An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite

An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite

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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...

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Détails bibliographiques
Auteurs principaux:	Hermoso, M, Minoletti, F, Aloisi, G, Bonifacie, M, McClelland, H, Labourdette, N, Renforth, P, Chaduteau, C, Rickaby, R
Format:	Journal article
Publié:	Elsevier 2016

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