Abstract

Coral reefs are declining worldwide as a result of many anthropogenic disturbances. This trend is alarming because coral reefs are hotspots of marine biodiversity and considered the ‘rainforests of the sea. As in the rainforest, much of the diversity on a coral reef is cryptic, remaining hidden among the cracks and crevices of structural taxa. Although the cryptofauna make up the majority of a reef’s metazoan biodiversity, we know little about their basic ecology or how these communities respond to reef degradation. Emerging research shows that the species richness of the motile cryptofauna is higher among dead (framework) vs. live coral substrates and, surprisingly, increases within successively more eroded reef framework structures, ultimately reaching a maximum in dead coral rubble. Consequently, the paradigm that abundant live coral is the apex of reef diversity needs to be clarified. This provides guarded optimism amidst alarming reports of declines in live coral cover and the impending doom of coral reefs, as motile cryptic biodiversity should persist independent of live coral cover. Granted, the maintenance of this high species richness is contingent on the presence of reef rubble, which will eventually be lost due to physical, chemical, and biological erosion if not replenished by live coral calcification and mortality. The trophic potential of a reef, as inferred from the abundance of cryptic organisms, is highest on live coral. Among dead framework substrates, however, the density of cryptofauna reaches a peak at intermediate levels of degradation. In summary, the response of the motile cryptofauna, and thus a large fraction of the reef’s biodiversity, to reef degradation is more complex and nuanced than currently thought; such that species richness may be less sensitive than overall trophic function.

Highlights

  • Coral reefs are in a state of decline due to climate change and overpopulation [1,2,3]

  • The 1997–1998 widespread mass coral bleaching event was reported to have caused the “loss” or “destruction” of 16% of the world’s coral reefs [16]. If we couple this estimate with the assumptions of the aforementioned calculations [14], this translates to a loss of 4,000 described coral reef species and a total loss of up to 40,000 species if one includes those both described and undescribed

  • The “loss” of 16% of coral reefs should be more accurately labeled the decline in percent live coral cover as it is clearly stated in Wilkinson [16] that this “loss” should be viewed as temporary, with the potential for recovery

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Summary

Introduction

Coral reefs are in a state of decline due to climate change and overpopulation [1,2,3]. If we couple this estimate with the assumptions of the aforementioned calculations [14], this translates to a loss of 4,000 described coral reef species and a total loss of up to 40,000 species if one includes those both described and undescribed Despite these alarming statistics, the “loss” of 16% of coral reefs should be more accurately labeled the decline in percent live coral cover as it is clearly stated in Wilkinson [16] that this “loss” should be viewed as temporary, with the potential for recovery. These declines in coral-dwelling species represent only a small fraction of the total number of organisms found on reefs

Evidence from Eastern Pacific Pocilloporid Reefs
Predicting Ecosystem Responses to Climate Change
Parallels with Forest Ecosystems
Findings
Conclusions

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