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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Bibliografiske detaljer
Main Authors:	Hermoso, M, Minoletti, F, Aloisi, G, Bonifacie, M, McClelland, H, Labourdette, N, Renforth, P, Chaduteau, C, Rickaby, R
Format:	Journal article
Udgivet:	Elsevier 2016

Lignende værker

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Coccolith chemistry considered
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Publisher Correction: Coccolith-calcite Sr/Ca as a proxy for transient export production related to Saharan dust deposition in the tropical North Atlantic
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