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Future habitat suitability for coral reef ecosystems under global warming and ocean acidification

机译:全球变暖和海洋酸化下珊瑚礁生态系统的未来生境适应性

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Rising atmospheric CO2 concentrations are placing spatially divergent stresses on the world's tropical coral reefs through increasing ocean surface temperatures and ocean acidification. We show how these two stressors combine to alter the global habitat suitability for shallow coral reef ecosystems, using statistical Bioclimatic Envelope Models rather than basing projections on any a priori assumptions of physiological tolerances or fixed thresholds. We apply two different modeling approaches (Maximum Entropy and Boosted Regression Trees) with two levels of complexity (one a simplified and reduced environmental variable version of the other). Our models project a marked temperature-driven decline in habitat suitability for many of the most significant and bio-diverse tropical coral regions, particularly in the central Indo-Pacific. This is accompanied by a temperature-driven poleward range expansion of favorable conditions accelerating up to 40-70km per decade by 2070. We find that ocean acidification is less influential for determining future habitat suitability than warming, and its deleterious effects are centered evenly in both hemispheres between 5 degrees and 20 degrees latitude. Contrary to expectations, the combined impact of ocean surface temperature rise and acidification leads to little, if any, degradation in future habitat suitability across much of the Atlantic and areas currently considered marginal' for tropical corals, such as the eastern Equatorial Pacific. These results are consistent with fossil evidence of range expansions during past warm periods. In addition, the simplified models are particularly sensitive to short-term temperature variations and their projections correlate well with reported locations of bleaching events. Our approach offers new insights into the relative impact of two global environmental pressures associated with rising atmospheric CO2 on potential future habitats, but greater understanding of past and current controls on coral reef ecosystems is essential to their conservation and management under a changing climate.
机译:大气中二氧化碳浓度的不断升高,通过增加海洋表面温度和海洋酸化作用,在世界热带珊瑚礁上造成了空间上的分散应力。我们使用统计的生物气候信封模型,而不是基于生理耐受性或固定阈值的任何先验假设进行预测,来说明这两种压力源如何结合起来改变全球浅海珊瑚礁生态系统的栖息地适应性。我们应用两种不同的建模方法(最大熵树和增强回归树),具有两种复杂度(一种是简化的且减少了环境变量的版本)。我们的模型预测了许多最重要和生物多样化的热带珊瑚地区,特别是中部印度洋-太平洋地区,温度驱动的栖息地适应性明显下降。伴随着温度驱动的极地范围扩展,到2070年,有利条件将加速至每十年40-70km。我们发现,海洋酸化对确定未来生境适宜性的影响小于变暖,其有害影响在这两个方面均集中纬度介于5度和20度之间的半球。与预期相反,海洋表面温度上升和酸化的综合影响导致整个大西洋大部分地区和目前被认为是热带珊瑚边缘地区(例如赤道东太平洋)的未来栖息地适应性几乎没有下降。这些结果与过去温暖时期范围扩大的化石证据一致。此外,简化的模型对短期温度变化特别敏感,它们的预测与报告的漂白事件位置具有很好的相关性。我们的方法为与大气CO2上升相关的两个全球环境压力对潜在的未来栖息地的相对影响提供了新的见解,但对气候变化不断变化下珊瑚礁生态系统的保护和管理至关重要的是,对珊瑚礁生态系统过去和当前的控制有更深入的了解。

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