Laboratory-grown coccoliths exhibit no vital effect in clumped isotope (Δ47) composition on a range of geologically relevant temperatures

The carbonate clumped isotope (or Δ47) thermometer relies on the temperature dependence of the abundance of 13C18O16O22− ion groups within the mineral lattice. This proxy shows tremendous promise to reconstruct past sea surface temperatures (SSTs), but requires calibration of the relationship betwee...

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Bibliografiset tiedot
Päätekijät: Katz, A, Bonifacie, M, Hermoso, M, Cartigny, P, Calmels, D
Aineistotyyppi: Journal article
Julkaistu: Elsevier 2017

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