Sheppard Charles R C
Department of Biological Sciences, University of Warwick, Coventry CV4 7AL, UK.
Nature. 2003 Sep 18;425(6955):294-7. doi: 10.1038/nature01987.
In 1998, more than 90% of shallow corals were killed on most Indian Ocean reefs. High sea surface temperature (SST) was a primary cause, acting directly or by interacting with other factors. Mean SSTs have been forecast to rise above the 1998 values in a few decades; however, forecast SSTs rarely flow seamlessly from historical data, or may show erroneous seasonal oscillations, precluding an accurate prediction of when lethal SSTs will recur. Differential acclimation by corals in different places complicates this further. Here I scale forecast SSTs at 33 Indian Ocean sites where most shallow corals died in 1998 (ref. 1) to identify geographical patterns in the timing of probable repeat occurrences. Reefs located 10-15 degrees south will be affected every 5 years by 2010-2025. North and south from this, dates recede in a pattern not directly related to present SSTs; paradoxically, some of the warmest sites may be affected last. Temperatures lethal to corals vary in this region by 6 degrees C, and acclimation of a modest 2 degrees C by corals could prolong their survival by nearly 100 years.
1998年,印度洋大部分珊瑚礁上90%以上的浅海珊瑚死亡。高海表温度(SST)是主要原因,它直接作用或与其他因素相互作用。预计在几十年内平均海表温度将升至高于1998年的水平;然而,预测的海表温度很少能直接从历史数据中得出,或者可能显示出错误的季节性振荡,从而无法准确预测致命海表温度何时会再次出现。不同地区的珊瑚适应性差异使情况更加复杂。在此,我对1998年多数浅海珊瑚死亡的33个印度洋站点的预测海表温度进行了尺度分析,以确定可能再次出现的时间的地理模式。到2010 - 2025年,南纬10 - 15度的珊瑚礁每5年就会受到影响。在此范围以北和以南,时间间隔呈一种与当前海表温度无直接关联的模式向后推迟;自相矛盾的是,一些温度最高的站点可能最后才受到影响。该地区对珊瑚致命的温度相差6摄氏度,而珊瑚适度适应2摄氏度的温度变化就能使其存活期延长近100年。