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
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2019
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Acceso en línea:https://doaj.org/article/c34719e361d34492a0e57907c25fde98
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