Abstract

Coral reef decline persists as a global issue with ties to climate change and human footprint. The SeaFlower Biosphere reserve includes some of the most isolated oceanic coral reefs in the Southwestern Caribbean, which provide natural experiments to test global and/or basin-wide factors affecting coral reefs. In this study, we compared coral and other substrate cover (algae, cyanobacteria and octocorals), along population densities of keystone urchin species from two atolls (Serrana and Roncador Banks), during 1995, 2003 and 2015/2016. We also surveyed benthic foraminifera as a water quality proxy for coral growth in the last period. A steady reduction in coral cover was clearly observed at Roncador`s lagoon, but not at Serrana`s reefs, with significant differences between 1995 and 2015/2016. Percent cover of fleshy algae decreased significantly also at Roncador between 1995 and 2003 but did not change notably from 1995 to 2016 at Serrana. However, both Banks exhibited a loss in crustose coralline algae from 2003 to 2015/16. Likewise, a reduction in bottom complexity, measured as bottom rugosity, was evident between 1995 and 2003. Roncador Bank had unprecedented high octocoral densities, which increased almost threefold from 2003 to 2015. In contrast, urchin densities were low in Roncador; only Diadema antillarum increased from 2003-2016 in Serrana Bank. The FORAM Index (FI) in the two Banks was below the range expected for healthy coral reefs. Although both Banks follow a reduction in CCA and CA cover, Roncador Bank also faces an alarming decline in coral cover, urchins and bottom complexity (rugosity) in contrast to increases in octocoral densities and potential loss of resilience and eutrophication suggested by the FI index. These unexpected findings led us to consider and discuss potential outcomes, where these reefs deteriorate (i.e., erode and drown) providing ideal conditions for octocoral growth. Hence, it is of utmost urgency to start monitoring reef budgets, octocorals and nutrient sources.

Highlights

  • Marine biodiversity reaches its highest complexity in coral reefs

  • Roncador Bank mid-water reefs experienced a mean decline in crustose coralline algae (CCA) (10.13%) and fleshy algae (FA) (53.41%), but not hard coral (HC) (22.58%), from 1995 to 2015 (CCA: 2.15%, FA: 28.88%, HC: 9.85% )

  • HC cover at this Bank decrease from 22.6% in 1995 to 14.9% in 2003, and to 9.9% during 2016; a continuous reduction in HC cover of 12.7% over 20 years

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Summary

Introduction

Marine biodiversity reaches its highest complexity in coral reefs. These formidable tropical ecosystems account for at least 30% of marine biodiversity at an extent of less than 1% of the planet’s surface (Roberts et al, 2002). The increase of atmospheric carbon dioxide (CO2) concentration alters seawater chemistry leading to ocean acidification, which includes adverse effects on the calcification rates of marine organisms including corals (Orr et al, 2005; Hoegh-Guldberg et al, 2007). These processes act in synergy with the human footprint, increasing sewage and overexploitation, which reduces the resilience of marine ecosystems like coral reefs (Mumby, 2009; Graham et al, 2013; Wiedenmann et al, 2013). Failure to protect coral reefs will affect millions of livelihoods worldwide and provoke unparalleled rapid biodiversity losses in the years to come

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