收稿日期: 2002-07-02
修回日期: 2002-10-24
网络出版日期: 2003-06-01
基金资助
国家重点基础研究发展规划项目“东、黄海生态动力学与生物资源可持续利用”(编号:G1999043705);“我国近海有害赤潮发生的生态学、海洋学机制及预测防治”(编号:2001CB409703);国家自然科学基金重点项目“胶州湾流域生源要素流失与海湾富营养化演变过程”(编号:40036010)资助.
THE DETERMINATION OF BIOGENIC SILICA AND ITS BIOGEOCHEMISTRY SIGNIFICANCE
Received date: 2002-07-02
Revised date: 2002-10-24
Online published: 2003-06-01
叶曦雯 , 刘素美 , 张经 . 生物硅的测定及其生物地球化学意义[J]. 地球科学进展, 2003 , 18(3) : 420 -426 . DOI: 10.11867/j.issn.1001-8166.2003.03.0420
Biogenic silica(BSi) is a chemical determination of the amount of amorphous. BSi is also known as biogenic opal or simple opal by geologists. Recent compilation of percent biogenic silica in surface sediments have revealed a close link to biosiliceous productivity patterns in the overlying surface waters. Amorphous silica can be comprised of different components mainly of biological origin such as diatoms phytoliths, radiolarians, silicoflagellates and sponge spicules. The opal content of marine sediments carries a valuable paleoceanographic record of changes in the strengths and locations of surface ocean productivity. Measuring the silicon isotopic composition of diatoms can provide a record of environmental change. The BSi sedimentary record also has been used to study climate change. The sedimentary BSi record is a sensitive indicator of anthropogenic nutrient enrichment because it integrates seasonal uptake of dissolved silicate utilized in diatom production. In this paper,the author discussed some questions in the measurement of BSi in marine sediments and particulates. The importance of determination of biogenic silica in biogeochemical research is also analyzed.
Key words: Biogenic silica; Sediments; Clay; Analytical methods.
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