An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite
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...
| Päätekijät: | , , , , , , , , |
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| Aineistotyyppi: | Journal article |
| Julkaistu: |
Elsevier
2016
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An explanation for the 18O excess in Noelaerhabdaceae coccolith calcite.
Julkaistu 2016
Journal article