OXYGEN ISOTOPIC RECORD AND ITS PALEOCLIMATIC IMPLICATIONS OF BENTHONIC FORAMINIFERA OF EAST CHINA SEA CORE SHIM-I IN MID-EOCENE,PLIOCENE AND EARLY-PLEISTOCENE  

作　　者：王大锐 王乃文 S.G.WHITTAKER 

机构地区：[1]Scientific Research Institute of Petroleum Exploration & Development, Beijing 100083, PRC [2]Institute of Geological Sciences, Chinese Academy of Geological Sciences, Beijing 100037, PRC [3]Department of Geological Sciences, University of Saskatchewan, Canada S7N, OWO

出　　处：《Chinese Science Bulletin》1990年第24期2076-2080,共5页

摘　　要：Oxyegen and carbon isotopic ratios in the Quatermary-Pliocene,Pleistocene and Eocene Benthonic foraminiferahave been investigated from a single core drilled inthe East

关 键 词：FORAMINIFERA stable isotope paleotemperature. 

分 类 号：N[自然科学总论]