Abstract

Coral reef ecosystems thrive in tropical oligotrophic oceans because of the relationship between corals and endosymbiotic dinoflagellate algae called Symbiodinium. Symbiodinium convert sunlight and carbon dioxide into organic carbon and oxygen to fuel coral growth and calcification, creating habitat for these diverse and productive ecosystems. Light is thus a key regulating factor shaping the productivity, physiology, and ecology of the coral holobiont. Similar to all oxygenic photoautotrophs, Symbiodinium must safely harvest sunlight for photosynthesis and dissipate excess energy to prevent oxidative stress. Oxidative stress is caused by environmental stressors such as those associated with global climate change, and ultimately leads to breakdown of the coral–algal symbiosis known as coral bleaching. Recently, large-scale coral bleaching events have become pervasive and frequent threatening and endangering coral reefs. Because the coral–algal symbiosis is the biological engine producing the reef, the future of coral reef ecosystems depends on the ecophysiology of the symbiosis. This review examines the photobiology of the coral–algal symbiosis with particular focus on the photophysiological responses and timescales of corals and Symbiodinium. Additionally, this review summarizes the light environment and its dynamics, the vulnerability of the symbiosis to oxidative stress, the abiotic and biotic factors influencing photosynthesis, the diversity of the coral–algal symbiosis, and recent advances in the field. Studies integrating physiology with the developing “omics” fields will provide new insights into the coral–algal symbiosis. Greater physiological and ecological understanding of the coral–algal symbiosis is needed for protection and conservation of coral reefs.

Highlights

  • Coral reefs flourish as one of the world’s most diverse and productive ecosystems

  • Because of the central role of Symbiodinium photosynthesis as the engine of the coral reef ecosystem, this review summarizes the critical components and timescales of the photobiology of the coral–algal symbiosis and the underlying factors influencing the responses

  • This review aims to reach an audience that extends beyond photobiologists to all scientists and managers who work on coral reefs to provide them with a basic understanding of the important concepts, fundamental mechanisms and principal players in the photobiology of the coral–algal symbiosis

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Summary

INTRODUCTION

Coral reefs flourish as one of the world’s most diverse and productive ecosystems. Economic goods and ecosystem services of coral reefs are valued at over US $20 trillion annually (Costanza et al, 1997; de Groot et al, 2012). Coral reefs are a paradoxical ecosystem, “an oasis in a desert ocean” (Odum, 1971), in which corals build complex structures teeming with life in shallow, oligotrophic oceans (Figures 1A,B) This calcium carbonate bioconstruction, so extensive it is visible from outer space, is powered by the coral–algal symbiosis. Reef-building corals acclimate by reducing energetic requirements through decreasing tissue biomass, skeleton thickness, respiration rates, translocation, and growth (Anthony and Hoegh-Guldberg, 2003b). The most pronounced but consistent light cycle is the diurnal light cycle, in which Symbiodinium switches from producing oxygen via photosynthesis to consuming oxygen via respiration This switch causes the environment within coral cells to change from hyperoxic during the day to hypoxic during the night (Kühl et al, 1995), and was first observed within the tissues of symbiotic sea anemones (Dykens and Shick, 1982).

Adaptation Speciation
CP MAAs
Findings
Symbiodinium Symbiodinium
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