4.7 Article

State of corals and coral reefs of the Galapagos Islands (Ecuador): Past, present and future

Journal

MARINE POLLUTION BULLETIN
Volume 133, Issue -, Pages 717-733

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.marpolbul.2018.06.002

Keywords

El Nino-Southern Oscillation; Echinoid bioerosion; Coral recovery; Coral loss; Caulerpa; Overfishing; Galapagos National Park

Funding

  1. U.S. National Geographic Society [9738-15]
  2. U.S. National Science Foundation [OCE-1447306, OCE-9314798]
  3. NSF RAPID grant through the ENSO [OCE-1447306]
  4. Khaled bin Sultan Living Oceans Foundation
  5. U.K.'s DEFRA Darwin Initiative [14-048]
  6. Conservation International (Puerto Ayora, Galapagos Islands)

Ask authors/readers for more resources

Coral populations and structural coral reefs have undergone severe reductions and losses respectively over large parts of the Galapagos Islands during and following the 1982-83 El Nino event. Coral tissue loss amounted to 95% across the Archipelago. Also at that time, all coral reefs in the central and southern islands disappeared following severe degradation and eventual collapse due primarily to intense bioerosion and low recruitment. Six sites in the southern islands have demonstrated low to moderate coral community (scattered colonies, but no carbonate framework) recovery. The iconic pocilloporid reef at Devil's Crown (Floreana Island) experienced recovery to 2007, then severe mortality during a La Nina cooling event, and is again (as of 2017) undergoing rapid recovery. Notable recovery has occurred at the central (Marchena) and northern islands (Darwin and Wolf). Of the 17 structural reefs first observed in the mid-1970s, the single surviving reef (Wellington Reef) at Darwin Island remains in a positive growth mode. The remainder either degraded to a coral community or was lost. Retrospective analyses of the age structure of corals killed in 1983, and isotopic signatures of the skeletal growth record of massive corals suggest the occurrence of robust coral populations during at least a 500-year period before 1983. The greatest potential threats to the recovery and persistence of coral reefs include: ocean warming and acidification, bioerosion, coral diseases, human population growth (increasing numbers of residents and tourists), overfishing, invasive species, pollution, and habitat destruction. Such a diverse spectrum of disturbances, acting alone or in combination, are expected to continue to cause local and archipelago-wide mortality and degradation of the coral reef ecosystem.

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