An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite

An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite

Taispeáin leaganacha eile (1)

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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Príomhchruthaitheoirí:	Hermoso, M, Minoletti, F, Aloisi, G, Bonifacie, M, McClelland, H, Labourdette, N, Renforth, P, Chaduteau, C, Rickaby, R
Formáid:	Journal article
Foilsithe / Cruthaithe:	Elsevier 2016

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