Research articleHydromechanical boundary layers over a coral reef
References (53)
- et al.
Effect of water motion on coral photosynthesis and calcification
J. Exp. Mar. Biol. Ecol.
(1988) - et al.
The influence of colony morphology and orientation to flow on particle capture by the scleractinian coral Agaricia agaricites (Linnaeus)
J. Exp. Mar. Biol. Ecol.
(1993) Effects of water motion on reef corals
J. Exp. Mar. Biol. Ecol.
(1978)- et al.
Effects of morphology and water motion on carbon delivery and productivity in the reef coral, Pocillopora damicornis (Linnaeus): Diffusion barriers, inorganic carbon limitation and biochemical plasticity
J. Exp. Mar. Biol. Ecol.
(1994) - et al.
Hydrodynamic enhancement of larval settlement in the bivalve Mulinia lateralis (Say) and the polychaete Capitella sp. I in microdepositinal environments
J. Exp. Mar. Biol. Ecol.
(1993) - et al.
Skeletal modifications in stony corals caused by indwelling crabs: Hydromechanical advantages for crab feeding
Symbiosis
(1991) - et al.
Flow patterns induced by substrata and body morphologies of benthic organisms and their roles in determining availability of food particles
Limnol. Oceanogr.
(1993) - et al.
Influence of circulation on self-seeding patterns at Helix Reef-Great Barrier Reef
- et al.
Effects of water velocity on phosphate uptake in coral reef-flat communities
Limnol. Oceanogr.
(1992) - et al.
Water flow and hydromechanical adaptations of branched corals
Bull. Mar. Sci.
(1975)
Effects of temperature on photosynthesis and respiration in hermatypic corals
Mar. Biol.
Near-bed turbulence and hydrodynamic control of diffusional mass transfer at the sea floor
Limnol. Oceanogr.
Measurement of water movement in reference to benthic algal growth
Botanica Marina
Effects of flow on competitive superiority in scleractinian corals
Limnol. Oceanogr.
Effects on benthic diffusive boundary layer imposed by microelectrodes
Limnol. Oceanogr.
Reproduction, dispersal and recruitment in scleractinian corals
Preliminary observation on the abundance and distribution of planktonic coral larvae in Kaneohe Bay, Oahu, Hawaii
Sediment and the settlement of larvae of the reef coral Pocillopora damicornis
Coral Reefs
Effects of temperature on the mortality and growth of Hawaiian reef corals
Mar. Biol.
Hydromechanical adaptation in the solitary free-living coral Fungia scutaria
Nature
Water motion on coral reefs: evaluation of the ‘clod card’ technique
Mar. Ecol. Prog. Ser.
The diffusive boundary layer of sediments: Oxygen microgradients over microbial matter
Limnol. Oceanogr.
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Depth-related drivers of benthic community structure on shallow subtidal rocky reefs
2022, Estuarine, Coastal and Shelf ScienceCitation Excerpt :The morphology of P. caribaeorum colonies is known to minimize the mechanical effects of flowing water (Koehl, 1977) and at shallower depths it is also favored because more light is available for photosynthesis by its symbiotic zooxanthellae. Furthermore, suspension feeders such as P. caribaeorum, P. nigra and the sponge D. anchorata may benefit from a greater offer of suspended food brought by the greater exchange of water in the shallows (Shashar et al., 1996; de Santana et al., 2015). In contrast, the relative cover of the macroalgae Jania sp., Sargassum spp. and L. trichoclados, turf, the sponge D. reticulatum and the gorgonians L. setacea and L. punicea were mostly associated with the interface-bottom stratum (with colder, higher sediment cover and salinity, lower water movement and clarity conditions) (Fig. 2 and Table 2).