2023
DOI: 10.1111/brv.12990
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Carbon sequestration and climate change mitigation using macroalgae: a state of knowledge review

Abstract: The conservation, restoration, and improved management of terrestrial forests significantly contributes to mitigate climate change and its impacts, as well as providing numerous co‐benefits. The pressing need to reduce emissions and increase carbon removal from the atmosphere is now also leading to the development of natural climate solutions in the ocean. Interest in the carbon sequestration potential of underwater macroalgal forests is growing rapidly among policy, conservation, and corporate sectors. Yet, o… Show more

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Cited by 47 publications
(17 citation statements)
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“…Figure 4 highlights the fates of both the parcel of water bearing the CO 2 deficit and seaweed biomass. There is no doubt that on a global scale, seaweeds form long‐term carbon storage pools in ocean sediments on timescales of 100 years or more, although their contribution is extremely small (<1%, 55 Tg C·y −1 ) compared to >99% from oceanic phytoplankton via the biological pump (5–15 Pg C·y −1 ; Boyd et al., 2019; Filbee‐Dexter et al., in revision; Pessarrodona et al., 2023). For any seaweed system (natural seaweed bed, nearshore or open ocean aquaculture) under consideration for carbon credits/offsets, two steps are required for MRV (Figure 4): (1) The parcel of seawater that bears the CO 2 deficit resulting from seaweed photosynthesis must be tracked over long timescales (weeks to months to over a year) to quantify the amount of atmospheric CO 2 that enters seawater, and (2) the amount of the organic carbon from the same seaweed system that enters long‐term storage (>100 years; as POC, DOC) must be quantified.…”
Section: Discussionmentioning
confidence: 99%
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“…Figure 4 highlights the fates of both the parcel of water bearing the CO 2 deficit and seaweed biomass. There is no doubt that on a global scale, seaweeds form long‐term carbon storage pools in ocean sediments on timescales of 100 years or more, although their contribution is extremely small (<1%, 55 Tg C·y −1 ) compared to >99% from oceanic phytoplankton via the biological pump (5–15 Pg C·y −1 ; Boyd et al., 2019; Filbee‐Dexter et al., in revision; Pessarrodona et al., 2023). For any seaweed system (natural seaweed bed, nearshore or open ocean aquaculture) under consideration for carbon credits/offsets, two steps are required for MRV (Figure 4): (1) The parcel of seawater that bears the CO 2 deficit resulting from seaweed photosynthesis must be tracked over long timescales (weeks to months to over a year) to quantify the amount of atmospheric CO 2 that enters seawater, and (2) the amount of the organic carbon from the same seaweed system that enters long‐term storage (>100 years; as POC, DOC) must be quantified.…”
Section: Discussionmentioning
confidence: 99%
“…For example, the photochemical breakdown of DOC will likely increase in the optically brighter open oceans compared to turbid coastal waters (Wada et al., 2015). The contribution of seaweed carbon to the DOC pool is unknown, and we have little understanding of its transit time and fate offshore (Paine et al., 2021; Pessarrodona et al., 2023).…”
Section: Seaweed Carbon Storage Poolsmentioning
confidence: 99%
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“…Kelp forests are also recognized as critical ecological habitats that provide several direct and indirect ecosystem services (Smale et al ., 2013; Vásquez et al ., 2014; Filbee-Dexter and Wernberg, 2020). These globally significant, highly productive ecosystems are however under threat from climate change, habitat destruction, and over-fishing (Harley et al ., 2012; Spalding et al ., 2019; Wernberg et al ., 2019a; Buglass et al ., 2022; Coleman et al ., 2022; Pessarrodona et al ., 2023), and require ongoing research to better understand and communicate their socio-ecological value, and to improve their conservation and management.…”
Section: Introductionmentioning
confidence: 99%