Flow and coral morphology control coral surface pH: implications for the effects of ocean acidification
The future impact of ocean acidification (OA) on corals is disputed in part because mathematical models used to predict these impacts do not seem to capture, or offer a framework to adequately explain, the substantial variability in acidification effects observed in empirical studies. The build-up o...
Published in: | Frontiers in Marine Science |
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Online Access: | https://researchonline.jcu.edu.au/47812/1/ChanEtAl_Frontiers2016.pdf |
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ftjamescook:oai:researchonline.jcu.edu.au:47812 2024-02-11T10:07:24+01:00 Flow and coral morphology control coral surface pH: implications for the effects of ocean acidification Chan, Neil C.S. Wangpraseurt, Daniel Kuhl, Michael Connolly, Sean R. 2016 application/pdf https://researchonline.jcu.edu.au/47812/1/ChanEtAl_Frontiers2016.pdf unknown Frontiers Research Foundation http://dx.doi.org/10.3389/fmars.2016.00010 https://researchonline.jcu.edu.au/47812/ https://researchonline.jcu.edu.au/47812/1/ChanEtAl_Frontiers2016.pdf Chan, Neil C.S., Wangpraseurt, Daniel, Kuhl, Michael, and Connolly, Sean R. (2016) Flow and coral morphology control coral surface pH: implications for the effects of ocean acidification. Frontiers in Marine Science, 26. pp. 637-641. open Article PeerReviewed 2016 ftjamescook https://doi.org/10.3389/fmars.2016.00010 2024-01-15T23:40:57Z The future impact of ocean acidification (OA) on corals is disputed in part because mathematical models used to predict these impacts do not seem to capture, or offer a framework to adequately explain, the substantial variability in acidification effects observed in empirical studies. The build-up of a diffusive boundary layer (DBL), wherein solute transport is controlled by diffusion, can lead to pronounced differences between the bulk seawater pH, and the actual pH experienced by the organism, a factor rarely considered in mathematical modeling of ocean acidification effects on corals. In the present study, we developed a simple diffusion-reaction-uptake model that was experimentally parameterized based on direct microsensor measurements of coral tissue pH and O2 within the DBL of a branching and a massive coral. The model accurately predicts tissue surface pH for different coral morphologies and under different flow velocities as a function of ambient pH. We show that, for all cases, tissue surface pH is elevated at lower flows, and thus thicker DBLs. The relative effects of OA on coral surface pH was controlled by flow and we show that under low flow velocities tissue surface pH under OA conditions (pHSWS = 7.8) can be equal to the pH under normal conditions (pHSWS = 8.2). We conclude that OA effects on corals in nature will be complex as the degree to which they are controlled by flow appears to be species specific. Article in Journal/Newspaper Ocean acidification James Cook University, Australia: ResearchOnline@JCU Frontiers in Marine Science 3 |
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James Cook University, Australia: ResearchOnline@JCU |
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The future impact of ocean acidification (OA) on corals is disputed in part because mathematical models used to predict these impacts do not seem to capture, or offer a framework to adequately explain, the substantial variability in acidification effects observed in empirical studies. The build-up of a diffusive boundary layer (DBL), wherein solute transport is controlled by diffusion, can lead to pronounced differences between the bulk seawater pH, and the actual pH experienced by the organism, a factor rarely considered in mathematical modeling of ocean acidification effects on corals. In the present study, we developed a simple diffusion-reaction-uptake model that was experimentally parameterized based on direct microsensor measurements of coral tissue pH and O2 within the DBL of a branching and a massive coral. The model accurately predicts tissue surface pH for different coral morphologies and under different flow velocities as a function of ambient pH. We show that, for all cases, tissue surface pH is elevated at lower flows, and thus thicker DBLs. The relative effects of OA on coral surface pH was controlled by flow and we show that under low flow velocities tissue surface pH under OA conditions (pHSWS = 7.8) can be equal to the pH under normal conditions (pHSWS = 8.2). We conclude that OA effects on corals in nature will be complex as the degree to which they are controlled by flow appears to be species specific. |
format |
Article in Journal/Newspaper |
author |
Chan, Neil C.S. Wangpraseurt, Daniel Kuhl, Michael Connolly, Sean R. |
spellingShingle |
Chan, Neil C.S. Wangpraseurt, Daniel Kuhl, Michael Connolly, Sean R. Flow and coral morphology control coral surface pH: implications for the effects of ocean acidification |
author_facet |
Chan, Neil C.S. Wangpraseurt, Daniel Kuhl, Michael Connolly, Sean R. |
author_sort |
Chan, Neil C.S. |
title |
Flow and coral morphology control coral surface pH: implications for the effects of ocean acidification |
title_short |
Flow and coral morphology control coral surface pH: implications for the effects of ocean acidification |
title_full |
Flow and coral morphology control coral surface pH: implications for the effects of ocean acidification |
title_fullStr |
Flow and coral morphology control coral surface pH: implications for the effects of ocean acidification |
title_full_unstemmed |
Flow and coral morphology control coral surface pH: implications for the effects of ocean acidification |
title_sort |
flow and coral morphology control coral surface ph: implications for the effects of ocean acidification |
publisher |
Frontiers Research Foundation |
publishDate |
2016 |
url |
https://researchonline.jcu.edu.au/47812/1/ChanEtAl_Frontiers2016.pdf |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
http://dx.doi.org/10.3389/fmars.2016.00010 https://researchonline.jcu.edu.au/47812/ https://researchonline.jcu.edu.au/47812/1/ChanEtAl_Frontiers2016.pdf Chan, Neil C.S., Wangpraseurt, Daniel, Kuhl, Michael, and Connolly, Sean R. (2016) Flow and coral morphology control coral surface pH: implications for the effects of ocean acidification. Frontiers in Marine Science, 26. pp. 637-641. |
op_rights |
open |
op_doi |
https://doi.org/10.3389/fmars.2016.00010 |
container_title |
Frontiers in Marine Science |
container_volume |
3 |
_version_ |
1790605962143334400 |