A 600 kyr reconstruction of deep Arctic seawater <i>δ</i><sup>18</sup>O from benthic foraminiferal <i>δ</i><sup>18</sup>O and ostracode Mg ∕ Ca paleothermometry
<p>The oxygen isotopic composition of benthic foraminiferal tests (<span class="inline-formula"><i>δ</i><sup>18</sup>O</span><span class="inline-formula"><sub>b</sub></span>) is one of the pre-eminent tools for correlating marine sediments and interpreting past terrestrial ice volume and deep-ocean...
Gorde:
| Egile Nagusiak: | , , , , , , , |
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Copernicus Publications
2023-03-01
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| Saila: | Climate of the Past |
| Sarrera elektronikoa: | https://cp.copernicus.org/articles/19/555/2023/cp-19-555-2023.pdf |
| Etiketak: |
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