Department of Environmental Biology and Fisheries Science, National Taiwan Ocean University, Keelung, Taiwan, R.O.C.
Department of Environmental Biology and Fisheries Science, National Taiwan Ocean University, Keelung, Taiwan, R.O.C..
Sci Rep. 2022 Aug 12;12(1):13715. doi: 10.1038/s41598-022-17882-w.
Spatial variations in tuna population and abundance are strongly linked to large-scale climate fluctuations, such as the Pacific decadal oscillation (PDO) and Atlantic multidecadal oscillation (AMO). However, the mechanisms underlying the association of climate indices with yellowfin tuna (YFT) abundance and habitat preference remain unclear. We analysed long-term longline fishery data for YFT and oceanic climate variability index data for 1971-2018. The standardized catch per unit effort (CPUE) of Indo-Pacific Ocean YFT was higher during negative AMO and positive PDO phases. In tropical Pacific Ocean, the trend of YFT habitat preference exhibited seesaw patterns because of the distinct environmental factors influenced by the PDO phase. The PDO changed the environmental parameters throughout the tropical Indian Ocean such that the habitat preference of YFT remained consistent throughout. However, the variations in habitat suitability did not correspond to the distribution or standardized CPUE of YFT throughout the Pacific Ocean during AMO events. Moreover, the changes in habitat suitability had a positive periodicity of 8-16 years with AMO in the Indian Ocean, but revealed opposite trends with the distribution or standardized CPUE of YFT. Our results provide sufficient information to distinguish the variations between PDO phase changing and YFT standardized CPUE/ habitat preference. Furthermore, the AMO phase shift period 60-100 years longer than that of the PDO (20-30 years), and models employing time series of fishery and environmental data must be extended the time period of our study to make the AMO match the fishery data more complete.
金枪鱼种群和丰度的空间变化与大规模的气候波动密切相关,如太平洋十年涛动(PDO)和大西洋多年代际振荡(AMO)。然而,气候指数与黄鳍金枪鱼(YFT)丰度和栖息地偏好之间关联的机制仍不清楚。我们分析了 1971-2018 年长时间延绳钓渔业数据和海洋气候变率指数数据。印度洋-太平洋 YFT 的标准化单位捕捞努力量(CPUE)在负 AMO 和正 PDO 阶段较高。在热带太平洋,由于受 PDO 阶段影响的环境因素不同,YFT 栖息地偏好的趋势呈现出跷跷板模式。PDO 改变了整个热带印度洋的环境参数,使 YFT 的栖息地偏好保持一致。然而,在 AMO 事件期间,栖息地适宜性的变化与太平洋 YFT 的分布或标准化 CPUE 并不对应。此外,在印度洋,与 YFT 的分布或标准化 CPUE 相反,栖息地适宜性的变化与 AMO 呈正周期性,周期为 8-16 年。我们的研究结果提供了足够的信息来区分 PDO 相位变化和 YFT 标准化 CPUE/栖息地偏好之间的变化。此外,AMO 相位的变化周期比 PDO 长 60-100 年(20-30 年),并且采用渔业和环境数据时间序列的模型必须延长我们研究的时间段,以使 AMO 更完整地与渔业数据匹配。