Biogeosciences, 10, 6807-6814, 2013
www.biogeosciences.net/10/6807/2013/
doi:10.5194/bg-10-6807-2013
© Author(s) 2013. This work is distributed
under the Creative Commons Attribution 3.0 License.
Calcification responses of symbiotic and aposymbiotic corals to near-future levels of ocean acidification
S. Ohki1, T. Irie2, M. Inoue2, K. Shinmen2, H. Kawahata2, T. Nakamura3, A. Kato1, Y. Nojiri4, A. Suzuki5, K. Sakai1, and R. van Woesik6
1Sesoko Station, Tropical Biosphere Research Center, University of the Ryukyus, Motobu, Okinawa 905-0227, Japan
2Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Chiba 277-8564, Japan
3Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903-0213, Japan
4Center for Global Environmental Research, National Institute for Environmental Studies, Tsukuba, Ibaraki 305-8506, Japan
5Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba, Ibaraki 305-8567, Japan
6Department of Biological Sciences, Florida Institute of Technology, 150 West University Drive, Melbourne, Florida 32901, USA

Abstract. Increasing the acidity of ocean waters will directly threaten calcifying marine organisms such as reef-building scleractinian corals, and the myriad of species that rely on corals for protection and sustenance. Ocean pH has already decreased by around 0.1 pH units since the beginning of the industrial revolution, and is expected to decrease by another 0.2–0.4 pH units by 2100. This study mimicked the pre-industrial, present, and near-future levels of pCO2 using a precise control system (± 5% pCO2), to assess the impact of ocean acidification on the calcification of recently settled primary polyps of Acropora digitifera, both with and without symbionts, and adult fragments with symbionts. The increase in pCO2 of ~100 μatm between the pre-industrial period and the present had more effect on the calcification rate of adult A. digitifera than the anticipated future increases of several hundreds of micro-atmospheres of pCO2. The primary polyps with symbionts showed higher calcification rates than primary polyps without symbionts, suggesting that: (i) primary polyps housing symbionts are more tolerant to near-future ocean acidification than organisms without symbionts, and (ii) corals acquiring symbionts from the environment (i.e., broadcasting species) will be more vulnerable to ocean acidification than corals that maternally acquire symbionts.

Citation: Ohki, S., Irie, T., Inoue, M., Shinmen, K., Kawahata, H., Nakamura, T., Kato, A., Nojiri, Y., Suzuki, A., Sakai, K., and van Woesik, R.: Calcification responses of symbiotic and aposymbiotic corals to near-future levels of ocean acidification, Biogeosciences, 10, 6807-6814, doi:10.5194/bg-10-6807-2013, 2013.
 
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