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Host-associated coral reef microbes respond to the cumulative pressures of ocean warming and ocean acidification
Webster, N.S.; Negri, A.P.; Botté, E.S.; Laffy, P.W.; Flores, F.; Noonan, S.; Schmidt, C.; Uthicke, S. (2016). Host-associated coral reef microbes respond to the cumulative pressures of ocean warming and ocean acidification. NPG Scientific Reports 6(19324): 9 pp. http://dx.doi.org/10.1038/srep19324
In: Scientific Reports (Nature Publishing Group). Nature Publishing Group: London. ISSN 2045-2322; e-ISSN 2045-2322
Peer reviewed article  
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  • Webster, N.S.
  • Negri, A.P.
  • Botté, E.S.
  • Laffy, P.W.
  • Flores, F.
  • Noonan, S.
  • Schmidt, C.
  • Uthicke, S.
Abstract
    Key calcifying reef taxa are currently threatened by thermal stress associated with elevated sea surface temperatures (SST) and reduced calcification linked to ocean acidification (OA). Here we undertook an 8 week experimental exposure to near-future climate change conditions and explored the microbiome response of the corals Acropora millepora and Seriatopora hystrix, the crustose coralline algae Hydrolithon onkodes, the foraminifera Marginopora vertebralis and Heterostegina depressa and the sea urchin Echinometra sp. Microbial communities of all taxa were tolerant of elevated pCO(2)/reduced pH, exhibiting stable microbial communities between pH 8.1 (pCO(2) 479-499 mu atm) and pH 7.9 (pCO(2) 738-835 mu atm). In contrast, microbial communities of the CCA and foraminifera were sensitive to elevated seawater temperature, with a significant microbial shift involving loss of specific taxa and appearance of novel microbial groups occurring between 28 and 31 degrees C. An interactive effect between stressors was also identified, with distinct communities developing under different pCO(2) conditions only evident at 31 degrees C. Microbiome analysis of key calcifying coral reef species under near-future climate conditions highlights the importance of assessing impacts from both increased SST and OA, as combinations of these global stressors can amplify microbial shifts which may have concomitant impacts for coral reef structure and function.
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