Centre for Ecology and Conservation, University of Exeter, Cornwall, UK.
Department of Earth Sciences, Utrecht University, Utrecht, The Netherlands.
Glob Chang Biol. 2022 May;28(9):2875-2894. doi: 10.1111/gcb.16105. Epub 2022 Feb 17.
Subtidal marine sediments are one of the planet's primary carbon stores and strongly influence the oceanic sink for atmospheric CO . By far the most widespread human activity occurring on the seabed is bottom trawling/dredging for fish and shellfish. A global first-order estimate suggested mobile demersal fishing activities may cause 0.16-0.4 Gt of organic carbon (OC) to be remineralized annually from seabed sediment carbon stores (Sala et al., 2021). There are, however, many uncertainties in this calculation. Here, we discuss the potential drivers of change in seabed sediment OC stores due to mobile demersal fishing activities and conduct a literature review, synthesizing studies where this interaction has been directly investigated. Under certain environmental settings, we hypothesize that mobile demersal fishing would reduce OC in seabed stores due to lower production of flora and fauna, the loss of fine flocculent material, increased sediment resuspension, mixing and transport and increased oxygen exposure. Reductions would be offset to varying extents by reduced faunal bioturbation and community respiration, increased off-shelf transport and increases in primary production from the resuspension of nutrients. Studies which directly investigated the impact of demersal fishing on OC stocks had mixed results. A finding of no significant effect was reported in 61% of 49 investigations; 29% reported lower OC due to fishing activities, with 10% reporting higher OC. In relation to remineralization rates within the seabed, four investigations reported that demersal fishing activities decreased remineralization, with three reporting higher remineralization rates. Patterns in the environmental and experimental characteristics between different outcomes were largely indistinct. More evidence is urgently needed to accurately quantify the impact of anthropogenic physical disturbance on seabed carbon in different environmental settings and to incorporate full evidence-based carbon considerations into global seabed management.
潮下带海洋沉积物是地球主要碳储存库之一,对海洋吸收大气 CO 的作用影响巨大。迄今为止,在海底进行的最广泛的人类活动是底拖网/挖泥船捕捞鱼类和贝类。一项全球一级的初步估计表明,移动的底栖捕鱼活动可能导致每年有 0.16-0.4 吉吨的有机碳(OC)从海底沉积物碳储量中再矿化(Sala 等人,2021 年)。然而,在这一计算中存在许多不确定性。在这里,我们讨论了由于底栖拖网捕鱼活动而导致海底沉积物 OC 储量变化的潜在驱动因素,并进行了文献综述,综合研究了这一相互作用直接调查的研究。在某些环境条件下,我们假设由于动植物产量减少、细絮凝物质损失、增加沉积物再悬浮、混合和输运以及增加氧气暴露,底栖拖网捕鱼会减少海底储存的 OC。这种减少在一定程度上会因减少的动物生物扰动和群落呼吸、增加的离岸运输以及从营养物再悬浮中增加的初级生产力而得到补偿。直接调查底栖捕鱼对 OC 储量影响的研究结果喜忧参半。在 49 项调查中,有 61%的调查结果报告没有显著影响;29%的报告显示由于捕捞活动导致 OC 减少,10%的报告显示 OC 增加。关于海底再矿化率,有四项调查报告称底栖捕鱼活动降低了再矿化率,有三项报告称再矿化率较高。不同结果之间的环境和实验特征模式基本上没有区别。迫切需要更多的证据来准确量化人为物理干扰对不同环境条件下海底碳的影响,并将基于充分证据的碳考虑因素纳入全球海底管理。