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  5. Evolution of planktonic foraminifera and thermocline in the southern South China Sea since 12 Ma (OD

Evolution of planktonic foraminifera and thermocline in the southern South China Sea since 12 Ma (OD

来源 :中国科学：地球科学英文版 | 被引量 : 0次 | 上传用户：yilong_hongru
【摘 要】
：
Down-core variation in planktonic foraminifera (PF) at Site 1143 (ODP 184) has dis closed the evolution of upper water-column structure over the last 12 Ma in t
【作 者】
：
Ll Baohua 
【机 构】
：
1.NanjingInstituteofGeologyandPaleontology,2.KeyLaboratoryofMarineGeology
【出 处】
：
中国科学：地球科学英文版
【发表日期】
：
2001年10期
【关键词】
：
南部的华南海 迟了的晚第三纪 planktonic 有孔虫类 THERMOCLINE 向西和平的温暖的水池 southern South China Sea L 
【基金项目】
：
国家科学基金
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Down-core variation in planktonic foraminifera (PF) at Site 1143 (ODP 184) has dis closed the evolution of upper water-column structure over the last 12 Ma in the southern South China Sea. In the early Late Miocene (～10.6-7.8 Ma), there existed a lower p
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