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Ocean deoxygenation after the Sturtian Snowball
Abstract The abrupt ending of the Sturtian ‘Snowball’ glaciation was characterised by enhanced chemical weathering and carbon cycle perturbations, but there is less certainty over how oxygen levels responded to those changes. Here we reconcile conflicting views using a carbonate-based multiproxy dat...
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| Asıl Yazarlar: | , , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Nature Portfolio
2025-07-01
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| Seri Bilgileri: | Nature Communications |
| Online Erişim: | https://doi.org/10.1038/s41467-025-60700-w |
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