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估算有无捕捞情况下海洋鱼类的全球生物量及生物地球化学循环。

Estimating global biomass and biogeochemical cycling of marine fish with and without fishing.

作者信息

Bianchi Daniele, Carozza David A, Galbraith Eric D, Guiet Jérôme, DeVries Timothy

机构信息

Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, Los Angeles, CA, USA.

Département de Mathématiques, Université du Québec à Montréal, Montréal, Quebec, Canada.

出版信息

Sci Adv. 2021 Oct 8;7(41):eabd7554. doi: 10.1126/sciadv.abd7554.

Abstract

The biomass and biogeochemical roles of fish in the ocean are ecologically important but poorly known. Here, we use a data-constrained marine ecosystem model to provide a first-order estimate of the historical reduction of fish biomass due to fishing and the associated change in biogeochemical cycling rates. The pre-exploitation global biomass of exploited fish (10 g to 100 kg) was 3.3 ± 0.5 Gt, cycling roughly 2% of global primary production (9.4 ± 1.6 Gt year) and producing 10% of surface biological export. Particulate organic matter produced by exploited fish drove roughly 10% of the oxygen consumption and biological carbon storage at depth. By the 1990s, biomass and cycling rates had been reduced by nearly half, suggesting that the biogeochemical impact of fisheries has been comparable to that of anthropogenic climate change. Our results highlight the importance of developing a better mechanistic understanding of how fish alter ocean biogeochemistry.

摘要

鱼类在海洋中的生物量和生物地球化学作用在生态上很重要,但却鲜为人知。在此,我们使用一个数据受限的海洋生态系统模型,对因捕捞导致的鱼类生物量的历史减少以及生物地球化学循环速率的相关变化进行一阶估计。被捕捞鱼类(10克至100千克)在开发前的全球生物量为33±5亿吨,循环利用约2%的全球初级生产量(94±16亿吨/年),并产生10%的表层生物输出。被捕捞鱼类产生的颗粒有机物质推动了约10%的深层氧气消耗和生物碳储存。到20世纪90年代,生物量和循环速率已减少近一半,这表明渔业对生物地球化学的影响已与人为气候变化的影响相当。我们的结果凸显了更好地从机制上理解鱼类如何改变海洋生物地球化学的重要性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5c2e/8500507/d45ee543d873/sciadv.abd7554-f1.jpg

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