ARC Centre of Excellence for Coral Reef Studies, James Cook University, Townsville, QLD 4811, Australia.
J Exp Biol. 2012 Nov 15;215(Pt 22):3865-73. doi: 10.1242/jeb.074765.
Average sea-surface temperature and the amount of CO(2) dissolved in the ocean are rising as a result of increasing concentrations of atmospheric CO(2). Many coral reef fishes appear to be living close to their thermal optimum, and for some of them, even relatively moderate increases in temperature (2-4°C) lead to significant reductions in aerobic scope. Reduced aerobic capacity could affect population sustainability because less energy can be devoted to feeding and reproduction. Coral reef fishes seem to have limited capacity to acclimate to elevated temperature as adults, but recent research shows that developmental and transgenerational plasticity occur, which might enable some species to adjust to rising ocean temperatures. Predicted increases in P(CO(2)), and associated ocean acidification, can also influence the aerobic scope of coral reef fishes, although there is considerable interspecific variation, with some species exhibiting a decline and others an increase in aerobic scope at near-future CO(2) levels. As with thermal effects, there are transgenerational changes in response to elevated CO(2) that could mitigate impacts of high CO(2) on the growth and survival of reef fishes. An unexpected discovery is that elevated CO(2) has a dramatic effect on a wide range of behaviours and sensory responses of reef fishes, with consequences for the timing of settlement, habitat selection, predator avoidance and individual fitness. The underlying physiological mechanism appears to be the interference of acid-base regulatory processes with brain neurotransmitter function. Differences in the sensitivity of species and populations to global warming and rising CO(2) have been identified that will lead to changes in fish community structure as the oceans warm and becomes more acidic; however, the prospect for acclimation and adaptation of populations to these threats also needs to be considered. Ultimately, it will be the capacity for species to adjust to environmental change over coming decades that will determine the impact of climate change on marine ecosystems.
由于大气中二氧化碳浓度的增加,海水表面平均温度和溶解在海洋中的二氧化碳含量都在上升。许多珊瑚礁鱼类似乎生活在接近其热最佳状态的地方,对于其中一些鱼类,即使温度适度升高(2-4°C),也会导致有氧范围显著降低。有氧能力的降低可能会影响种群的可持续性,因为用于进食和繁殖的能量减少。珊瑚礁鱼类似乎在成年时适应高温的能力有限,但最近的研究表明,存在发育和跨代可塑性,这可能使一些物种能够适应不断上升的海洋温度。预计二氧化碳(P(CO(2)))的增加以及随之而来的海洋酸化也会影响珊瑚礁鱼类的有氧范围,尽管存在相当大的种间差异,一些物种在接近未来的二氧化碳水平下有氧范围下降,而另一些物种则增加。与热效应一样,对高二氧化碳的反应存在跨代变化,这可能减轻高二氧化碳对珊瑚礁鱼类生长和生存的影响。一个意想不到的发现是,升高的二氧化碳对珊瑚礁鱼类的广泛行为和感官反应产生了巨大影响,对定居时间、栖息地选择、捕食者回避和个体适应性都有影响。潜在的生理机制似乎是酸碱调节过程干扰了大脑神经递质的功能。已经确定了物种和种群对全球变暖以及二氧化碳升高的敏感性差异,随着海洋变暖并变得更加酸化,鱼类群落结构将发生变化;然而,还需要考虑种群对这些威胁的适应和适应能力。最终,物种适应环境变化的能力将决定气候变化对海洋生态系统的影响。