闽江下游黄岐屿遗址的光释光测年

为了更好地理解闽江下游的连江县黄岐屿遗址的环境背景和考古年代,在已有AMS¹⁴C年代学研究的基础上,选择黄岐屿遗址的T2剖面进行年代学样品采样,在室内运用中颗粒石英的单片再生剂量法进行光释光年代学研究。结果表明：黄岐屿遗址地层的OSL埋藏年龄范围为8.5±0.5－4.4±0.2 ka,属于早－中全新世阶段的沉积/文化地层。其中2019118样品的年龄为4.4±0.2 ka,属于昙石山文化,与AMS¹⁴C年龄相当;2019117样品年龄为5.7±0.3 ka,可能存在年龄的高估;2019119样品的年龄为8.5±0.5 ka,受采样环境的影响,该地层的OSL埋藏年龄可能指示遗址底界的最大年龄。对比黄岐屿遗址所在的福州盆地地貌和环境演化过程以及区域史前人类活动发现,该遗址对应6 500－4 000 a B P的大暖期气候和相对高海面时期,该时期福州盆地发育了众多的同时期的史前遗存,区域内产生了繁荣的昙石山文化和昙石山下层文化。新石器时代末期4.2－4.0 ka气候突变的冷事件、4 000－3 000 a B P太平洋两岸热带－亚热带地区的气候环境的急剧变化以及北方吴越文化的侵入可能是造成该遗址缺失后续文化遗存的原因。     

南极红酵母AN5的发酵及对海参体成分的影响

红酵母是海洋酵母中的常见种类,在水产养殖中常作为微生态制剂。本实验以第22次南极考察从海冰中分离的红酵母AN5为研究对象,对酵母菌的发酵生长条件进行了优化,结果表明,红酵母培养的最佳碳源和氮源分别为2%的糖蜜和0.5%的酵母粉,最适装液量为50 m L/250 mL,摇瓶转速为140 r·min~(–1),培养基初始pH=3.0,20℃下可获得最佳培养,此时酵母发酵密度可达5.81×10~7 cells·mL~(–1)。发酵后测得酵母中水分含量为69.15%,干酵母蛋白质含量为42.00%,多糖含量为32.08%,脂肪含量为0.39%。在幼参养殖过程中以0.3 g(湿重)·m~(–3)水体的用量投喂极地红酵母,养殖2个月后,与对照相比,幼参体内水分和脂肪含量基本没有变化,而蛋白质和多糖含量明显升高。因此,极地红酵母可大量发酵生产,作为微生态制剂应用于海参的养殖中。     

外来饮食文化影响下广州本地居民地方身份建构过程的代际差异

伴随着地理学的文化转向以及“身体”“情感”视角的引入,饮食文化的空间问题开始引发人文地理学界的关注。借助身份建构过程模型理论（identity process theory, IPT）,依托对38位广州本地人的深度访谈,阐释外来饮食文化对其身份建构过程的影响及代际差异。研究发现,外来饮食文化的涌入引发了老一辈广州人多重的身份危机感,激发他们投身于地方传统饮食文化复兴实践,以对传统的忠诚和坚守来建构其地方身份。而自幼就被外来及本土饮食文化共同包围的年轻人则善于在不同情境下采纳不同文化态度和策略来建构其地方身份,缓解身份危机。该代际差异折射出饮食文化空间政治结构的轮回,而恰恰是这一空间政治的轮回孕育了地方饮食文化的继替。     

金钱鱼肾细胞系的建立及生长特性研究

金钱鱼(Scatophagus argus)是一种重要的广盐性海水养殖鱼类,可直接在海水、淡水、咸淡水等不同环境中正常生长。为研究金钱鱼独特的渗透调节机制,本文研究了金钱鱼肾细胞的原代和传代条件及其生长特性,结果表明:原代肾细胞在含有20%胎牛血清(FBS)的L-15培养基里贴壁和生长较好,添加10ng/mL的碱性成纤维细胞因子(basic fibroblast growth factor)bFGF能明显促进细胞增殖,传代细胞采用含有10%胎牛血清的L-15培养基,细胞生长迅速,3—4d即可传代。金钱鱼肾细胞为成纤维样细胞,命名为SK细胞,目前已传至22代。扩增第11代SK细胞的细胞色素氧化酶I(COI)基因,比对结果证明此细胞系来源于金钱鱼。采用CCK-8法检测第12代细胞在低渗(95,137,200mmol/kg),等渗(330mmol/kg)和高渗(430,550mmol/kg)中的增殖情况,结果发现肾细胞在137—430mm/kg的渗透压范围内均可增殖,说明金钱鱼肾细胞对渗透压的耐受性较强。本试验首次建立了金钱鱼肾细胞系,并初步证明了肾细胞对盐度有较强的耐受性,为今后渗透压调节的深入研究奠定了基础。     

The Influence of Culture on Wildfire Mitigation at Peavine Métis Settlement,Alberta, Canada

This article presents findings of a study that explored how culture influenced support for wildfire mitigation in Peavine Métis Settlement, an Aboriginal community located in Alberta, Canada. Community-based research was completed using interviews, focus groups, and participant observation. The results show that cultural factors appeared to influence wildfire mitigation preferences. Participants indicated the current state of the forest was not natural, and that mitigation activities would likely improve forest health. Participants supported Settlement Council-led wildfire mitigation activities at both the residential and community level due to a preference for communal action and collective problem solving. Participants also were found to distrust “outsiders” and preferred programs developed by members of their own community. The results of this study show that wildfire mitigation programs based on local culture can be well supported in an Aboriginal community.     

基于SLQAS的上海石库门里弄保护与更新研究

基于GIS构建上海里弄查询分析系统(SLQAS),并对2006—2012年上海内环线以内210个地块石库门里弄的更新进程分析发现,石库门更新呈现出显著的行政逻辑,位于街道中心的石库门率先更新,而后才涉及街道边界的石库门,为此,要加强街道边界地区、综合价值较高的石库门里弄管理,并进一步划定保护与更新范围,创新保护更新的方法和模式,强化政府、企业、公众等各主体对城市更新的参与。期待对我国城市更新及其文脉传承等有所裨益。     

全新世浙江地区气候变化对史前文化的影响(英文)

The temporal-spatial distribution features of prehistoric cultures since the Holocene in Zhejiang region were comparatively analyzed based on GIS spatial analysis. Results show that the prehistoric cultures expanded gradually in this region before 4000 cal. a BP. The notable expansions occurred twice, one in the Majiabang-Hemudu cultural period, the other in the Liangzhu cultural period. Meanwhile, the prehistoric cultures were disseminated from west to east coast along river valleys. After 4000 cal. a BP, as represented by the Maqiao Culture, the distributed area of each prehistoric culture contracted. This is obviously due to the termination of spreading trends to east coast, which was simultaneously accompanied by two different modes of production and economic transitions in the north and south Zhejiang region respectively. The distribution of prehistoric cultures was closely related with Holocene sea-level fluctuations, especially on the banks of Hangzhou Bay, where the distribution changes of prehistoric cultural sites were greatly affected by sea-level changes, with the closest relationships between them. After 7000 cal. a BP, the process of lowered sea-level and regression-epeirogenesis provided wider terrestrial living spaces for prehistoric inhabitants. Based on the comparative analyses of the changes of prehistoric cultures and the environmental evolution information recorded in the Qianmutian subalpine peat of Mt. Tianmu and muddy area on the inner shelf of the East China Sea, it is indicated that the changes of prehistoric cultures were synchronized with environmental changes in Zhejiang region. Before 4000 cal. a BP, the eastward expansion of prehistoric cultures in Zhejiang occurred under the background of the Holocene Optimum, and was the expansion and extension under the joint influences of agricultural civilization and maritime civilization. However, after 4000 cal. a BP, the geographical contraction of prehistoric cultures in Zhejiang occurred under the back-ground of dry-cold climate trend and deterioration of coastal marine environment. It is evidenced from the above fact that the development, expansion and contraction of prehistoric cultures are positively correlated to environmental change. The change of the climatic environment is just the underlying reason for these changes and transitions of production modes and economic forms. Therefore, the climatic environment is the dominant factor of prehistoric culture vicissitudes in Zhejiang region, which has exerted great influence on distribution, dissemination, expansion and transmutation of the culture.     

Impact of Holocene climate change on the prehistoric cultures of Zhejiang region,East China

The temporal-spatial distribution features of prehistoric cultures since the Holocene in Zhejiang region were comparatively analyzed based on GIS spatial analysis. Results show that the prehistoric cultures expanded gradually in this region before 4000 cal. a BP. The notable expansions occurred twice, one in the Majiabang-Hemudu cultural period, the other in the Liangzhu cultural period. Meanwhile, the prehistoric cultures were disseminated from west to east coast along river valleys. After 4000 cal. a BP, as represented by the Maqiao Culture, the distributed area of each prehistoric culture contracted. This is obviously due to the termination of spreading trends to east coast, which was simultaneously accompanied by two different modes of production and economic transitions in the north and south Zhejiang region respectively. The distribution of prehistoric cultures was closely related with Holocene sea-level fluctuations, especially on the banks of Hangzhou Bay, where the distribution changes of prehistoric cultural sites were greatly affected by sea-level changes, with the closest relationships between them. After 7000 cal. a BP, the process of lowered sea-level and regression-epeirogenesis provided wider terrestrial living spaces for prehistoric inhabitants. Based on the comparative analyses of the changes of prehistoric cultures and the environmental evolution information recorded in the Qianmutian subalpine peat of Mt. Tianmu and muddy area on the inner shelf of the East China Sea, it is indicated that the changes of prehistoric cultures were synchronized with environmental changes in Zhejiang region. Before 4000 cal. a BP, the eastward expansion of prehistoric cultures in Zhejiang occurred under the background of the Holocene Optimum, and was the expansion and extension under the joint influences of agricultural civilization and maritime civilization. However, after 4000 cal. a BP, the geographical contraction of prehistoric cultures in Zhejiang occurred under the background of dry-cold climate trend and deterioration of coastal marine environment. It is evidenced from the above fact that the development, expansion and contraction of prehistoric cultures are positively correlated to environmental change. The change of the climatic environment is just the underlying reason for these changes and transitions of production modes and economic forms. Therefore, the climatic environment is the dominant factor of prehistoric culture vicissitudes in Zhejiang region, which has exerted great influence on distribution, dissemination, expansion and transmutation of the culture.     

海洋贝类细胞培养技术及其应用

综述了海洋贝类细胞培养的意义以及国内外在贝类细胞培养的一些进展和应用,并总结了目前贝类细胞培养所存在的问题。以此为探索贝类细胞培养条件、方法,并最终成功建立细胞系提供参考。     

肇庆市旅游气象服务发展对策探讨

通过分析肇庆市旅游气象服务现状和存在问题,结合当地旅游资源和气候特征,探讨发展肇庆市旅游气象服务体系的思路,对提高肇庆市旅游气象服务能力和水平有着十分重要的意义。