Large scale patterns of antimicrofouling defenses in the hard coral Pocillopora verrucosa in an environmental gradient along the Saudi Arabian coast of the Red Sea

PLoS One. 2014 Dec 8;9(12):e106573. doi: 10.1371/journal.pone.0106573. eCollection 2014.

Abstract

Large scale patterns of ecologically relevant traits may help identify drivers of their variability and conditions beneficial or adverse to the expression of these traits. Antimicrofouling defenses in scleractinian corals regulate the establishment of the associated biofilm as well as the risks of infection. The Saudi Arabian Red Sea coast features a pronounced thermal and nutritional gradient including regions and seasons with potentially stressful conditions to corals. Assessing the patterns of antimicrofouling defenses across the Red Sea may hint at the susceptibility of corals to global change. We investigated microfouling pressure as well as the relative strength of 2 alternative antimicrofouling defenses (chemical antisettlement activity, mucus release) along the pronounced environmental gradient along the Saudi Arabian Red Sea coast in 2 successive years. Microfouling pressure was exceptionally low along most of the coast but sharply increased at the southernmost sites. Mucus release correlated with temperature. Chemical defense tended to anti-correlate with mucus release. As a result, the combined action of mucus release and chemical antimicrofouling defense seemed to warrant sufficient defense against microbes along the entire coast. In the future, however, we expect enhanced energetic strain on corals when warming and/or eutrophication lead to higher bacterial fouling pressure and a shift towards putatively more costly defense by mucus release.

Publication types

  • Research Support, Non-U.S. Gov't

MeSH terms

  • Animals
  • Anthozoa / microbiology*
  • Anthozoa / physiology*
  • Disease Resistance*
  • Environment*
  • Indian Ocean
  • Oceanography
  • Saudi Arabia

Grants and funding

This collaboration of the Jeddah Transect Project between King Abdulaziz University (KAU) and Helmholtz-Center for Ocean Research GEOMAR was funded by KAU, Jeddah, Saudi Arabia, under grant no. T-065/430-DSR. Further support was given by GEOMAR and King Abdullah University for Science. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.