An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite
Coccoliths have dominated the sedimentary archive in the pelagic environment since the Jurassic. The biominerals produced by the coccolithophores are ideally placed to infer sea surface temperatures from their oxygen isotopic composition, as calcification in this photosynthetic algal group only occu...
主要な著者: | Hermoso, M, Minoletti, F, Aloisi, G, Bonifacie, M, McClelland, H, Labourdette, N, Renforth, P, Chaduteau, C, Rickaby, R |
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フォーマット: | Journal article |
出版事項: |
Elsevier
2016
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