaction, including the formation of regional traditions, exchange systems, and foreign “influence,” and others that help contextualize the events and processes of that time, like household studies and environmental degradation. We stress that this part of Mexico is undergoing relentless development so time is of the essence if we are to broaden our perspectives on social evolution in the Central Highlands. This issue cannot be resolved by rescue and salvage work because it requires long-term, interdisciplinary projects to unravel multifaceted problems.     

Evolution of small valley mire in central Poland as a result of hydroclimatic oscillations

This paper demonstrates the results of analyses of Cladocera, pollen, plant macrofossil, lithological and radiocarbon data recovered from a mire located in the Rawka River valley in central Poland. These studies permit to recognise the development of hydrology phases in Kopanicha mire and give insight into Holocene fluvial dynamics of the system; radiocarbon dating partly allowed da-ting of the patterns of Holocene valley floor development of the Rawka River. The Kopanicha mire was formed during the Atlantic period. At that time, an oxbow lake formed, becoming a mire during the Subboreal and possibly Subatlantic periods. The high sensitivity of the oxbow lakes, fens, fauna, and flora remains to climate variations - especially to changes in water level connected with the ag-gradation-erosion cycle of rivers - allows the reconstruction of the palaeoecological changes that oc-curred in the mire. The frequency and timing of hydroclimatic oscillations at Kopanicha show strong similarities to records from other sites in Poland. Changes in Cladocera frequency and plant assem-blages were mostly influenced by the Rawka River which controlled the hydrological regime of the mire. The main factors controlling the presence of Cladocera taxa were the water level and the pres-ence of favourable conditions in the mire (e.g. pH, vegetation). Most of the changes occurred in re-sponse to climate changes, but some of them were connected with local factors.