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      Acclimatization to high-variance habitats does not enhance physiological tolerance of two key Caribbean corals to future temperature and pH

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          Abstract

          Corals are acclimatized to populate dynamic habitats that neighbour coral reefs. Habitats such as seagrass beds exhibit broad diel changes in temperature and pH that routinely expose corals to conditions predicted for reefs over the next 50–100 years. However, whether such acclimatization effectively enhances physiological tolerance to, and hence provides refuge against, future climate scenarios remains unknown. Also, whether corals living in low-variance habitats can tolerate present-day high-variance conditions remains untested. We experimentally examined how pH and temperature predicted for the year 2100 affects the growth and physiology of two dominant Caribbean corals ( Acropora palmata and Porites astreoides) native to habitats with intrinsically low (outer-reef terrace, LV) and/or high (neighbouring seagrass, HV) environmental variance. Under present-day temperature and pH, growth and metabolic rates (calcification, respiration and photosynthesis) were unchanged for HV versus LV populations. Superimposing future climate scenarios onto the HV and LV conditions did not result in any enhanced tolerance to colonies native to HV. Calcification rates were always lower for elevated temperature and/or reduced pH. Together, these results suggest that seagrass habitats may not serve as refugia against climate change if the magnitude of future temperature and pH changes is equivalent to neighbouring reef habitats.

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          Author and article information

          Journal
          Proc Biol Sci
          Proc. Biol. Sci
          RSPB
          royprsb
          Proceedings of the Royal Society B: Biological Sciences
          The Royal Society
          0962-8452
          1471-2954
          25 May 2016
          : 283
          : 1831
          : 20160442
          Affiliations
          [1 ] Coral Reef Research Unit, School of Biological Sciences, University of Essex , Colchester CO4 3SQ, UK
          [2 ] Climate Change Cluster (C3), University of Technology Sydney , PO Box 123, Broadway, New South Wales 2007, Australia
          [3 ] School of Mathematical and Physical Sciences, University of Technology Sydney , PO Box 123, Broadway, New South Wales 2007, Australia
          [4 ] Cooperative Institute for Marine and Atmospheric Studies, Rosenstiel School of Marine and Atmospheric Science, University of Miami , 4600 Rickenbacker Causeway, Miami, FL 33149, USA
          [5 ] Atlantic Oceanographic and Meteorological Laboratory (AOML), NOAA , 4301 Rickenbacker Causeway, Miami, FL 33149, USA
          Author notes
          Author information
          http://orcid.org/0000-0003-1962-1336
          Article
          PMC4892798 PMC4892798 4892798 rspb20160442
          10.1098/rspb.2016.0442
          4892798
          27194698
          05772374-103f-431a-9c64-9f3a0fcf2b75
          © 2016 The Author(s)

          Published by the Royal Society. All rights reserved.

          History
          : 2 March 2016
          : 22 April 2016
          Categories
          1001
          69
          15
          202
          Research Articles
          Custom metadata
          May 25, 2016

          thermal stress,climate change,coral reefs,ocean acidification,seagrass beds,environmental variance

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