2023
DOI: 10.1038/s43247-023-00833-2
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Large global variations in the carbon dioxide removal potential of seaweed farming due to biophysical constraints

Abstract: Estimates suggest that over 4 gigatons per year of carbon dioxide (Gt-CO2 year−1) be removed from the atmosphere by 2050 to meet international climate goals. One strategy for carbon dioxide removal is seaweed farming; however its global potential remains highly uncertain. Here, we apply a dynamic seaweed growth model that includes growth-limiting mechanisms, such as nitrate supply, to estimate the global potential yield of four types of seaweed. We estimate that harvesting 1 Gt year−1 of seaweed carbon would r… Show more

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Cited by 12 publications
(12 citation statements)
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References 99 publications
(141 reference statements)
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“…Additionally, other unaccounted environmental variables could represent confounding factors. Nevertheless, adverse climatic changes and anthropogenic activities are predicted to elevate the duration and intensity of seawater light penetration through mechanisms like increased stratification, thermocline shoaling and by influencing primary productivity. , The former two are especially concerning for the development of seaweed aquaculture in offshore waters, where nutrient availability is typically lower. While excessive light may induce stress and impair photosynthesis in kelp, kelp typically adapts to fluctuating light levels, rendering such negative impacts transient, after which kelp may resume normal functioning .…”
Section: Discussionmentioning
confidence: 99%
“…Additionally, other unaccounted environmental variables could represent confounding factors. Nevertheless, adverse climatic changes and anthropogenic activities are predicted to elevate the duration and intensity of seawater light penetration through mechanisms like increased stratification, thermocline shoaling and by influencing primary productivity. , The former two are especially concerning for the development of seaweed aquaculture in offshore waters, where nutrient availability is typically lower. While excessive light may induce stress and impair photosynthesis in kelp, kelp typically adapts to fluctuating light levels, rendering such negative impacts transient, after which kelp may resume normal functioning .…”
Section: Discussionmentioning
confidence: 99%
“…alkalinity enhancement and ocean fertilization; thousands to tens of thousands of Tg C year −1 ; NASEM, 2021), but compares favourably to other blue carbon ecosystems (Krause-Jensen & Duarte, 2016). Unlike other coastal vegetated habitats, the area occupied by macroalgae forests can be extensively increased by the expansion of coastal and open ocean farms (Arzeno-Soltero et al, 2023). Some of the carbon assimilated into biomass during the farming process can be lost before harvesting and buried under the farm soils under the right sedimentary conditions, potentially remaining stored long-term (Pan et al, 2021).…”
Section: Main Macroalgal Carbon Sequestration Pathwaysmentioning
confidence: 99%
“…We focus on wild macroalgal ecosystems and intentionally refrain from contextualising these topics in relation to macroalgae farming. This focus arises because interventions around wild ecosystems presently have substantially higher potential abatement (NASEM, 2021), present more co-benefits (Forbes et al, 2022), and the CO 2removal capacity of macroalgae farming has been explored elsewhere (Arzeno-Soltero et al, 2023;Ross et al, 2022;Wu, Keller & Oschlies, 2023). Specifically, our review is largely centered on macroalgal forests formed by large brown algae (sensu Wernberg & Filbee-Dexter, 2019), which draw the greatest atmospheric CO 2 flux of any macroalgae habitat (Duarte et al, 2022;Pessarrodona et al, 2022) and whose contribution to sequestration is presumably the largest (Krause-Jensen & .…”
Section: Introductionmentioning
confidence: 99%
“…In addition to the natural fluxes of seaweed carbon beyond the continental shelf, there is considerable interest in enhancing these processes by growing seaweeds on artificial structures in the open ocean, termed “ocean (macroalgal) afforestation,” and sinking resulting biomass to the deep ocean (Figure 1b; Arzeno‐Soltero et al., 2023; Ocean Visions and Monterey Bay Aquarium Research Institute, 2022; Ross et al., 2023; Figures S1, S4, S5, S7). As seaweeds sink, a range of processes (as above) will affect their degradation and the amount of biomass that reaches the deep ocean floor (Figure 1b).…”
Section: Seaweed Carbon Storage Poolsmentioning
confidence: 99%
“…;Arzeno- Soltero et al, 2023; Ocean Visions and Monterey Bay Aquarium Research Institute, 2022;Ross et al, 2023; Figures …”
mentioning
confidence: 99%