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Mass transfer limitation of photosynthesis of coral reef algal turfs

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Abstract

Algal turfs are the major primary producing component on many coral reefs and this production supports higher levels in the complex reef trophic web. Rates of metabolism of algal turfs are related positively to water motion, consistent with limitation by the diffusion of a substance through a boundary layer. Based on engineering mass transfer theory, we hypothesized that photosynthesis of algal turfs is controlled by rates of mass transfer and responses of photosynthesis to increasing flow speed should be predicted by engineering correlations. This hypothesis was tested in ten experiments where photosynthesis was estimated in a flume/respirometer from changes in dissolved oxygen at eight flow speeds between 0.08 and 0.52 m/s. Flow in the flume and over the reef at Kaneohe Bay, Oahu, Hawaii was estimated using hot-film thermistor and electromagnetic current meters. Rates of photosynthesis were related positively to flow in all experiments and plots of the log of the average Sherwood number (Shmeas) versus log Reynolds number (ReD) for each experiment are lower than predicted for mass transfer through a turbulent boundary layer. Algal turf-covered plates are characterized as hydrodynamically transitional to fully rough surfaces and the lower than predicted slopes suggest that roughness reduces rates of mass transfer. A negative correlation between algal turf biomass and slopes of the log Shmeas−log ReD plots suggests that mass transfer to algal turfs is affected significantly by the physical structure of the algal community. Patterns of photosynthesis based on changes in dissolved oxygen and dissolved inorganic carbon concentrations (DIC) indicate that the flow speed effect is not the result of increased flux of oxygen from the algal turfs, and combined with the short response time to flow speed, suggest that DIC may limit rates of photosynthesis. Although there are differences between flow in the flume and flow over algal turfs on the reef, these results suggest that photosynthesis is controlled, at least in part, by mass transfer. The chemical engineering approach provides a framework to pose further testable hypotheses about how algal canopy height, flow oscillation, turbulence, and substratum roughness may modulate rates of metabolism of coral reef algal turfs.

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Acknowledgments

We are grateful to Dr. M. Atkinson for making facilities available at HIMB and for discussions on mass transfer processes on coral reefs. P. Ewanchuk, S. Longmore, A. Cheroske, R. Peachey, G. Lowe, B. Nyden and H. Carpenter assisted with data collection. We thank Dr. F. Thomas for assistance in the initial stages of the project, Dr. M. Okihiro for assistance with flowmeter sampling and analysis, and three reviewers whose comments improved the manuscript. This research was supported by grants from the Biological Oceanography Program at the National Science Foundation (OCE9314470 and OCE 0241885 [to RC] and OCE 9317733 [to SW]), a NIH MBRS (S06 GM48680) grant (to RC), and the University of Hawaii 1995 Pauley Summer Program. This is Contribution No. 129 from the CSUN Marine Biology Program and contribution number 2354 from the Bodega Marine Laboratory, University of California at Davis.

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Correspondence to Robert C. Carpenter.

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Communicated by O. Kinne, Oldendorf/Luhe.

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Carpenter, R.C., Williams, S.L. Mass transfer limitation of photosynthesis of coral reef algal turfs. Mar Biol 151, 435–450 (2007). https://doi.org/10.1007/s00227-006-0465-3

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