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Contrasting spawning temperature optima: Why are anchovy and sardine regime shifts synchronous across the North Pacific?

机译:产卵温度的最佳对比:为什么Why鱼和沙丁鱼的变化在北太平洋同步发生?

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Anchovy and sardine are both abundant small pelagic fish that have exhibited out-of-phase population oscillations in both the western boundary current region off Japan and the eastern boundary current upwelling region off California. These species alternations could indicate approximately synchronous patterns (with some variations in timing between ecosystems) despite the reversed temperature regimes for certain periods across the North Pacific, at least until recently. Here we suggest a contrasting pattern of temperature optima for anchovy and sardine spawnings between the opposite sides of the North Pacific as a possible mechanism of the synchronous phases of species alternations. Spawning temperature optima were examined for Japanese anchovy (Engraulis japonicus) and Japanese sardine (Sardinops mela-nostictus), based on occurrence of eggs and larvae in relation to sea surface temperature. The analyses were based on an updated long-term data set of egg and larval surveys from 1978 to 2004 (102,660 net tows) in the western North Pacific. The ratio of relative frequencies of plankton net samples that are positive for eggs or larvae versus all samples was calculated for temperature intervals of 0.1 ℃ for both species. This spawning temperature index exceeded 1.0 (baseline for optimum) from ca. 15 to 28 ℃ with a mid-point at 22 ℃ for anchovy and ca. 13-20 ℃ with a marked peak at 16-17 ℃ for sardine. Patterns of spawning temperature clearly show "warm" and "eurythermal" Japanese anchovy and "cool" and "stenothermal" Japanese sardine in the western North Pacific. This relationship between anchovy and sardine showed a marked contrast to earlier published reports on the spawning temperature optima of northern anchovy (E. mordax) and California sardine (S. sagqx) in the California Current system. The spawning temperature optimum appears to be species-specific rather than genus-specific. The reversed species-specific temperature optima of anchovy and sardine under the reversed temperature regimes could provide a possible theoretical solution to the synchronous anchovy and sardine regime shifts across the North Pacific.
机译:cho鱼和沙丁鱼都是丰富的中上层鱼类,在日本境外的西部边界流域区域和加州境外的东部边界流域上升区域均表现出异相种群振荡。尽管整个北太平洋的某些时期的温度体制发生了逆转,但至少直到最近,这些物种的交替可能表明它们的模式大致同步(生态系统之间的时间有一些变化)。在这里,我们提出了北太平洋对岸之间between鱼和沙丁鱼产卵温度最佳形成对比的模式,这是物种交替同步阶段的可能机制。根据与海表温度有关的卵和幼虫的发生情况,对日本an鱼(Engraulis japonicus)和日本沙丁鱼(Sardinops mela-nostictus)的产卵温度进行了优化。这些分析是基于1978年至2004年北太平洋西部地区卵和幼虫调查的最新长期数据集(净拖曳量为102,660)。对于两种物种,温度间隔为0.1℃,计算出卵或幼虫为阳性的浮游生物网样品的相对频率与所有样品的相对频率之比。此产卵温度指数从大约1超过1.0(最佳基准)。 15到28℃,中点在22℃,an鱼和约。 13-20℃,沙丁鱼在16-17℃有一个明显的峰。产卵温度的模式清楚地显示出北太平洋西部的“温暖”和“极热”日本an鱼和“凉”和“绝热”日本沙丁鱼。 earlier鱼和沙丁鱼之间的这种关系与早先发表的有关加利福尼亚流系统中北部northern鱼(E. mordax)和加利福尼亚沙丁鱼(S. sagqx)的产卵温度最优化的报道形成了鲜明对比。最佳产卵温度似乎是物种特定的,而不是属特定的。在相反的温度条件下,cho鱼和沙丁鱼的物种特异性温度最优值反向,可以为整个北太平洋的an鱼和沙丁鱼同步变化提供理论上的可能解决方案。

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