全球气候变化和珊瑚的耐热性

O. Hoegh‐Guldberg
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引用次数: 32

摘要

造礁珊瑚的热环境对它们的分布和生存至关重要。最近的证据表明,在过去的一个世纪里,全球平均气温上升了1摄氏度。对热带海洋温度的研究表明,它们在过去100年中也增加了近1°C,目前正以每世纪约1-2°C的速度增加。日本海域也不例外。冲绳海域自1930年以来上升了1.4°C,目前正以每世纪2.3°C的速度上升(95%置信区间为1.4-3.1°C)。当珊瑚及其虫黄藻的耐热性超过时,珊瑚就会发生白化,这可能是由于虫黄藻对慢性光抑制的敏感性增加。白化的后果可能是毁灭性的,珊瑚大量死亡,珊瑚繁殖等方面受到严重限制。1998年,世界上的珊瑚礁经历了有史以来最严重的白化。日本的珊瑚礁受到严重影响,1998年7月至8月,白化现象与大规模的温度异常同时发生。大量珊瑚死亡。本文的目的是从生物化学,生理学和生态学的角度收集我们对珊瑚白化的了解,并讨论珊瑚礁(特别是冲绳周围)在下个世纪可能发生的变化。在这些讨论中出现了一个重要的问题。如果温度继续升高,珊瑚将经历更大的白化和死亡,除非它们能在生理上或基因上适应。从这个问题中得出的结论令人非常关注。首先,现有的证据表明,珊瑚在生理上并没有真正适应海洋温度的零星和季节性变化。其次,海洋温度的变化速度可以说超过了珊瑚种群的基因适应能力。第三个结论是最令人担忧的。如果珊瑚变化不够快,那么珊瑚礁将经历更频繁和更严重的白化。考虑到1998年白化事件对地球上许多珊瑚礁造成的影响,这必须引起世界各地珊瑚礁使用者和管理者的高度关注。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Global climate change and the thermal tolerance of corals
The thermal environment of reef-building corals is critical to their distribution and survival. Recent evidence has revealed that the mean global temperature has increased by 1 degree Celsius over the past century. Examination of tropical sea temperatures reveal that they have also increased by almost 1°C over the past 100 years and are currently increasing at the rate of approximately 1-2°C per century. Japanese waters are no exception. Waters off Okinawa have increased by 1.4°C since 1930 and are currently increasing at the rate of 2.3°C per century (95% confidence interval, 1.4-3.1°C). Coral bleaching occurs when the thermal tolerance of corals and their zooxanthellae are exceeded, probably due to an increased sensitivity of the zooxanthellae to chronic photoinhibition. The consequences of bleaching can be devastating, with corals dying in vast numbers and such aspects as coral reproduction being severely curtailed. In 1998, the world's coral reefs experienced the worst bleaching on record. Japanese reefs were severely effected, with bleaching coinciding with a massive temperature anomaly in July-August 1998. Vast numbers of corals died. The intention of this paper is collect what we know about coral bleaching from biochemical, physiological and ecological perspectives and to discuss to how reefs (especially around Okinawa) might change in the next century. A single important issue surfaces in these deliberations. If temperatures continue to increase, then corals will experience greater incidences of bleaching and mortality unless they can acclimate physiologically or adapt genetically. The conclusions that stem from this issue are of great concern. Firstly, available evidence suggests that corals are not acclimating physiologically to any really extent to the sporadic and seasonal changes in sea temperature. Secondly, the rate of change in sea temperature arguably exceeds the capacity of coral populations to genetically adapt fast enough. The third conclusion is the most worrying. If corals are not changing fast enough, then coral reefs will experience more frequent and more intense bleaching. Given the outcome for many coral reefs across the planet during the 1998 episodes of bleaching, this has to be of great concern to coral reef users and managers everywhere.
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