闽南长泰地区景观格局特征及其影响因素分析

利用景观学的研究方法，以GIS技术为支撑，分析了闽南长泰地区耕地、林地(包括果因)、草地、水域、城镇工矿居民用地、未利用土地等景观格局特征，研究了景观多样性优势度、均匀度、破碎化指数、分离度、分维数等景观指数，显示出该区域多样性程度不高，景观类型以林地、耕地、草地单元为主，整体优势度较大，均匀度较低及“南耕北林”的空间景观格局特征，并指出了影响景观格局特征的主要因素是地形地貌特征和人类生产活动。     

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.     

Quaternary high-resolution opal record and its paleoproductivity implication at ODP Site 1143,southern South China Sea

The correlation of opal content and MAR with oxygen isotopic records of benthonic foraminifera at Site 1143, southern South China Sea indicates that,since about 900 ka,the increasing opal content and MAR during the interglacial periods is inferred to reflect the bigher surface productivity ,for the intensified summer monsoon during the interglacial periods would result in the enhanced upwelling and nutrient supply,Time-sequence spectral analyses of oxygen isotopic record ,opal content and MAR at intervals of 0-900 ka reveal that the changes of surface productivity were dominantly forced by the variations of the earth orbital cycles.     

Early Cambrian eodiscoid trilobites of the Yangtze Platform and their stratigraphic implications

Analysis of the taxonomy and stratigraphic distribution of the Early Cambrian eodiscoid trilobites of the Yangtze Platform indicates that species of Tsunyidiscus and Hupeidiscus can be used for biostratigraphic correlation. T. aclis occurs only in the lower Qiongzhusian, T. armatus occurs in the lower and middle Qiongzhusian, while T. niutitangensis and T. tingi occur mainly in the middle and upper Qiongzhusian, with only T. tingi extending upward into the lower Canglangpuian. H. orientalis first appears in the upper Qiongzhusian, reaching peak abundance in the lower Canglangpuian and becoming extinct above the Drepanuroides Zone. Biostratigraphic and lithostratigraphic correlations indicate that the limestone in the lower part of the Mingxinsi Formation, the Upper Member of Jiumenchong Formation, and the upper part of the Middle Member of the Huangbailing Formation, can be correlated with each other as Hupediscus, an index fossil of the lower Canglangpuian, is abundant in all these units. The lower part of the Niutitang and Jiumenchong formations in eastern Guizhou, which mainly represent Qiongzhusian strata, can be correlated with the Lower Member of the Huangbailing Formation. The basal part of the Niutitang Formation, which may be equivalent to the Upper Meishucunian Shiyantou Formation in eastern Yunnan, is very condensed. Well-preserved sponge faunas and non-mineralized fossils in the lower part of the Niutitang and Hetang formations are not older than Qiongzhusian in age.     

Evolution of the South China Sea and monsoon history revealed in deep-sea records

As the third summary report of ODP Leg 184 to the South China Sea (SCS), this paper discusses the evolution of the East Asian monsoon and the SCS basin. A multi-proxy approach, involving geochemistry, micropale-ontology, pollen and other analyses, was adopted for reconstructing the evolutionary history of the East Asian monsoon, which was characterized by a series of paleo-climate events especially at 8, 3.2, 2.2 and 0.4 Ma. The new record indicates similar stages in the development of the East and South Asian monsoons, with an enhanced winter monsoon over East Asia being the major difference. The rich spectrums of monsoon variability from the southern SCS also reveal other characteristic features of the low latitude ocean. Evidence for the evolution of the SCS includes the hemipelagic Oligocene sediments, implying the existence of deep water environments during the early seafloor spreading stage of the SCS basin. The four major unconformities and some remarkabl ediagenetic features in upper Oligocene deposits indicate the strongest tectonic events in the region. From a careful comparison of lithologies and sedimentation rates, we conclude that the prominent differences in sedimentary environments between the southern and northern SCS were established only by ～3 Ma.     

南海海底特征、资源区位与疆界断续线

根据南海海底的成因与地形特征 ,并通过建立和分析南海海底数字地形模型 ,将南海的海底分为中央的深海盆地、两侧的阶梯状大陆坡、以及周边亚洲大陆延伸的大陆架 3个地貌单元 .再据 194 7年“南海诸岛位置图”精确计算出二战后依据波茨坦公告为国际认可的断续线疆界的经纬度坐标 ,阐述了中国对南海主权的历史延续性 .最后 ,论述了南海区位与资源的优势 ,论证了其海域具体位置与巨大的经济政治战略意义 .     

瀑河水库加固扩建工程的环境影响及其对策

对南水北调中线的一个调蓄水库－－瀑河水库环境质量现状进行评价，利用实验室模拟和WQRRS模型预测蓄水后不同情景下的水库水质状况，分析水库对生态环境、水文泥沙、环境地质等影响，从环境角度论证水库建设项目的可行性。提出了环境改善和保护的对策和建议，为南水北调中线工程的决策提供依据。     

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     

生态空间·人本生活———华南师范大学校园环境景观的初步评价

从生态学的角度,人本思想为理念,从空间和形态上,通过建筑、水体、植被、道路和景观小品等方面,对华南师范大学校园环境景观进行了初步的评价.探索如何营造一个人文环境和自然环境和谐共存、整体完善的高校校园生态环境系统.