Recurring marine phosphorus spikes during major palaeozoic mass extinctions and climate change
Abstract Mass extinctions in the early Palaeozoic have been attributed to global climate change and ocean anoxia with elevated phosphorus (P) proposed as a key driver. However, this hypothesis has lacked geochemical support due to the absence of proxies that can reconstruct changes in marine P avail...
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| Autores principales: | , , , , , , , , , , , , , , |
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| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
Nature Portfolio
2026-03-01
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| Colección: | Nature Communications |
| Acceso en línea: | https://doi.org/10.1038/s41467-026-70701-y |
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