Mid Pleistocene foraminiferal mass extinction coupled with phytoplankton evolution
The cause of a 20% decline in sea floor calcareous foraminifera species during the Mid-Pleistocene remains enigmatic. Here, the authors present new geochemical evidence, from the Tasman Sea that supports a change in phytoplankton food source as the primary driver.
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| Autores principales: | , , , , , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2016
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/62aa4e816d244bdf8307d5786f04724a |
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