Ocean Carbon Dioxide Removal and Storage

The ocean, Earth's largest carbon reservoir, exerts a central role over atmospheric CO<sub>2</sub> through its capacity to store carbon primarily as bicarbonate ions. Direct observations indicate that the global ocean has a net carbon uptake of 2.6-3.0 petagrams of carbon annually, representing nearly 30% of anthropogenic CO<sub>2</sub> emissions. This review examines two principal domains of oceanic carbon cycling. The first concerns the natural uptake and storage of anthropogenic CO<sub>2</sub>, with emphasis on the response of the marine carbonate system and the spatial distribution of absorbed carbon. The second addresses emerging marine CO<sub>2</sub> removal strategies, especially ocean alkalinity enhancement and macroalgae-based approaches. Ocean alkalinity enhancement aims to increase seawater buffering capacity to facilitate greater CO<sub>2</sub> uptake, whereas macroalgae-based strategies rely on photosynthetic fixation and the subsequent storage of organic and inorganic carbon in various reservoirs. Effective implementation of these approaches necessitates rigorous monitoring, reporting, and verification frameworks to ensure their quantifiable efficacy and environmental integrity.

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Publication Details

Journal
Chemical Reviews
Published
2026-01-06
DOI
https://doi.org/10.1021/acs.chemrev.5c00433
Citations
3
Primary Topic
Ocean Acidification Effects and Responses
Type
article
Field-Weighted Citation Impact
84.97
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article

Ocean Carbon Dioxide Removal and Storage

J. Kim, Adam V. Subhas, C. Lee, Kitack Lee
3 citations
Chemical Reviews
Ocean Acidification Effects and Responses
84.97
article

Ocean Carbon Dioxide Removal and Storage

J. Kim, Adam V. Subhas, C. Lee, Kitack Lee
article en
3 citations

Abstract

The ocean, Earth's largest carbon reservoir, exerts a central role over atmospheric CO<sub>2</sub> through its capacity to store carbon primarily as bicarbonate ions. Direct observations indicate that the global ocean has a net carbon uptake of 2.6-3.0 petagrams of carbon annually, representing nearly 30% of anthropogenic CO<sub>2</sub> emissions. This review examines two principal domains of oceanic carbon cycling. The first concerns the natural uptake and storage of anthropogenic CO<sub>2</sub>, with emphasis on the response of the marine carbonate system and the spatial distribution of absorbed carbon. The second addresses emerging marine CO<sub>2</sub> removal strategies, especially ocean alkalinity enhancement and macroalgae-based approaches. Ocean alkalinity enhancement aims to increase seawater buffering capacity to facilitate greater CO<sub>2</sub> uptake, whereas macroalgae-based strategies rely on photosynthetic fixation and the subsequent storage of organic and inorganic carbon in various reservoirs. Effective implementation of these approaches necessitates rigorous monitoring, reporting, and verification frameworks to ensure their quantifiable efficacy and environmental integrity.

Chemical ReviewsVol. 126(2)
Kunsan National University (KR), Pohang University of Science and Technology (KR), Aquatic Systems (United States) (US), National Fisheries Institute (US), Woods Hole Oceanographic Institution (US)
Life below water
Openalex Percentile: Top 0%
Ocean Acidification Effects and Responses
84.97
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