期刊文献+

冬季南海北部陆架锋区悬浮颗粒态硅的分析 被引量:4

A study on particulate silica in the northern part of the South China Sea in winter
下载PDF
导出
摘要 对冬季南海北部陆架锋区的悬浮颗粒态生物硅(Particulate Biogenic Silica,PBSi)和成岩硅(Lithogenic Silica,LSi)含量进行了调查分析,讨论了悬浮颗粒态生物硅分布及其影响因素。结果表明,南海北部陆架区悬浮颗粒态生物硅和成岩硅平均含量分别为0.59和8.93μmol/dm3。生物硅分布与水团关系密切:在营养盐充足的沿岸水生物硅含量高(1.0μmol/dm3);而在营养盐缺乏的陆架表层水生物硅含量低(0.23μmol/dm3);在两种水团过渡区生物硅含量居中(0.65μmol/dm3)并与溶解硅酸盐(Dissolved Silicate,DSi)成显著正相关(R=0.48,N=44,P=0.001,a=0.01)。此外锋面位置也直接影响生物硅的含量与分布。大部分调查海区被高温高盐低营养盐海水占据,因此导致了调查海区以低浓度的生物硅和成岩硅为特征,且与世界其他海区相比,生物硅含量处于低值区。 The distribution of particulate biogenic silica (PBSi) and lithogenic silica (LSi) were studied in the northern part of South China Sea in winter 2004. The average concentrations of PBSi and LSi were 0.59 and 8.93 μmol/dm^3 , respectively. Due to the intrusion of offshore seawater, the concentrations of PBSi decreased greatly from the coastal water (1.0 μmol/dm^3) to the offshore water (0.23 μmol/dm^3), just like the distribution of dissolved silicate (DSi), which is related to the water mass and shelf front. The concentration of PBSi in the northern part of South China Sea is ranked at the lower end among the world coastal areas.
出处 《海洋学报》 CAS CSCD 北大核心 2009年第5期31-39,共9页
基金 国家自然科学基金与香港研究资助局联合资助项目(40218001 N-HKUST609/32) 科技部国际科技合作交流专项(No.2007DFB20380)资助
关键词 生物硅 成岩硅 分布 陆架锋 南海北部 biogenic silica lithogenic silica distribution shelf front South China Sea
  • 相关文献

参考文献50

  • 1RAGUENEAU O, TREGUER P, LEYNAERT A, et al. A review of the Si cycle in the modern ocean: recent progress and missing gaps in the application of biogenic opal as a paleoproductivity proxy [J] . Global and Planetary Change, 2000, 26(4) : 317--365.
  • 2BUESSELER K O. The decoupling of production and particulate export in the surface ocean[J]. Global Biogeochemistry Cycles, 1998, 12: 297--310.
  • 3LIU S M, YE X W, ZHANG J, et al. The silicon balance in Jiaozhou Bay, North China[J]. Journal of Marine Systems, 2008, 74 (1/2) : 639--648.
  • 4GOLDMAN J G. Spatial and temporal discontinuities of biological processes in pelagic surface waters[M]// Rothschild B J. Toward a Theory of Biological-Physical Interactions in the World Ocean. Dordrecht: Kluwer Academic Publishing, 1988..273--296.
  • 5GOLDMAN J C. Potential role of large oceanic diatoms in new primary production[J]. Deep-Sea Res, 1993, 40: 159--168.
  • 6NELSON D M, TREGUER P, BRZEZINSKI M A, et al. Production and dissolution of biogenic silica in the ocean: revised global estimates, comparison with regional data and relationship to biogenic sedimentation[J]. Global Biogeochemistry Cycles, 1995, 9: 359--372.
  • 7CUSHING D H. A difference in structure between ecosystems in strongly stratified waters and in those that are only weakly stratified [J]. Journal of Plankton Research, 1989, 11(1): 1--13.
  • 8NIXON S W, AMMERMAN J W, Atkinson L, et al. The fate of nitrogen and phosphorus at the land-sea margin of the North Atlantic Ocean[J]. Biogeochemistry, 1996, 35:141--180.
  • 9HOWARTH R W, BILLEN G, SWANEY D, et al. Regional nitrogen budgets and riverine inputs of N & P for the drainages to the North Atlantic Ocean:natural and human influences[J]. Biogeochemistry, 1996, 35: 75--139.
  • 10Conley D J, Schelske C L, Stoermer E F. Modification of the biogeochemical cycle of silica with eutrophication[J]. Marine Ecology Progress Series, 1993, 101.. 179--192.

二级参考文献153

共引文献331

同被引文献144

引证文献4

二级引证文献13

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部