Coral reefs are one of the most productive and diverse ecosystems on the biosphere, with gross primary production rates ranging from 256 to 1,696 mmol C m −2 day −1 , comparable to that of tropical rain forests (Silveira et al., 2017). In contrast to open and coastal oceans where phytoplankton is generally the major local producer of organic matter (Opsahl & Benner, 1997), high gross primary production in coral reef ecosystems mostly results from the benthic organisms, including corals, coral-associated symbiotic zooxanthellae, turfs, and macroalgae (Cardini et al., 2016). These reef benthic organisms release organic matter, a heterogeneous mixture of proteins, lipids, and polysaccharides, to sustain high production of coral reefs (Ducklow & Mitchell, 1979;Haas & Wild, 2010). Growing evidence suggests that organic matter derived from reef benthic organisms is highly bioavailable to sustain the diverse and rich bacteria (Haas et al., 2016;Rohwer et al., 2002). Meanwhile, bacterial abundance (BA) in the coral reefs is generally higher than the surrounding pristine seawater owing to labile organic matter originating from reef benthos (Nakajima et al., 2013;Torréton & Dufour, 1996).