An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite

Geochimica et Cosmochimica Acta

Volumn 189, Issue , 2016, Pages 132-142

  Hermoso, M ^a   Minoletti, F ^b,c   Aloisi, G ^b,d   Bonifacie, M ^e   McClelland, H L O ^a,g   Labourdette, N ^b,c   Renforth, P ^f   Chaduteau, C ^e   Rickaby, R E M ^a  

^a UNIVERSITY OF OXFORD   (United Kingdom)

^b SORBONNE UNIVERSITÉ   (France)

^c Sorbonne Universités   (France)

^d UNIVERSITÉ PIERRE ET MARIE CURIE   (France)

^e INSTITUT DE PHYSIQUE DU GLOBE DE PARIS   (France)

^f CARDIFF UNIVERSITY   (United Kingdom)

^g WASHINGTON UNIVERSITY   (United States)

Author keywords

Biomineralisation; Carbon (CO2) limitation; Emiliania huxleyi; Gephyrocapsa oceanica; Oxygen isotope fractionation; Temperature proxy; Vital effect

Indexed keywords

BIOMINERALIZATION; CALCITE; CARBON DIOXIDE; COCCOLITH; ISOTOPIC COMPOSITION; ISOTOPIC FRACTIONATION; JURASSIC; OXYGEN ISOTOPE; PELAGIC ENVIRONMENT; TEMPERATURE PROFILE;

ALGAE; EMILIANIA HUXLEYI; GEPHYROCAPSA OCEANICA; HAPTOPHYCEAE; NOELAERHABDACEAE;

EID: 84975221231     PISSN: 00167037     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.gca.2016.06.016     Document Type: Article

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