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81.
? Lawrence Butler & Jonathan Clark 《考古杂志》2013,170(2):423-442
The purpose of this short article is to put on record the archaeological observations made between 1990 and 2002 during the decade of stonework conservation on the northern run of the frieze panels on the west front of Lincoln Cathedral. It is not concerned with the frieze sculpture itself but with its stones and the spaces behind the stones. Equally, this article is not an assessment of the sculpture and its dating but is an archaeological investigation which potentially has wider implications for the sequence of construction and carving of the Romanesque frieze now visible at Lincoln. 相似文献
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Henry C. Clark 《History of European Ideas》2013,39(3):382-384
This article reflects on the relationship between historical writing and enquiry and philosophy, and more particularly the manner in which the pursuit of a particular natural philosophy can influence historical narratives. The article begins with a comparison of Roman and Greek approaches to history, employing a distinction between narrative and logic. It goes on to consider the impact of Christianity, the relationship between enlightenment narratives and philosophical developments regarding the nature of causation, and the Hegel/Marx critique of the kinds of empiricism associated with Hume. The article ends by considering the counterfactual historical analysis and the proper relationship between history and philosophy for modern historians. 相似文献
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Carol L. Clark 《Eurasian Geography and Economics》2013,54(2):88-112
The author examines the role played by the economic geography of the former Soviet Union in the evolution of labor relations in Russian industry, using the iron and steel industry as a case study. More specifically, three regional factors are analyzed as they affect enterprise economic strategies, organization, and management-labor relations: (1) the inherited industrial structure; (2) the degree of product specialization at the regional level; and (3) the level and sophistication of regional political and labor structures combined with the presence (or lack of same) of a “regional agenda.” These factors are examined within the context of a model predicting several possible variants of post-communist labor relations at the enterprise level. 36 references. 相似文献
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The paper reports fish bone and shellfish assemblages from Ulong Island in the Rock Islands of Palau, western Micronesia dating from ∼3100 to 500 BP . Use of marine resources in early prehistory appears to have been highly localised with increasing capture of outer‐reef/pelagic taxa including shark and tuna after 1000 BP . Local stocks of large Tridacnids were depleted during initial human use of Ulong Island, and there is a size decrease in Scarus sp. remains consistent with pressure on the inshore fishery, especially after establishment of permanent stonework villages in late prehistory. Comparison of archaeological assemblages of fish bone from other Rock Islands dated to after 2000 BP indicate that the captured fish species and major capture methods differ between sites and likely reflect local marine environments at each location. Copyright © 2010 John Wiley & Sons, Ltd. 相似文献
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Patrick G. Quilty Nicola Clark Ty Hibberd 《Alcheringa: An Australasian Journal of Paleontology》2013,37(2):200-206
Quilty, P.G., Clark, N. & Hibberd, T., 21.01.2015. Crenostrea sp. cf. C. cannoni (Marwick, 1928) (Bivalvia: Ostreacea) and associated fauna from east of Heard Island, Kerguelen Plateau: age and palaeoenvironmental value. Alcheringa 39, xxx–xxx. ISSN 0311-5518A well-preserved single left valve of a large oyster embedded in coarse volcaniclastic sediment and identified as Crenostrea sp. cf. C. cannoni (Marwick, 1928) was dredged from east of Heard Island, central southern Indian Ocean. It is accompanied by a fragment of the pectinid bivalve Austrochlamys sp. indet. and foraminifera. Austrochlamys sp. indet. and other bivalve fragments were analysed for 87Sr/86Sr, δ18O and δ13C, the results yielding an age of 17.5 Ma (later early Miocene) and a water temperature of ca 10°C. Foraminifera and sediment characteristics indicate that accumulation occurred in mid-continental shelf depths, at a location where nutrient supply was good.Patrick G. Quilty [p. quilty@utas. edu. au], School of Earth Sciences (Private Bag 79) and Institute for Marine and Antarctic Studies (IMAS: Private Bag 129), University of Tasmania, Hobart, Tasmania 7001, Australia. Nicola Clark [nc118@leicester. ac. uk], Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK. Ty Hibberd [ty. hibberd@aad. gov. au], Australian Antarctic Division, Channel Highway, Kingston, Tasmania 7050, Australia. 相似文献