Bleaching occurs when the tiny plant-like coral organisms die, often because of higher temperatures, and leave behind only a white limestone reef skeleton.
细小而形似植物的珊瑚生物死亡时会褪色变白，原因通常是不断升高的温度，留下的只是一具白色的石灰岩珊瑚礁骨架。
This paper introduces the geological features and the unhomogeneous weathering phenomenon of coral reef limestone of Sudan Port Area, and the bearing capacity of this layer.
简单介绍苏丹港区珊瑚礁灰岩的地质特征及不均匀风化现象，以及该层的地基承载力。
Bleaching occurs when the organisms that make up coral die and leave behind the white limestone skeleton of the reef.
白化现象即组成珊瑚的生物于死亡后所留下、如石灰石般的骨骼。
Bleaching occurs when the organisms that make up coral die and leave behind the white limestone skeleton of the reef.
白化现象即组成珊瑚的生物于死亡后所留下、如石灰石般的骨骼。
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