Coral Reefs and Atolls

W. Hobbs
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Abstract

Coral reefs are calcium carbonate (limestone) structures which are created by colonies of polyps that create a hard exoskeleton (the coral), which then becomes home to zooxanthellae which give the corals their colour. The zooxanthellae and corals live in a rela onship which is mutually beneficial, called a symbio c rela onship. Coral bleaching refers to the loss of the zooxanthellae, reducing the stability of the coral; they also lose their colour. Coral reefs have three main structure types. The first is a fringing reef, which forms along the shoreline of most tropical islands. The Barrier Reef is created through the sinking of land below the sea surface, due to a lack of volcanic ac vity. Lastly the third is an atoll, which is created similarly to the Barrier Reef, but the land sinks quicker, and the reef grows upwards to be near the sunlight.
珊瑚礁和环礁
珊瑚礁是由碳酸钙(石灰石)结构形成的,这种结构是由成群的珊瑚虫形成的,珊瑚虫形成了坚硬的外骨骼(珊瑚),然后成为虫黄藻的家园,虫黄藻赋予珊瑚颜色。虫黄藻和珊瑚生活在一种互利的关系中,这种关系被称为共生关系。珊瑚白化是指虫黄藻的丧失,降低了珊瑚的稳定性;它们也会失去颜色。珊瑚礁有三种主要的结构类型。第一个是沿大多数热带岛屿海岸线形成的边缘礁。由于缺乏火山活动,大堡礁是通过陆地下沉到海面以下而形成的。最后第三个是环礁,它的形成与大堡礁相似,但陆地下沉得更快,珊瑚礁向上生长,靠近阳光。
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