Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth
<p>The translation of the original seawater signal (i.e. ambient temperature and <span class="inline-formula"><i>δ</i><sup>18</sup>O<sub>sw</sub></span>) into distinct chambers of a single shell of a foraminifer during calcification can...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2019-02-01
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| Series: | Biogeosciences |
| Online Access: | https://www.biogeosciences.net/16/643/2019/bg-16-643-2019.pdf |