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Trailing edges projected to move faster than leading edges for large pelagic fish habitats under climate change

机译:在气候变化下,大型中上层鱼类栖息地的后缘移动速度比前缘快

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There is mounting evidence to suggest that many species are shifting their ranges in concordance with the climate velocity of their preferred environmental conditions/habitat While accelerated rates in species' range shifts have been noted in areas of intense warming, due to climate change, few studies have considered the influence that both spatial temperature gradients and rates of warming (i.e., the two components of climate velocity) could have on rates of movement in species habitats. We compared projected shifts in the core habitat of nine large pelagic fish species (five tuna, two billfish and two shark species) off the east coast of Australia at different spatial points (centre, leading and trailing edges of the core habitat), during different seasons (summer and winter), in the near-(2030) and long-term (2070), using independent species distribution models and habitat suitability models. Model projections incorporated depth integrated temperature data from 11 climate models with a focus on the IPCC SRES A2 general emission scenario. Projections showed a number of consistent patterns: southern (poleward) shifts in all species' core habitats; trailing edges shifted faster than leading edges; shifts were faster by 2070 than 2030; and there was little difference in shifts among species and between seasons. Averaging across all species and climate models, rates of habitat shifts for 2030 were 45-60 km decade(-1) at the trailing edge, 40-45 km decade(-1) at the centre, and 20-30 km decade(-1) at the leading edge. Habitat shifts for 2070 were 60-70 km decade(-1) at the trailing edge, 50-55 km decade(-1) at the centre, and 30-40 km decade(-1) at the leading edge. It is often assumed that the leading edge of a species range will shift faster than the trailing edge, but there are few projections or observations in large pelagic fish to validate this assumption. We found that projected shifts at the trailing edge were greater than at the centre and leading of core habitats in all large pelagic fish included in our study. Faster shifts at species trailing edges were due to weaker spatial gradients in temperature in the north than in the south of the study region, in conjunction with relatively constant rates of warming across latitudes. Rather than assuming that leading edges will always move faster, this study suggests that spatial gradients of temperature could be important in determining differences in shifts at different points in species core habitats. (C) 2014 Elsevier Ltd. All rights reserved.
机译:越来越多的证据表明,许多物种正在根据其首选环境条件/栖息地的气候速度改变其范围。虽然由于气候变化,在剧烈变暖的地区,物种范围的改变速度有所加快,但很少有研究已经考虑了空间温度梯度和变暖速率(即气候速度的两个分量)可能对物种生境的运动速率的影响。我们比较了澳大利亚东海岸外9个大型远洋鱼类物种(5种金枪鱼,2条比目鱼和2种鲨鱼)的核心生境在不同空间点(核心生境的中心,前缘和后缘)在不同时期的预计变化(2030)和长期(2070)的季节(夏季和冬季),使用独立的物种分布模型和生境适应性模型。模型预测结合了来自11个气候模型的深度综合温度数据,重点是IPCC SRES A2一般排放情景。投影显示出许多一致的模式:所有物种的核心栖息地向南(极地)移动;后缘比前缘移动得快;到2070年,变化要比2030年快;物种之间和季节之间的变化几乎没有差异。根据所有物种和气候模型的平均值,到2030年的栖息地迁移速率在后缘为45-60 km十年(-1),在中心为40-45 km十年(-1),以及20-30 km十年(- 1)在前沿。 2070年的生境变化在后缘为60-70 km十年(-1),在中心为50-55 km十年(-1),在前沿为30-40 km十年(-1)。通常认为,某个物种范围的前缘将比后缘移动得快,但是在大型远洋鱼类中很少有预测或观察到的证据可以证实这一假设。我们发现,在我们的研究中,所有大型远洋鱼类的后缘预计移动量都大于中心和核心生境的移动量。物种后缘更快的变化是由于研究区域北部的温度空间梯度小于南部的温度梯度,以及跨纬度相对恒定的升温速度所致。该研究表明,温度的空间梯度对于确定物种核心栖息地不同点的变化差异可能不重要,而不是假设前沿总是会移动得更快。 (C)2014 Elsevier Ltd.保留所有权利。

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