Fossil biocalcite remains open to isotopic exchange with seawater for tens of millions of years
Abstract Fossilized remains of marine calcifiers constitute the physical basis for reconstructions of both deep ocean and sea-surface temperatures going back millions of years, but paleoclimate records derived from their isotope and trace-element chemistry can be biased by diagenesis. Experiments si...
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| Hoofdauteurs: | , , , , , , , , , , , , , |
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| Formaat: | Artigo |
| Taal: | Inglês |
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Nature Portfolio
2024-10-01
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| Reeks: | Scientific Reports |
| Online toegang: | https://doi.org/10.1038/s41598-024-75588-7 |
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