Abstract
MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsTheme Sections MEPS 475:85-92 (2013) - DOI: https://doi.org/10.3354/meps10077 Temperature affects the early life history stages of corals more than near future ocean acidification Chia Miin Chua1,*, William Leggat1,2, Aurelie Moya1,3,4, Andrew H. Baird1 1ARC Centre of Excellence for Coral Reef Studies and 2School of Pharmacy and Molecular Sciences, James Cook University, Townsville, Queensland, 4811, Australia 3INSU-CNRS, Laboratoire d’Océanographie de Villefranche, B.P. 28, 06234 Villefranche-sur-mer Cedex, France 4UPMC University of Paris 06, Observatoire Océanologique de Villefranche, 06230 Villefranche-sur-mer, France *Email: chiamiin.chua@my.jcu.edu.au ABSTRACT: Climate change is projected to increase ocean temperatures by at least 2°C, and levels of pH by ~0.2 units (ocean acidification, OA) by the end of this century. While the effects of these stressors on marine organisms have been relatively well explored in isolation, possible interactions between temperature and OA have yet to be thoroughly investigated. OA at levels projected to occur within this century has few direct ecological effects on the early life history stages of corals. In contrast, temperature has pronounced effects on many stages in the early life history of corals. Here, we test whether temperature might act in combination with OA to produce a measurable ecological effect on fertilization, development, larval survivorship or metamorphosis of 2 broadcast spawning species, Acropora millepora and A. tenuis, from the Great Barrier Reef. We used 4 treatments: control, high temperature (+2°C), high partial pressure of CO2 (pCO2) (700 µatm) and a combination of high temperature and high pCO2, corresponding to the current levels of these variables and the projected values for the end of this century under the IPCC A2 scenario. We found no consistent effect of elevated pCO2 on fertilization, development, survivorship or metamorphosis, neither alone nor in combination with temperature. In contrast, a 2°C rise in temperature increased rates of development, but otherwise had no consistent effect on fertilization, survivorship or metamorphosis. We conclude that OA is unlikely to be a direct threat to the early life history stages of corals, at least in the near future. In contrast, rising sea temperatures are likely to affect coral population dynamics by increasing the rate of larval development with resulting changes in patterns of connectivity. KEY WORDS: Coral reefs · Climate change · Connectivity · Development · Larval ecology · Survivorship · Settlement Full text in pdf format PreviousNextCite this article as: Chua CM, Leggat W, Moya A, Baird AH (2013) Temperature affects the early life history stages of corals more than near future ocean acidification. Mar Ecol Prog Ser 475:85-92. https://doi.org/10.3354/meps10077 Export citation RSS - Facebook - Tweet - linkedIn Cited by Published in MEPS Vol. 475. Online publication date: February 14, 2013 Print ISSN: 0171-8630; Online ISSN: 1616-1599 Copyright © 2013 Inter-Research.
Highlights
Increasing carbon dioxide (CO2) concentrations in the atmosphere are causing the oceans to warm
We found no consistent effect of elevated pressure of CO2 (pCO2) on fertilization, development, survivorship or metamorphosis, neither alone nor in combination with temperature
Rates of development were faster at high temperature, as predicted by metabolic theory (Gillooly et al 2001)
Summary
Increasing carbon dioxide (CO2) concentrations in the atmosphere are causing the oceans to warm. Sea surface temperatures have risen by a global average of 0.7°C since the industrial revolution (Feely et al 2009) and are predicted to rise by a further 2 to 3°C by the end of the century under the IPCC A2 scenario (Bindoff et al 2007). The effects of rising sea surface temperature on marine organisms are well documented. Symbiotic organisms, such as corals, seem sensitive to elevated temperatures (Baird et al 2009), and the resulting coral bleaching has a range of ecological effects from reductions in growth, reproduction and competitive ability to high mortality of individuals over large spatial scales (see review in McClanahan et al 2009).
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