No detectable influence of the carbonate ion effect on changes in stable carbon isotope ratios (<i>δ</i><sup>13</sup>C) of shallow dwelling planktic foraminifera over the past 160 kyr
<p>Laboratory experiments showed that the isotopic fractionation of <span class="inline-formula"><i>δ</i><sup>13</sup></span>C and of <span class="inline-formula"><i>δ</i><sup>18</sup></span>O during calcite formation of planktic foraminifera are species-specific functions of ambient CO<span class=...
Guardat en:
| Autors principals: | , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Copernicus Publications
2024-04-01
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| Col·lecció: | Climate of the Past |
| Accés en línia: | https://cp.copernicus.org/articles/20/991/2024/cp-20-991-2024.pdf |
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