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Shouliang Huo
Cyanobacteria have ruled marine situations and have been reef builders on Soil for more than three million a long time (myr). Cyanobacteria still play an fundamental part in advanced coral reef biological systems by shaping a major component of epiphytic, epilithic, and endolithic communities as well as of microbial mats. Cyanobacteria are brushed by reef life forms additionally give nitrogen to the coral reef environments through nitrogen obsession. As of late, modern unicellular cyanobacteria that express nitrogenase were found within the open sea and in coral reef tidal ponds. Moreover, cyanobacteria are critical in calcification and decalcification. All limestone surfaces have a layer of boring green growth in which cyanobacteria frequently play a prevailing part. Cyanobacterial symbioses are plenteous in coral reefs; the foremost common has are wipes and ascidians. Cyanobacteria utilize strategies past space occupation to restrain coral enrolment. Cyanobacteria can moreover shape pathogenic microbial consortia in affiliation with other organisms on living coral tissues, causing coral tissue lysis and passing, and significant decreases in coral reefs. In profound tidal ponds, coccoid cyanobacteria are inexhaustible and are touched by ciliates, heteroflagellates, and the benthic coral reef community. Cyanobacteria create metabolites that act as attractants for a few species and obstructions for a few grazers of the reef communities.