University of Exeter researchers are investigating "reef carbonate budgets" – the net production or erosion of reef structure over time.
To study the impacts of climate change on reef functions, they examined 12 reefs in the remote Chagos Islands in the Indian Ocean before and after the global coral bleaching event in 2015/16.
In 2018, the formerly thriving reefs were “shrinking”, with coral cover and carbonate production down by more than 70% and erosion processes exceeding new coral growth.
When the researchers returned in 2021, all reefs were on a trajectory of recovery, although the speed varied from place to place.
Where key coral species returned quickly and the underlying physical reef structure had stayed intact, reefs showed a rapid transition back to positive growth only six years after the bleaching event.
Bleaching is caused by warmer water temperatures, which can trigger corals to expel their symbiotic algae and turn white. Corals can survive this, but an extreme heat wave causes large-scale mortality.
The speed of subsequent recovery is an important indicator of a reef’s health and resilience.
"Such high rates of coral recruitment and the rapid restoration of reef functions are a very nice surprise and imply that this location is showing some resilience, thus far, to ongoing ocean warming," said lead author Dr Ines Lange, a postdoctoral research fellow in a multi-institutional project funded by the Bertarelli Program in Marine Science.
Read more at: University of Exeter
A recovering reef in the Chagos Archipelago six years after the bleaching event (Photo Credit: Dr Ines Lange)