Mn/Ca ratio in planktonic foraminifer from ODP Site 1144, the northern South China Sea : A possible paleoclimate indicator
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概要
- 論文の詳細を見る
- 2009-08-01
著者
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LIU Ying
Key Laboratory of Modern Chinese Medicines (China Pharmaceutical University), Ministry of Education
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Wei Gang-jian
Key Laboratory Of Isotope Geochronology And Geochemistry Guangzhou Institute Of Geochemistry Chinese
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Chen Jian-fang
The Second Institute Of Oceanography Soa
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Li Xian-hua
Key Laboratory Of Isotope Geochronology And Geochemistry Guangzhou Institute Of Geochemistry Chinese
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Liu Ying
Key Laboratory Of Isotope Geochronology And Geochemistry Guangzhou Institute Of Geochemistry Chinese
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ZOU LIANG
Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chine
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DENG WEN-FENG
Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chine
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Zou Liang
Key Laboratory Of Isotope Geochronology And Geochemistry Guangzhou Institute Of Geochemistry Chinese
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Deng Wen-feng
Key Laboratory Of Isotope Geochronology And Geochemistry Guangzhou Institute Of Geochemistry Chinese
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Liu Ying
Key Lab. Of Modern Chinese Medicines (china Pharmaceutical University) Ministry Of Education
関連論文
- Mn/Ca ratio in planktonic foraminifer from ODP Site 1144, the northern South China Sea : A possible paleoclimate indicator
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