Coastal wetland in South China： Degradation trends, causes and protection countermeasures

There are abundant coastal wetlands in South China and their main characters are the tidal flats, mangroves and coral reefs. In this paper, the status quo of coastal wetlands in South China is introduced and their degradation trends in the last decades are analyzed based on the existing literatures and information. Their degradation trends are characterized by reduction of coastal wetlands＇ area, pollution of seawater environment, degeneration of ecological environment, sharp decrease of biodiversity in the wetlands and so on. At the same time, the causes resulting in the above-mentioned degradations are discussed, mainly concluding imperfect systems of management and legislation, deficient property and assessment systems of the wetlands, weak consciousness of protecting coastal wetlands, shortage of basic study and backward management level and so on. Some countermeasures are put forward for the sake of a sustainable use of the coastal wetlands of South China, mainly including establishing and perfecting administrative and legal systems for the coastal wetlands, developing the study on assessment of coastal wetland, heightening the consciousness of public participation, and strengthening scientific research and establishment of wetland nature reserves.     

感受帕隆天险

青藏高原既是世界上最高的高原,同时也是地球上最年轻的高原.专家们通过地质历史考察发现,早在400多万年前,现在的青藏高原南部还是汪洋一片,后来受来自印度板块次大陆与欧亚主大陆碰撞的影响,致使青藏高原逐步隆起.     

台风Utor登陆广东过程的数值研究

台风Utor(0104)于2001年7月6日00时(UTC,下同)在广东汕尾地区登陆,带来比较严重的灾害性天气.以美国国家大气研究中心和宾州大学联合研制的第五代中尺度模式(MM5)为基础设计的台风预报模式比较准确地预报出台风Utor(0104)的移动路径(前24 h的移动路径平均误差为 68 km)和天气现象的分布.在此基础上,设计了3个敏感性试验:①是把华南地区(26°N以南,110°E以东)的陆地变为海洋,②是把华南地区的山地变为平地,③是减小华南地区陆地的粗糙度,即取为近似于静风的洋面上的值.对比数值试验的结果表明:引起台风登陆后减弱的最主要因子是下垫面水汽供应的切断,其次是下垫面粗糙度(摩擦)的影响;地形作用能使迎风坡的降水明显增加,但对台风强度则没有明显的影响.     

走向深海大洋:揭开地球的隐秘档案

深海大洋到底有何奥秘?人类面临能源危机，为何要走向深海大洋?同济大学海洋地质系教授、中科院院士汪品先在2004科协年会上做了题为《走向深海大洋》的报告，初步揭开了深海大洋的神秘面纱。汪品先院士从地球演变历史及海洋板块说切入，探究深海大洋神奇海底的世界。     

"虚实结合"的华南技术交易网

一、我省技术交易现状 近几年随着长江三角洲等经济区崛起、西部地区大开发的实施,广东原有的政策优势与地理的优势已逐步减弱,广东的企业需要重新树立新的优势,就必须加强技术引进、技术开发及技术创新,加快进入国际市场。     

C－isotope composition and significance of the Sinian on the Tarim plate

102 samples of limestones,mudrocks shales and tillites from the Sinian in Kuluketage have been analyzed ,Four formations in the Sinian belong to glacial deposits in which the differences in δ^13C are distinct (-14.7‰- 4.2‰),Distinctly negative δ^13C excursions for three times support the viwe of three glacial deposits in this area suggested by previous authors,except for the durations of them ,δ^13C values are generally positive in the Beiyixi Formation of lower part of the Lower Sinian ,representing probably the rock records of a continental rift related to break-up of the Rodinian supercontinent,There are three times of distinct excursions of δ^13C curve in all strata,The first one is from positive values at the bottom to about -5‰ at the top of the Beiyixi Formation ,The second one,from 0‰-3‰ in the Arletonggou Formation of upper part of the Lower Sinian to -3.4‰---14.4‰ in the Teruiaiken Formation.The third one,from positive values in the Zhamoketi Formation of lower part of the Upper Sinian to negative values in glacial varves at the top of the Hankeerqiaoke Formation.     

缙云山华南黑桫椤种群的遗传多样性研究初探

从种群分化和保护生物学的角度出发，运用方差分析和聚类分析，对缙云山不同生境下的8个华南黑桫椤种群的形态分化进行研究，方差分析表明该种的形态特征对环境的可塑性较大，繁殖器官的变异小于营养器官，聚类分析表明8个种群间总体上无明显分化．     

强中纬力作用下地球板块的运移

以一个块体的理论运动轨迹特殊对象 ,分析在强中纬力作用下 ,地球板块在高纬度带 (6 8°2 7′～ 90°0 0′)、中纬度带 (2 1°33′～ 6 8°2 7′)、低纬度带 (南纬 2 1°33′～北纬 2 1°33′)内等不同地域的受强中纬力作用时的运动方向及其 F- t关系图 ,以及板块在随着地球的自转 ,作跨越赤道的运动情况。结果表明 :地球板块的运动特点随着纬度的变化而变化 ,强中纬力的主要控制因素为地球的黄纬 ;黄纬的变化发生在板块所受强中纬力变化的情况下 ,其外部现象表现为地球纬度的变化。这一结论为由特殊到一般的板块运动分析提供了理论依据     

华南几个杂岩体中产铀与非产铀花岗岩的成因及其与铀成矿关系

文章在对华南地区诸广山、贵东和桃山杂岩体中产铀与非产铀花岗岩的特征进行全面对比的基础上，对其成因进行了探讨。认为产铀与非产铀花岗岩的成因类型不同，前者属Ｓ型花岗岩，后者与Ｉ型花岗岩相似。岩石成因类型不同是造成上述杂岩体中不同地段铀成矿差异的主要原因     

论上饶构造四省交界区域中心战略的载体--板块经济

上饶市委从区域经济的梯度转移出发，把握重大的战略机遇，适时提出了构造四省交界区域中心战略。四省交界区域中心战略要通过恰当的载体——板块经济来承接，实施非均衡又互补性的发展。寻求区域中心及各板块载体的产业集聚、空间资源配置、公共产品供给的路径选择和策略依据，探讨上饶经济圈的形成。