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

冲绳海槽D-086孔颗石藻化石及其古海洋学意义的初步探讨
引用本文:苍树溪,钟石兰,薛胜吉.冲绳海槽D-086孔颗石藻化石及其古海洋学意义的初步探讨[J].海洋地质与第四纪地质,1994(3).
作者姓名:苍树溪  钟石兰  薛胜吉
作者单位:中国科学院海洋研究所
基金项目:国家"八五"攻关项目,国家自然科学基金
摘    要:本文通过对冲绳海槽D-086孔颗石藻化石的研究,自下而上划分出三个颗石藻化石组合:Gephyrocapsaaperta-G.oceanica组合,Gephyro-capsaericsonii-Coccolithuscrassipons组合,Emilianiahuxleyi-Gephyrocapsao-ceanica组合;划分出E.huxleyi带和E.huxleyi高峰带的界线;每一个颗石藻化石组合代表一个气候期,它们分别与标准气候期的玉木亚间冰期,晚玉木冰期和冰后期相当。

关 键 词:冲绳海槽,颗石藻化石,古海洋学

THE PRIMARY STUDY ON CALCAREOUS NANNOFOSSILS FOR PALEO-OCEANOGRAPHY IN D-086 CORE OF THE OKINAWA TROUGH
Cang Shuxi Zhong Shilan Xue Shengji.THE PRIMARY STUDY ON CALCAREOUS NANNOFOSSILS FOR PALEO-OCEANOGRAPHY IN D-086 CORE OF THE OKINAWA TROUGH[J].Marine Geology & Quaternary Geology,1994(3).
Authors:Cang Shuxi Zhong Shilan Xue Shengji
Abstract:Calcareous nannofossils for the primary study are taken from D-086 core in the Oki-nawa Trough.There are three assemblages recognized,from bottom to top of the core,i.e.,Cephyrocapsa aperta-G.oceanica;Gephyrocapsa ericsonii-Cocclithus crassipons and E-miliania huxleyi-Gephyrocapsa oceanica. The age of stratigraphy,and the boundary be-tweed E.huxleyi zone and the peak zone of E.huxleyi,were discussed.Each of the threeassemblages represents a climatic period,corresponding to Wurm subinterglacial,the latelast glacial and post glacial(Holocene)respectively.
Keywords:Okinawa Trough calcareous nannofossil paleo-oceanography1)From Nanjing Institute of Geology and Paleontology  Academia Sinica  Nanjing  210008  China    
本文献已被 CNKI 等数据库收录!
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