摘要
本文从浮游有孔虫壳体保存,数量,分异度值,底栖类/浮游类比率和CaCO_3含量诸方面讨论马里亚纳海槽区岩芯中溶解及其影响溶解的因素。
The dissolution of planktonic Foraminifera and CaCO_3 and their controlling factors in the cores of the Mariana Trough were discussed based on the preservation and the total number of pianktonic Foraminifera shells, the value of diversity H(S), the benthon/plankton ratio and the CaCO_3 content.
出处
《黄渤海海洋》
CSCD
1993年第2期21-27,共7页
Journal of Oceanography of Huanghai & Bohai Seas
关键词
岩芯
浮游有孔虫
碳酸钙
溶解
Mariana Trough
Cores
Planktonic Foraminifera
CaCO_3
Dissolution Factors