Article Synopsis

  • Documenting coral reef changes after bleaching helps us understand their resilience to climate change.
  • At Aldabra Atoll, coral loss was greater in deeper, seaward areas (51-62%) compared to lagoonal areas (34%), likely due to temperature variability.
  • While shallow reefs showed gradual recovery from 2016 to 2019, deeper reefs remained dominated by algae, indicating that full recovery could take over five years and may be threatened by future bleaching events.

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Article Abstract

Documenting post-bleaching trajectories of coral reef communities is crucial to understand their resilience to climate change. We investigated reef community changes following the 2015/16 bleaching event at Aldabra Atoll, where direct human impact is minimal. We combined benthic data collected pre- (2014) and post-bleaching (2016-2019) at 12 sites across three locations (lagoon, 2 m depth; seaward west and east, 5 and 15 m depth) with water temperature measurements. While seaward reefs experienced relative hard coral reductions of 51-62%, lagoonal coral loss was lower (- 34%), probably due to three-fold higher daily water temperature variability there. Between 2016 and 2019, hard coral cover did not change on deep reefs which remained dominated by turf algae and Halimeda, but absolute cover on shallow reefs increased annually by 1.3% (east), 2.3% (west) and 3.0% (lagoon), reaching, respectively, 54%, 68% and 93% of the pre-bleaching cover in 2019. Full recovery at the shallow seaward locations may take at least five more years, but remains uncertain for the deeper reefs. The expected increase in frequency and severity of coral bleaching events is likely to make even rapid recovery as observed in Aldabra's lagoon too slow to prevent long-term reef degradation, even at remote sites.

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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7550576PMC
http://dx.doi.org/10.1038/s41598-020-74077-xDOI Listing

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