Coral growth along a natural gradient of seawater temperature, pH, and oxygen in a nearshore seagrass bed on Dongsha Atoll, Taiwan.

Similarly, while Indo-Pacific massive Porites skeletal density has been reported as either inversely correlated to calcification [ 79 ] or not significantly correlated at all [ 83 , 85 ], we observed a weakly significant positive relationship for the corals at the mid and outer sites, and a significant negative relationship for the nearshore corals ( Fig 5E and S5 Table ).

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