Oxygen isotope and paleoclimate in piston core HY4-901 in north part of South China Sea  

作　　者：李学杰 陈芳 唐荣革 方小波 

机构地区：[1]Guangzhou Marine Geological Analysis Center, Ministry of Geology and Mineral Resources, Guangzhou 510760, China [2]Geological Testing-Analysis Research Centre of Guangdong, Guangzhou 510080, China

出　　处：《Chinese Science Bulletin》1996年第20期1722-1725,共4页

摘　　要：The δ¹⁸O value is mainly controlled by δ¹⁸O value of paleo-ocean water and the water skin temperature. The piston core HY4-901 is located at 14°49′N, 113°28′E, on the northern continental slope of the South China Sea, with the water depth of 1 120 m. 1 Sedimentary characteristics The core is characterized by continuous and even-textured sediments, mainly silty clay, with a small amount of clayey silt, bearing abundant planktonic foraminifers, calcareous nannofossils, diatoms and radiolaris.

关 键 词：South China Sea HOLOCENE oxygen isotope paleoclimatology. 

分 类 号：P532[天文地球—古生物学与地层学]