内蒙古自治区社区干预在新冠肺炎防控中的作用机制及影响因素探讨

社区作为基层自治组织以其独特的职能和地位对重大公共卫生事件防控产生影响。本文构建社区干预机制体系,并基于内蒙古社区防控新冠肺炎的实证分析,探讨社区干预在地区和城市、农牧区间的差异,结合问卷得分情况并运用主成分分析法分别探讨影响地区间、城市和农牧区社区干预的主要因素。研究发现：内蒙古中部地区社区干预表现突出,东部其次,西部最差,城市社区干预显著优于农牧区;组织架构和职能发挥对地区内的社区干预效果影响较大。城市社区干预以组织架构和职能发挥为主,内外联系为辅,农牧区社区干预强调组织架构和内外联系,职能发挥薄弱;社区干预依照“组织架构响应--自身职能发挥--内外联系建立”的机制推进。     

Commemorative events at destination memorials – a dark (heritage) tourism context

In the past, sites and events related to war and atrocities were viewed in the wider context of heritage tourism. The term ‘dark’ was added with the aim of recognising heritage sites closely related to death and suffering. Given that commemorative events as part of dark heritage are not prevalent in heritage and tourism literature, there is a need to understand the behaviour of visitors involved in visiting these sites or attending this type of event, which presents a special challenge. Public commemorations, especially those that mark particularly disturbing occurrences, such as ‘The Great School Hour’ – an event which is presented in the artistic form of a ‘school class’ – are unique form of tourist activity that has not been thoroughly investigated previously. Thus, the aim of the study is to explore the influence of the main motivators on revisit intention and willingness to recommend for those who attended the commemorative event ‘The Great School Hour’ in Kragujevac, Serbia, with a particular focus on younger people. The results suggest that learning, emotional response and uniqueness have a significant positive effect on revisit intention, while emotional response and uniqueness have a significant positive effect on willingness to recommend.     

The Late Upper Palaeolithic Occupation of the Moroccan Northwest Maghreb During the Last Glacial Maximum

New work at Kehf el Hammar Cave provides the first well-dated palaeoenvironmental sequence for the Late Upper Palaeolithic in this region of the northwest Maghreb. The archaeological layers are dated via a combination of AMS radiocarbon and luminescence dating methods. The sequence contains charcoal-rich occupation layers with faunal, human and lithic finds. Local vegetational patterns are reconstructed on the basis of preliminary analysis of the charcoal evidence. Using standard calibration curves the AMS radiocarbon dates are compared with proxy evidence for climatic change from sea core records in the Alborán Sea. These appear to show that the Late Upper Palaeolithic occupation of the region coincides closely with Heinrich Event 1, a period marked by intense aridification and dating to ca. 16,700–17,250 calendar years ago.Les nouvelles recherches dans la grotte de Kehf el Hammar ont permis d’obtenir la première séquence paléoenevironnementale bien datée du Paléolithique supérieur tardif au Nord Ouest du Maghreb. En effet, les niveaux archéologiques ont été datés par le radiocarbone par accélérateur (AMS) et des méthodes radiométriques basées sur la luminescence. En revanche, les paléoenvironnements végétaux ont été partiellement reconstitués à base des premières analyses des charbons de bois. Les dates AMS calibrées ont été comparées aux données climatiques issues des carottes marines dans la mer Alborán. Ainsi, les occupations humaines du Paléolithique supérieur tardif dans la région ont sensiblement coïncidé avec l’événement climatique Heinrich 1. Celui-ci correspond à une période qui a été marquée par une aridification intense entre 16.700 et 17.250 ans (cal.).     

Mortality date estimation using fetal pronghorn remains

Pronghorn (Antilocapra americana) fetal remains are sometimes recovered from archaeological contexts. Pronghorn have consistent reproductive schedules so their remains may provide information on seasonality of site occupation and number of mortality events. To investigate the reliability of fetal remains for seasonality and mortality event assessment, bone size and tooth eruption were measured in a sample of modern fetal pronghorn remains with known mortality dates. Results indicate a strong correlation between bone size and mortality date, but no significant correlation between tooth eruption level and mortality date. Fetal bone size was used to estimate a late April or early May mortality date at both the Oyster Ridge (48UT35) and Trappers Point (48SU1006) archaeological sites. The number of mortality events at Trappers Point was also investigated. Copyright © 2007 John Wiley & Sons, Ltd.     

The Temperature Response in the Ring Widths of Phyllocladus Aspleniifolius (Celery–top Pine) Along an Altitudinal Gradient in the Warra LTER Area,Tasmania

The temperature response of four Phyllocladus aspleniifolius (Celery–top Pine) sites along an altitudinal gradient within a cool temperate broad leaf forest environment in the southwest of Tasmania, Australia was examined. Although strong evidence of a systematically changing response with elevation could not be found, there was evidence that minimum temperature in particular may be important in determining the altitudinal extent of the species. Climatic responses of the Warra LTER (Long Term Ecological Research) area sites were representative of other known sites in southwestern Tasmania. A link between event years in P. aspleniifolius and warm/dry conditions indicates that these event years may provide a guide to the historical frequency of fire weather in Tasmania’s southwest.     

基于“主体功能”的新型村镇建设模式优选及聚落体系重构——藉由“图底关系理论”的探索

新型村镇建设与主体功能区规划是分别针对我国当前阶段乡村发展、国土开发的重要空间调控手段,基于主体功能思维而对聚落体系进行自上而下的分类指导应该作为促进乡村聚落有序发展的重要思维。论文借助于图底关系理论,将主体功能区作为"均质面集"的发展意图转译到县级单元内"异质面集"的主导土地用途区,并进一步聚焦到"点集"乃至"点"层面的村镇聚落体系组织与聚落建设,总结了三类主体功能区的7种主导新型村镇建设模式及对应的空间优化目标,拓展了主体功能区规划在县级以下尺度的规划指导价值,实现了不同尺度空间规划的法则演绎,为主体功能区格局下我国县域尺度的村镇聚落功能优化与体系重构提供一种思路。     

城市事件旅游活动的地域差异

城市事件旅游策划形式、类型、内容、强度等多方面都存在着明显的地域差异。城市规模大小、经济发展水平、政治化背景以及旅游竞争力因子等,会对事件旅游的发生、发展产生深刻的影响。     

Policy Change and Learning in Response to Extreme Flood Events in Hungary: An Advocacy Coalition Approach

In an analysis of the 200‐year history of flood management in Hungary, I use the advocacy coalition framework and the focusing event literature to examine what policy change occurs and what is learned as a result of experiencing extreme and damaging flood events. By analyzing the policy response to a series of extreme floods (1998–2001) in this newly democratizing nation, I attempt to identify the factors that influenced the occurrence of policy change and policy‐oriented learning. In 2003, Hungary enacted a comprehensive flood management program that included economic development and environmental protection goals, a distinct departure from Hungary's historical structural approach to flood management. However, it is less clear that long‐lasting changes in belief systems about how floods should be managed have occurred. In this analysis, I argue that processes external to the flood policy subsystem (e.g., process of democratization and Hungary's accession to the European Union), along with the occurrence of the extreme flood events, enabled a coalition of individuals and organizations to press for policy change.     

Remarks on the pattern of septal insertion in rugose corals

Wang, G., Percival, I.G. & Li, R., 25.2.2015. Remarks on the pattern of septal insertion in rugose corals. Alcheringa 39, xxx–xxx. ISSN 0311-5518

Well-preserved specimens of the Hirnantian (latest Ordovician) rugose coral Lambeophyllum? corniculum He from the Yangtze Platform of South China, clearly show how catasepta (minor septa) are inserted, confirming the model proposed by Weyer in the 1970s. Our observations indicate the insertion of counter lateral septa and their neighbouring catasepta on the counter side takes place in exactly the same manner as that of the subsequent metasepta and catasepta. We propose abandoning the use of the term counter lateral septa. Therefore, exclusion of the pair of counter lateral septa reduces the number of protosepta from six to four.

Guangxu Wang [gxwang@nigpas.ac.cn], State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (CAS), 39 East Beijing Road, Nanjing 210008, PR China; Ian G. Percival [ian.percival@trade.nsw.gov.au], Geological Survey of New South Wales, 947–953 Londonderry Road, Londonderry, NSW 2753, Australia; Rongyu Li [lir@brandonu.ca], Department of Geology, Brandon University, Manitoba R7A 6A9, Canada.