Recovery timeframe is a critical component in preserving carbon stocks in disturbed tropical seagrass meadows

IF 4.9 3区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES
Marine pollution bulletin Pub Date : 2026-05-01 Epub Date: 2026-01-26 DOI:10.1016/j.marpolbul.2026.119296
Taylor Renee Condron , Timothy M. Smith , Paul H. York , Nicholas J. Murray , Pere Masque , Michael A. Rasheed
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Abstract

Seagrass meadows, though covering a small percentage of the ocean floor, play a critical role in marine carbon sequestration. However, the mechanisms behind this role remain uncertain due to challenges in mapping seagrass extent and flux, accounting for spatial variation in carbon storage, and incorporating site-specific histories. This study investigates the effects of short-term (≤10 years) seagrass loss on sediment carbon stocks within a large seagrass meadow in the Great Barrier Reef region. Using remote sensing data to construct a seagrass recovery timeline, combined with field sampling and assessments of ecological factors, we found higher sediment organic carbon in areas where seagrass coverage was retained throughout the study period. Carbon stock and sediment accumulation varied with Recovery stage and were influenced by ecological factors and the length of seagrass absence. Minimal differences in sedimentary carbon stocks were observed between retained areas and those recovering within 3–8 years, suggesting limited disturbance impacts on carbon storage when recovery occurs within this timeframe. However, significant differences in carbon stocks were observed between persistent meadow areas and sites where no seagrass recovery had occurred for ≥10 years. The study meadow contained an estimated 39,779 Mg C (to 1 m), with spatial variation linked to seagrass loss and recovery history, as well as ecological and environmental factors. Our findings offer context to the permanence of seagrass Blue Carbon during meadow loss and suggest sedimentary carbon stocks can largely persist in similar systems experiencing cycles of seagrass loss and recovery that occur over 3-to-8-year timeframes.
恢复时间框架是保护受干扰热带海草草甸碳储量的关键组成部分
海草草甸虽然只占海底的一小部分,但在海洋碳封存中起着关键作用。然而,这一作用背后的机制仍然不确定,因为在绘制海草的范围和通量、计算碳储量的空间变化以及结合特定地点的历史方面存在挑战。本研究探讨了大堡礁地区大型海草草甸短期(≤10年)海草流失对沉积物碳储量的影响。利用遥感数据构建海草恢复时间线,结合野外采样和生态因子评估,我们发现在整个研究期间海草覆盖保持的区域沉积物有机碳含量较高。碳储量和沉积物积累随恢复阶段的不同而变化,并受生态因子和海草缺失长度的影响。沉积碳储量在保留区和3-8年内恢复区之间的差异很小,表明在这一时间段内发生恢复时,干扰对碳储量的影响有限。然而,在持续草甸区和未发生海草恢复≥10年的地点之间,碳储量存在显著差异。草甸碳含量为39,779 Mg (1 m),其空间变化与海草损失和恢复历史以及生态和环境因素有关。我们的研究结果为草甸损失期间海草蓝碳的持久性提供了背景,并表明沉积碳储量可以在类似的系统中持续存在,经历3至8年的海草损失和恢复周期。
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来源期刊
Marine pollution bulletin
Marine pollution bulletin 环境科学-海洋与淡水生物学
CiteScore
10.20
自引率
15.50%
发文量
1077
审稿时长
68 days
期刊介绍: Marine Pollution Bulletin is concerned with the rational use of maritime and marine resources in estuaries, the seas and oceans, as well as with documenting marine pollution and introducing new forms of measurement and analysis. A wide range of topics are discussed as news, comment, reviews and research reports, not only on effluent disposal and pollution control, but also on the management, economic aspects and protection of the marine environment in general.
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