世界文化遗产中国篇

中国申报并被批准的世界遗产有30处．其中有世界文化遗产21处、世界自然遗产4处、世界文化与自然遗产4处、文化景观1处。在这里．我们主要介绍21处世界文化遗产。     

全面落实科学发展观

去年第二期,本刊的卷首语是<确立科学的发展观>.如果从经济发展战略这一更高的层面回顾去年的工作,那么也可以说,其主线就是确立科学的发展观.贯穿全年的土地市场治理整顿,本质上就是治理整顿铺摊子、拼资源的粗放型经济发展模式;"三个暂停"的严厉措施,本质上就是对不可持续的经济发展模式实行"休克治疗".温家宝总理在日理万机中,关注到我省绍兴县"土地集约利用十法",因为这符合可持续发展的科学发展观,是方向.     

中国将设立国有土地收益基金

据透露．2005年政府将要设立国有土地收益基金。近年来．由于许多地方政府，片面追求政绩工程，到处圈地占地以地生财，把70年的土地收益用于本届政府土地开发和城市建设，导致许多中等城市，特别是东部城市现在已经没有地可卖．这样直接影响到了下届政府的土地收益，为此国家准备从今年开始设立国有土地建设资金，也就是将卖地收益纳入基金，为以后政府的使用做准备。     

地下权并非采矿权当然取得的产权界定

在矿业开发活动中,往往涉及采矿权、地下权、地表权以及产权界定、"负外部性"等诸多问题,其中采矿权取得时关于包裹矿产的地下土地部分产权应如何界定,已成为人们关注、讨论的重要问题.一直以来,许多学者却将地下权界定为采矿权的财产组成,即地下使用权随着采矿权的取得而当然取得.笔者则认为:地下权属相邻权,地下权并非采矿权当然取得的产权界定,采矿权取得时关于包裹矿产的地下土地部分应是采矿权人与地表权人共同拥有的互有物.     

生肖鸡的传说

鸡，在十二生肖中排行第十。因每天下午5～7点(即酉时)日落时鸡便归窝夜宿，故鸡的十二地支配属为“酉”。     

Silicon limitation on primary production and its destiny in Jiaozhou Bay, China——Ⅳ：Study on cross-bay transect from estuary to ocean

The authors analyzed the data collected in the Ecological Station Jiaozhou Bay from May 1991 to November 1994, including 12 seasonal investigations, to determine the characteristics, dynamic cycles and variation trends of the silicate in the bay. The results indicated that the rivers around Jiaozhou Bay provided abundant supply of silicate to the bay. The silicate concentration there depended on river flow variation. The horizontal variation of silicate concentration on the transect showed that the silicate concentration decreased with distance from shorelines. The vertical variation of it showed that silicate sank and deposited on the sea bottom by phytoplankton uptake and death, and zooplankton excretion. In this way, silicon would endlessly be transferred from terrestrial sources to the sea bottom. The silicon took up by phytoplankton and by other biogeochemical processes led to insufficient silicon supply for phytoplankton growth. In this paper, a 2D dynamic model of river flow versus silicate concentration was established by which silicate concentrations of 0.028–0.062 μmol/L in seawater was yielded by inputting certain seasonal unit river flows (m³/s), or in other words, the silicate supply rate; and when the unit river flow was set to zero, meaning no river input, the silicate concentrations were between 0.05–0.69 μmol/L in the bay. In terms of the silicate supply rate, Jiaozhou Bay was divided into three parts. The division shows a given river flow could generate several different silicon levels in corresponding regions, so as to the silicon-limitation levels to the phytoplankton in these regions. Another dynamic model of river flow versus primary production was set up by which the phytoplankton primary production of 5.21–15.55 (mgC/m²·d)/(m³/s) were obtained in our case at unit river flow values via silicate concentration or primary production conversion rate. Similarly, the values of primary production of 121.98–195.33 (mgC/m²·d) were achieved at zero unit river flow condition. A primary production conversion rate reflects the sensitivity to silicon depletion so as to different phytoplankton primary production and silicon requirements by different phytoplankton assemblages in different marine areas. In addition, the authors differentiated two equations (Eqs. 1 and 2) in the models to obtain the river flow variation that determines the silicate concentration variation, and in turn, the variation of primary production. These results proved further that nutrient silicon is a limiting factor for phytoplankton growth. This study was funded by NSFC (No. 40036010), and the Director's Fund of the Beihai Sea Monitoring Center, the State Oceanic Administration.     

我国西北高原盆地全新世沉积与环境变迁

本文通过对我国西北高原、盆地全新世黄土、古土壤、风沙层,冰缘层、冰碛层、盐(?)沉积、人类聚落位置迁移,植被演变等系统分析,论证了全新世气候和环境变化规律。认为(?)新世包含六个气候变化阶段,构成了三个冷干——暖湿气候旋回,每一旋回的周期大约为3600或3700年。