首页 | 本学科首页   官方微博 | 高级检索  
     检索      

白令海表层沉积物中硅质生物的变化及其环境控制因素
引用本文:王汝建,陈荣华.白令海表层沉积物中硅质生物的变化及其环境控制因素[J].地球科学,2004,29(6):685-690.
作者姓名:王汝建  陈荣华
作者单位:1.同济大学教育部海洋地质重点实验室, 上海 200092
基金项目:国家重点基础研究发展规划项目 (G2 0 0 0 785 0 0 ),国家自然科学基金项目 (Nos.40 3 2 160 3,40 2 760 2 0,40 1760 15 ),高等学校全国优秀博士学位论文作者专项资助 (No .2 0 0 12 6),高等学校骨干教师资助计划
摘    要:中国首次北极科学考察在白令海采取了12个表层沉积物样品, 其中对硅质生物和陆源碎屑的详细研究发现, 它们主要由硅藻、放射虫和海绵骨针组成.其中, 硅藻在样品中的丰度均占绝对优势, 高出放射虫和海绵骨针一个数量级.它们与环境控制因素关系的分析表明, 硅藻、放射虫和海绵骨针丰度的高低及其保存程度与深度、温度、盐度和受大规模季节性气候变化控制的表层海水的高营养和高生产力, 以及陆源物质输入的变化密切相关.这一研究结果对白令海第四纪的古气候与古海洋学研究具有十分重要的意义. 

关 键 词:表层沉积物    硅质生物丰度    环境控制因素    白令海
文章编号:1000-2383(2004)06-0685-06
收稿时间:2004-04-09

Variations of Siliceous Microorganisms in Surface Sediments of the Bering Sea and Their Environmental Control Factors
WANG Ru-jian,CHEN Rong-hua .Laboratory of Marine Geology of MOE,Tongji University,Shanghai,China .Key Laboratory of Submarine Geoscience,State Oceanic Administration,Hangzhou,China.Variations of Siliceous Microorganisms in Surface Sediments of the Bering Sea and Their Environmental Control Factors[J].Earth Science-Journal of China University of Geosciences,2004,29(6):685-690.
Authors:WANG Ru-jian  CHEN Rong-hua Laboratory of Marine Geology of MOE  Tongji University  Shanghai  China Key Laboratory of Submarine Geoscience  State Oceanic Administration  Hangzhou  China
Institution:WANG Ru-jian~1,CHEN Rong-hua~2 1.Laboratory of Marine Geology of MOE,Tongji University,Shanghai200092,China 2.Key Laboratory of Submarine Geoscience,State Oceanic Administration,Hangzhou310012,China
Abstract:Based on the quantitative studies of siliceous microorganisms and terrestrial detritus in 12 surface sediment samples, which were recovered by the First Chinese National Arctic Expedition team, in the Bering Sea, it goes without saying that diatom abundance is dominant within the microorganisms which consists of diatoms, radiolarians and sponge spicules. The relationship between the microorganisms and environmental control factors, for example, water depth, temperature and salinity are analyzed and discussed. It is evident that their abundance change and preservation are associated closely with these environmental control factors, and high surface nutrient and productivity controlled by the variations of large scale seasonal climate and input of terrestrial detritus. This investigation is very significant for the further studies on paleoclimate and paleoceanography in the Bering Sea.
Keywords:surface sediments  siliceous microorganism abundance  environmental control factor  the Bering Sea  
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《地球科学》浏览原始摘要信息
点击此处可从《地球科学》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号