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Unraveling the Unseen Players in the Ocean - A Field Guide to Water Chemistry and Marine Microbiology
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イソトープによる証拠は,ケノゾーイク期における海洋カルシウム循環の変動を示しています

C L De La Rocha1, D J DePaolo

  • 1Berkeley Center for Isotope Geochemistry, Department of Geology and Geophysics, University of California, Berkeley, CA 94720-4767, USA.

Science (New York, N.Y.)
|August 19, 2000
PubMed
まとめ

8千万年にわたる海洋カルシウムイソトープの変動は,気候変動を明らかにしています. 海洋カルシウムのこれらの変化は,気象と沈殿のバランスを反映し,大気中の二酸化炭素と地球温暖化に影響を与えます.

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