Coral Reefs

, Volume 32, Issue 3, pp 727–735

Calcification by juvenile corals under heterotrophy and elevated CO2


DOI: 10.1007/s00338-013-1021-5

Cite this article as:
Drenkard, E.J., Cohen, A.L., McCorkle, D.C. et al. Coral Reefs (2013) 32: 727. doi:10.1007/s00338-013-1021-5


Ocean acidification (OA) threatens the existence of coral reefs by slowing the rate of calcium carbonate (CaCO3) production of framework-building corals thus reducing the amount of CaCO3 the reef can produce to counteract natural dissolution. Some evidence exists to suggest that elevated levels of dissolved inorganic nutrients can reduce the impact of OA on coral calcification. Here, we investigated the potential for enhanced energetic status of juvenile corals, achieved via heterotrophic feeding, to modulate the negative impact of OA on calcification. Larvae of the common Atlantic golf ball coral, Favia fragum, were collected and reared for 3 weeks under ambient (421 μatm) or significantly elevated (1,311 μatm) CO2 conditions. The metamorphosed, zooxanthellate spat were either fed brine shrimp (i.e., received nutrition from photosynthesis plus heterotrophy) or not fed (i.e., primarily autotrophic). Regardless of CO2 condition, the skeletons of fed corals exhibited accelerated development of septal cycles and were larger than those of unfed corals. At each CO2 level, fed corals accreted more CaCO3 than unfed corals, and fed corals reared under 1,311 μatm CO2 accreted as much CaCO3 as unfed corals reared under ambient CO2. However, feeding did not alter the sensitivity of calcification to increased CO2; ∆ calcification/∆Ω was comparable for fed and unfed corals. Our results suggest that calcification rates of nutritionally replete juvenile corals will decline as OA intensifies over the course of this century. Critically, however, such corals could maintain higher rates of skeletal growth and CaCO3 production under OA than those in nutritionally limited environments.


Climate change Ocean acidification Coral reefs Coral calcification Heterotrophy Energetics 

Supplementary material

338_2013_1021_MOESM1_ESM.docx (122 kb)
Supplementary material 1 (DOCX 121 kb)

Copyright information

© Springer-Verlag Berlin Heidelberg 2013

Authors and Affiliations

  • E. J. Drenkard
    • 1
    • 5
  • A. L. Cohen
    • 2
    • 6
  • D. C. McCorkle
    • 2
  • S. J. de Putron
    • 3
  • V. R. Starczak
    • 2
  • A. E. Zicht
    • 4
    • 7
  1. 1.Woods Hole Oceanographic Institution Joint Program in OceanographyMassachusetts Institute of TechnologyCambridgeUSA
  2. 2.Woods Hole Oceanographic InstitutionWoods HoleUSA
  3. 3.Bermuda Institute of Ocean SciencesSt. George’sBermuda
  4. 4.Oberlin CollegeOberlinUSA
  5. 5.Woods HoleUSA
  6. 6.Woods HoleUSA
  7. 7.Rutgers University Institute of Marine and Coastal SciencesNew BrunswickUSA

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