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首页> 外文期刊>Frontiers in Marine Science >Thermal Niche Tracking and Future Distribution of Atlantic Mackerel Spawning in Response to Ocean Warming
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Thermal Niche Tracking and Future Distribution of Atlantic Mackerel Spawning in Response to Ocean Warming

机译:海洋变暖对大西洋鲭鱼产卵的热生态位追踪和未来分布

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North-east Atlantic mackerel spawning distribution has shifted northward in the last three decades probably in response to global sea warming. Yet, uncertainties subsist regarding on the shift rate, causalities, and how this species will respond to future conditions. Using egg surveys, we explored the influence of temperature change on mackerel’s spawning distribution (western and southern spawning components of the stock) between 1992 and 2013, and projected how it may change under future climate change scenarios. We developed three generalized additive models: (i) a spatiotemporal model to reconstruct the spawning distribution for the north-east Atlantic stock over the period 1992-2013, to estimate the rate of shift; (ii) a thermal habitat model to assess if spawning mackerel have tracked their thermal spawning-niche; and (iii) a niche-based model to project future spawning distribution under two predicted climate change scenarios. Our findings showed that mackerel spawning activity has shifted northward at a rate of 15.9 ± 0.9 km/decade between 1992 and 2013. Similarly, using the thermal habitat model, we detected a northward shift of the thermal spawning-niche. This indicates that mackerel has spawned at higher latitudes to partially tracking their thermal spawning-niche, at a rate of 28.0 ± 9.0 km/°C of sea warming. Under future scenarios (mid and end of the century), the extrapolation of the niche-based model to coupled hydroclimatic and biogeochemical models indicates that centre of gravity of mackerel spawning distribution is expected to shift westward (32 to 117 km) and northward (0.5 to 328 km), but with high variability according to scenarios and time frames. The future of the overall egg production in the area is uncertain (change from -9.3% to 12%). With the aim to allow the fishing industry to anticipate the future distribution of mackerel shoals during the spawning period, future research should focus on reducing uncertainty in projections.
机译:在过去的三十年中,东北大西洋鲭鱼的产卵分布向北移动,可能是由于全球海洋变暖所致。然而,关于转移率,因果关系以及该物种将如何应对未来条件的不确定性仍然存在。通过鸡蛋调查,我们研究了1992年至2013年温度变化对鲭鱼产卵分布(种群的西部和南部产卵成分)的影响,并预测了在未来的气候变化情景下温度可能如何变化。我们开发了三个广义的加性模型:(i)时空模型,以重建1992-2013年期间东北大西洋种群的产卵分布,以估计偏移率; (ii)一个热栖息地模型,以评估产卵鲭鱼是否已经追踪了其产卵的生态位; (iii)基于生态位的模型来预测两种预测的气候变化情景下的未来产卵分布。我们的发现表明,鲭鱼的产卵活动在1992年至2013年期间以15.9±0.9 km / decade的速率向北移动。类似地,使用热生境模型,我们检测到了热产卵位的北移。这表明鲭鱼在较高的纬度产卵,以28.0±9.0 km /°C的海洋升温速率部分追踪其热产卵位。在未来的情况下(本世纪中叶和本世纪末),将基于生态位的模型外推到耦合的水文气候和生物地球化学模型表明,鲭鱼产卵场的重心有望向西(32至117 km)向北移动(0.5到328公里),但根据情况和时间框架具有较高的可变性。该地区鸡蛋总产量的未来不确定(从-9.3%变为12%)。为了使捕捞业能够预期在产卵期间鲭鱼浅滩的未来分布,未来的研究应集中于减少预测的不确定性。

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