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Marine nitrogen fixers mediate a low latitude pathway for atmospheric CO2 drawdown
oleh: Pearse J. Buchanan, Zanna Chase, Richard J. Matear, Steven J. Phipps, Nathaniel L. Bindoff
Format: | Article |
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Diterbitkan: | Nature Portfolio 2019-10-01 |
Deskripsi
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 latitude ocean, made a significant contribution to CO2 drawdown and so amplified the global response to iron fertilisation during ice ages.