1433 / 2024-09-27 09:44:32
A largely overlooked mechanism for marine carbon storage
Biological carbon pump,ocean carbon cycle,preferential remineralization,inverse model
Abstract Accepted
Lyu Yan / State Key Lab of Marine Environmental Science and College of Ocean and Earth Sciences, Xiamen University
Wei-Lei Wang / State Key Lab of Marine Environmental Science and College of Ocean and Earth Sciences, Xiamen University
The ocean acts as a significant sink for atmospheric carbon dioxide (CO2), regulating global climate. The biological carbon pump (BCP) transfers organic carbon, fixed in the euphotic zone via phytoplankton photosynthesis, to the deep ocean. This mechanism is believed to have played a crucial role in regulating atmospheric CO2 during the glacial-interglacial transitions. However, paleo-records show that the export production preserved in the sediment is not high enough to explain the tens of ppm CO2 drawdown. On the other hand, field observations have shown that the ratio of dissolved organic carbon (DOC) to dissolved organic phosphorus (DOP) and the ratio of dissolved organic nitrogen (DON) to DOP increase with depth, suggesting a preferential remineralization of organic phosphorus, compared to nitrogen and carbon, and also suggesting a rapid recycling of phosphorus in the surface ocean. Consequently, preferential remineralization of organic phosphorus alleviates phosphorus limitation and enhance carbon sequestration, offering another explanation for the glacial-interglacial atmospheric CO2 oscillations. Our model results show that CO2 concentration can be drawn down by 121.35 ppm when both DOP and particulate organic phosphorus (POP) are allowed to be preferentially remineralized compared to DON/DOC and PON/POC.
Important Date
  • Conference Date

    Jan 13

    2025

    to

    Jan 17

    2025

  • Sep 27 2024

    Draft paper submission deadline

  • Feb 17 2025

    Registration deadline

Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University
Organized By
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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