Marine nitrogen fixers mediate a low latitude pathway for atmospheric CO2 drawdown
Iron fertilisation of the high latitude oceans is a well-established biological mechanism to explain the ice age drawdown of atmospheric CO2, yet modelling has so far struggled to account for a sufficient drawdown via this mechanism. Here, the authors propose that N2 fixers, which inhabit the lower...
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Autores principales: | Pearse J. Buchanan, Zanna Chase, Richard J. Matear, Steven J. Phipps, Nathaniel L. Bindoff |
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Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2019
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Materias: | |
Acceso en línea: | https://doaj.org/article/c34719e361d34492a0e57907c25fde98 |
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