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The benthic foraminiferal δ(34)S records flux and timing of paleo methane emissions
In modern environments, pore water geochemistry and modelling simulations allow the study of methane (CH(4)) sources and sinks at any geographic location. However, reconstructing CH(4) dynamics in geological records is challenging. Here, we show that the benthic foraminiferal δ(34)S can be used to r...
Tallennettuna:
| Julkaisussa: | Sci Rep |
|---|---|
| Päätekijät: | , , , , |
| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
Nature Publishing Group UK
2020
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| Aiheet: | |
| Linkit: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6987089/ https://ncbi.nlm.nih.gov/pubmed/31992778 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-020-58353-4 |
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