Purcell Kevin M, Craig J Kevin, Nance James M, Smith Martin D, Bennear Lori S
National Marine Fisheries Service, Southeast Fisheries Science Center, Beaufort Laboratory, Beaufort, NC, United States of America.
National Marine Fisheries Service, Southeast Fisheries Science Center, Galveston Laboratory, Galveston, TX, United States of America.
PLoS One. 2017 Aug 24;12(8):e0183032. doi: 10.1371/journal.pone.0183032. eCollection 2017.
The northwestern Gulf of Mexico shelf experiences one of the largest seasonal hypoxic zones in the western hemisphere. Hypoxia (dissolved oxygen, DO ≤ 2.0 mg·L-1) is most severe from May to August during the height of the Gulf shrimp fishery, but its effects on the fishery are not well known. Prior studies indicate that hypoxia alters the spatial dynamics of shrimp and other species through habitat loss and aggregation in nearby oxygenated refuge habitats. We hypothesized that hypoxia-induced changes in the distribution of shrimp also alter the spatial dynamics of the Gulf shrimp fleet. We integrated data on the geographic distribution of shrimp tows and bottom DO to evaluate the effects of hypoxia on spatial patterns in shrimping effort. Our analyses indicate that shrimping effort declines in low DO waters on both the Texas and Louisiana shelf, but that considerable effort still occurs in low DO waters off Louisiana, likely because riverine nutrients fuel both benthic production and low bottom DO in the same general regions. The response of the shrimp fleet to hypoxia on the Louisiana shelf was complex with shifts in effort inshore, offshore, westward, and eastward of the hypoxic zone, as well as to an oxygenated area between two hypoxia regimes associated with the Mississippi and the Atchafalaya River outflows. In contrast, effort on the Texas shelf mostly shifted offshore in response to low DO but also shifted inshore in some years. Spatial patterns in total shrimping effort were driven primarily by the number of shrimp tows, consistent with aggregation of the fleet outside of hypoxic waters, though tow duration also declined in low DO waters. Overall, our results demonstrate that hypoxia alters the spatial dynamics of the Gulf shrimp fishery with potential consequences for harvest interactions and the economic condition of the fishery.
墨西哥湾西北部大陆架是西半球最大的季节性缺氧区之一。缺氧(溶解氧,DO≤2.0mg·L-1)在墨西哥湾虾类渔业旺季的5月至8月最为严重,但其对渔业的影响尚不清楚。先前的研究表明,缺氧通过栖息地丧失以及在附近含氧避难栖息地的聚集,改变了虾类和其他物种的空间动态。我们假设,缺氧导致的虾类分布变化也会改变墨西哥湾虾类捕捞船队的空间动态。我们整合了虾类拖网捕捞的地理分布数据和底层溶解氧数据,以评估缺氧对捕捞作业空间格局的影响。我们的分析表明,在得克萨斯州和路易斯安那州大陆架的低溶解氧水域,捕捞作业量下降,但在路易斯安那州近海的低溶解氧水域仍有大量捕捞作业,这可能是因为河流养分在同一大致区域促进了底栖生物的生产以及底层低溶解氧状况。路易斯安那州大陆架上的虾类捕捞船队对缺氧的反应较为复杂,捕捞作业在缺氧区的近岸、离岸、向西和向东方向发生了转移,同时也转移到了与密西西比河和阿查法拉亚河河口流出相关的两个缺氧区域之间的一个含氧区域。相比之下,得克萨斯州大陆架上的捕捞作业大多因低溶解氧而向近海转移,但在某些年份也会向近岸转移。总的虾类捕捞作业空间格局主要由虾类拖网捕捞次数驱动,这与捕捞船队在缺氧水域之外的聚集情况一致,不过在低溶解氧水域拖网持续时间也有所下降。总体而言,我们的结果表明,缺氧改变了墨西哥湾虾类渔业的空间动态,可能对捕捞相互作用和渔业经济状况产生影响。