旅游视角下的上海F1大奖赛

F1作为世界三大赛事之一,将于2004年9月正式在中国举办上海大奖赛。F1大奖赛凭借其巨大的影响力,将为上海带来众多的社会经济效应。本文阐述了F1旅游活动的游客动机以及细分市场,分析了相关行业在F1旅游中的作用;同时,从城市旅游形象、旅游环境、基础设施、旅游经济、旅游产品几个方面论证了F1大奖赛是上海旅游发展的新极点。     

从卜辞看洹北商城一号宫殿的性质

将卜辞中有关宗庙的祭祀活动和祭祀场所资料与洹北商城一号宫殿基址的祭祀遗存相对照,内涵基本相合,从而证明洹北商城一号宫殿为商王的宗庙.     

PINE RESINS AND POTTERY SEALING: ANALYSIS OF ABSORBED AND VISIBLE POTTERY RESIDUES FROM CENTRAL NEW YORK STATE*

Analysis was performed on absorbed and visible residues from 21 New York State prehistoric pottery sherds dating from 2905 ± 35 bp (Intcal04) (1256–998 cal bc ) to 425 ± 40 bp (Intcal04) (1417–1626 cal ad ). The use of pine resin was detected in 10 of 12 absorbed residue samples and 11 of 17 sherds subjected to visible residue analysis. It seems likely that the pots were resin‐sealed to make them more impermeable, constituting the first chemical evidence of extensive resin‐sealing in North America. A comparison of the results of absorbed and visible residues from eight of the sherds indicates that the two kinds of residue provide complementary evidence of vessel use.     

Age of the final Middle Palaeolithic and Uluzzian levels at Fumane Cave,Northern Italy,using C,ESR, U/Th and thermoluminescence methods

This article presents and discusses the chronological layout of the final Mousterian and Uluzzian levels of Fumane Cave in northern Italy using ¹⁴C, ESR and TL methods. Given its complex sedimentary and cultural succession, Fumane is a key site to assess the Middle–Upper Palaeolithic transition in Southern Europe and to explore Neanderthal behaviour and to compare it with the first Aurignacians. Large ranges defined by the ESR and TL dates cover the radiocarbon ages for units from A11 to A4, respectively, from 42.8 to 32.5 ka BP become progressively younger in agreement with the stratigraphy, despite high dispersions within the same unit. Our estimates using chronometric data seem to support the hypothesis that the sequence may cover almost 10,000 radiocarbon yr and that from comparison with the sedimentological and palaeoecological data, the late Middle Palaeolithic and the early Upper Palaeolithic at Fumane occur in sediments formed under moderately cool to mild climatic conditions correlated to the Hengelo-Interstadial, shifting towards cooler and drier conditions. Finally, comparisons between the Fumane data set and other sites in the North-Adriatic region are discussed.     

Phytolith-rich layers from the Late Bronze and Iron Ages at Tel Dor (Israel): mode of formation and archaeological significance

The presence of many phytolith-rich layers in late Bronze and Iron Age deposits at Tel Dor, Israel, are indicative of specific locations where plants were concentrated. Detailed studies of six of these phytolith-rich layers and associated sediments from Tel Dor show that the phytoliths were derived mainly from wild and domestic grasses. The most common domestic grass was the cereal Triticum aestivum (bread wheat). Three of these layers have a microlaminated microstructure, associated dung spherulites and phosphate nodules; characteristics that all point to the phytolith-rich layers having formed from dung in animal enclosures. In two of the layers, the microlaminated structure is absent while dung spherulites and phosphate nodules are present, suggesting that these too originate from dung that was not deposited in an enclosure. The sixth layer is microlaminated but does not contain spherulites. We thus cannot suggest a parsimonious explanation of its observed properties. Concentrations of burnt phytoliths are present in three locations, implying that dung was either burnt in situ or the ashes from burnt dung were redeposited. The transformation of dung accumulations into phytolith-rich layers involves a loss of organic material and hence a significant reduction in sediment volume, which is clearly apparent in the stratigraphy of some of the locations examined. The volume reduction can be observed in the macrostratigraphy and has important implications with regard to macrostratigraphic interpretation. The presence of abundant phytolith-rich layers on the tell has significant implications for the concept of ‘urbanism’ during these periods.     

Memory,Identity and Aspiration: Early Modern Jewish Maps of the Promised Land

In the sixteenth century Jews began to produce maps showing the Exodus to the Promised Land. My aim in this article is to show that, through unique compositions of written biblical references and pictured symbolism (both Jewish and Christian), maps such as the Mantua map (1560s) and, a century later, the Amsterdam Haggadah [Passover] map (1695) were a means of constructing Jewish cultural memory and identity in the Diaspora and fostering aspiration for a second salvation through a return to Zion. I also explore the Jewish approach towards the biblical land as this was reflected in the maps.     

The Fall of Thomas Howard, 1st Earl of Suffolk and the Revival of Impeachment in the Parliament of 1621

The revival of impeachment in 1621 has tended to be viewed exclusively through the prism of parliament. However, this article, which builds on the work of Professor Allen Horstman, suggests that a key factor in impeachment's revival was the dismissal of Lord Treasurer Suffolk for corruption in 1618. Suffolk's removal caused widespread disquiet, since it was assumed that senior officials held office for life. In order to silence these criticisms it proved necessary for the king not only to put Suffolk on trial but also to justify by precedent the lord treasurer's removal. This latter task was performed by the former lord chief justice, Sir Edward Coke, himself not long disgraced, whose researches in the medieval parliamentary record revealed the following year that errant crown ministers had hitherto been held to account by means of impeachment. Coke subsequently put this discovery to good effect when parliament met in 1621. Against the backdrop of mounting criticism against his hated rival, the lord chancellor, Francis Bacon, Coke revealed the existence of impeachment to the house of commons, whose attention was then focused on finding a way to punish the monopolists, Sir Giles Mompesson and Sir Francis Michell. In so doing, Coke not only aided the lower House, which had been struggling since 1610 to find a way of punishing non‐members, but also sought to settle an old score.     

乾隆朝清宫十八罗汉唐卡名相解析

藏、汉两地佛教经典及佛学之传播,直承印度晚出之大乘佛学,但罗汉信仰却在两地佛教中均占一席之地,尤其是于汉藏两地家喻户晓的十六罗汉(后演绎成十八罗汉),不仅与佛和菩萨一样成为信徒崇拜的对象,而且以之为题材的绘塑作品更是广泛流传,及至帝廷内苑亦多有供奉收藏。清乾隆时期为安抚蒙藏势力而极力推崇藏传佛教,此信仰尤以宫中为盛,帝室庋藏、绘制及供奉有大量藏风浓郁的十六或十八罗汉唐卡组画,其名称、图像特征、排列顺序乃至绘画风格等与清官旧藏的内地各派罗汉图相比,同中存异。乾隆帝及藏传佛教大师们在对藏密佛像进行大规模系统化与规范化的同时,也涉及了汉藏两地十分流行的十六、十八罗汉,并在此基础上逐渐形成了具有乾隆时期清宫特色的十八罗汉图像标准。     

Arade River Archaeological Complex: Dredges and Archaeology

Situated on the southern coast of Portugal, the Arade River mouth has been visited and inhabited for over three millennia. Dredging operations, in the first and last decades of the 20th century, brought up the importance of Arade's cultural heritage and triggered a large-scale project of study, survey, and archaeological excavation. This project is conducted by Centro Nacional de Arqueologia Náutica e Subaquática, the Portuguese agency for nautical archaeology, under the direction of Francisco Alves, and with the support of both local and state authorities. This paper is a preliminary assessment of the finds made so far.
© 2005 The Nautical Archaeology Society     

GEOGRAPHICAL PATTERNS IN BIOLOGICALLY AVAILABLE STRONTIUM,CARBON AND OXYGEN ISOTOPE SIGNATURES IN PREHISTORIC SW GERMANY*

In order to interpret strontium and oxygen isotope values in Neolithic human skeletons analysed previously, we begin to map the biologically available strontium, carbon and oxygen isotopic signatures of prehistoric southern Germany by analysing tooth enamel of pigs from archaeological sites distributed around the region. The mapping shows a marked upland–lowland difference in biologically available ⁸⁷ Sr/ ⁸⁶ Sr values, ranging between 0.7086 and 0.7103 in the sedimentary lowlands, and from 0.710 to as high as 0.722 in the crystalline uplands of the Odenwald, the Black Forest and the Bavarian Forest. In addition, carbon isotopes in the carbonate fraction of pig enamel were generally about 1–2 more enriched in ¹³ C in the uplands. Despite the expected depletion of ¹⁸ O with altitude, oxygen isotopes in pig enamel showed little correlation with site altitude, although for pig samples not older than the Iron Age there was some geographical correlation withδ¹⁸O patterns in modern precipitation.