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...
| المؤلفون الرئيسيون: | , , , , , , , , |
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| التنسيق: | Journal article |
| منشور في: |
Elsevier
2016
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