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...

Полное описание

Библиографические подробности
Главные авторы: Hermoso, M, Minoletti, F, Aloisi, G, Bonifacie, M, McClelland, H, Labourdette, N, Renforth, P, Chaduteau, C, Rickaby, R
Формат: Journal article
Опубликовано: Elsevier 2016

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