Carbon export from seaweed forests to deep ocean sinks

IF 15.7 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Nature Geoscience Pub Date : 2024-05-22 DOI:10.1038/s41561-024-01449-7
Karen Filbee-Dexter, Albert Pessarrodona, Morten F. Pedersen, Thomas Wernberg, Carlos M. Duarte, Jorge Assis, Trine Bekkby, Michael T. Burrows, Daniel F. Carlson, Jean-Pierre Gattuso, Hege Gundersen, Kasper Hancke, Kira A. Krumhansl, Tomohiro Kuwae, Jack J. Middelburg, Pippa J. Moore, Ana M. Queirós, Dan A. Smale, Isabel Sousa-Pinto, Nobuhiro Suzuki, Dorte Krause-Jensen
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Abstract

The coastal ocean represents an important global carbon sink and is a focus for interventions to mitigate climate change and meet the Paris Agreement targets while supporting biodiversity and other ecosystem functions. However, the fate of the flux of carbon exported from seaweed forests—the world’s largest coastal vegetated ecosystem—is a key unknown in marine carbon budgets. Here we provide national and global estimates for seaweed-derived particulate carbon export below 200 m depth, which totalled 3–4% of the ocean carbon sink capacity. We characterized export using models of seaweed forest extent, production and decomposition, as well as shelf–open ocean water exchange. On average, 15% of seaweed production is estimated to be exported across the continental shelf, which equates to 56 TgC yr−1 (range: 10–170 TgC yr−1). Using modelled sequestration timescales below 200 m depth, we estimated that each year, 4–44 Tg seaweed-derived carbon could be sequestered for 100 years. Determining the full extent of seaweed carbon sequestration remains challenging, but critical to guide efforts to conserve seaweed forests, which are in decline globally. Our estimate does not include shelf burial and dissolved and refractory carbon pathways; still it highlights a relevant potential contribution of seaweed to natural carbon sinks. Coastal seaweed transported to the open ocean contributes up to 3–4% of the particulate organic carbon sinking into the deeper ocean, according to combined ecological and biogeochemical modelling.

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海藻林向深海碳汇输出碳
近海是全球重要的碳汇,也是减缓气候变化和实现《巴黎协定》目标的干预重点,同时还支持生物多样性和其他生态系统功能。然而,从海藻森林--世界上最大的沿海植被生态系统--输出的碳通量的去向是海洋碳预算中的一个关键未知数。在这里,我们提供了全国和全球 200 米深度以下海藻衍生颗粒碳输出的估计值,其总量占海洋碳汇容量的 3-4%。我们使用海藻林范围、生产和分解模型以及陆架-开阔洋水交换模型来描述碳输出的特征。据估计,平均有 15%的海藻产量被输出到大陆架上,相当于每年输出 56 TgC(范围:10-170 TgC/yr-1)。利用 200 米深度以下的模拟固碳时间尺度,我们估计每年有 4-44 兆吨海藻产生的碳可固存 100 年。确定海藻碳固存的全部范围仍然具有挑战性,但对于指导保护海藻森林的工作至关重要,因为全球海藻森林正在减少。我们的估算并不包括陆架埋藏以及溶解碳和难溶碳途径;但它强调了海藻对自然碳汇的潜在贡献。
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来源期刊
Nature Geoscience
Nature Geoscience 地学-地球科学综合
CiteScore
26.70
自引率
1.60%
发文量
187
审稿时长
3.3 months
期刊介绍: Nature Geoscience is a monthly interdisciplinary journal that gathers top-tier research spanning Earth Sciences and related fields. The journal covers all geoscience disciplines, including fieldwork, modeling, and theoretical studies. Topics include atmospheric science, biogeochemistry, climate science, geobiology, geochemistry, geoinformatics, remote sensing, geology, geomagnetism, paleomagnetism, geomorphology, geophysics, glaciology, hydrology, limnology, mineralogy, oceanography, paleontology, paleoclimatology, paleoceanography, petrology, planetary science, seismology, space physics, tectonics, and volcanology. Nature Geoscience upholds its commitment to publishing significant, high-quality Earth Sciences research through fair, rapid, and rigorous peer review, overseen by a team of full-time professional editors.
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