An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite

An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite

Εμφάνιση άλλων εκδόσεων (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...

Πλήρης περιγραφή

Λεπτομέρειες βιβλιογραφικής εγγραφής
Κύριοι συγγραφείς:	Hermoso, M, Minoletti, F, Aloisi, G, Bonifacie, M, McClelland, H, Labourdette, N, Renforth, P, Chaduteau, C, Rickaby, R
Μορφή:	Journal article
Έκδοση:	Elsevier 2016

Παρόμοια τεκμήρια

An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite.
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Coccolith chemistry considered
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Carbon Isotope Fractionation in Noelaerhabdaceae Algae in Culture and a Critical Evaluation of the Alkenone Paleobarometer
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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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Έκδοση: (2024-03-01)

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