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...

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Published in:Frontiers in Marine Science
Main Authors: Neil C. S. Chan, Daniel eWangpraseurt, Michael eKühl, Sean eConnolly
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2016
Subjects:
pH
CO2
Q
Online Access:https://doi.org/10.3389/fmars.2016.00010
https://doaj.org/article/87888e78bb9943d081c93e899409e6eb
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spelling ftdoajarticles:oai:doaj.org/article:87888e78bb9943d081c93e899409e6eb 2023-05-15T17:49:48+02:00 Flow and coral morphology control coral surface pH: Implications for the effects of ocean acidification Neil C. S. Chan Daniel eWangpraseurt Michael eKühl Sean eConnolly 2016-02-01T00:00:00Z https://doi.org/10.3389/fmars.2016.00010 https://doaj.org/article/87888e78bb9943d081c93e899409e6eb EN eng Frontiers Media S.A. http://journal.frontiersin.org/Journal/10.3389/fmars.2016.00010/full https://doaj.org/toc/2296-7745 2296-7745 doi:10.3389/fmars.2016.00010 https://doaj.org/article/87888e78bb9943d081c93e899409e6eb Frontiers in Marine Science, Vol 3 (2016) Climate Change pH ocean acidification CO2 coral reefs Coral calcification Science Q General. Including nature conservation geographical distribution QH1-199.5 article 2016 ftdoajarticles https://doi.org/10.3389/fmars.2016.00010 2022-12-31T06:22:34Z 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 modelling 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 Directory of Open Access Journals: DOAJ Articles Frontiers in Marine Science 3
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Climate Change
pH
ocean acidification
CO2
coral reefs
Coral calcification
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
spellingShingle Climate Change
pH
ocean acidification
CO2
coral reefs
Coral calcification
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
Neil C. S. Chan
Daniel eWangpraseurt
Michael eKühl
Sean eConnolly
Flow and coral morphology control coral surface pH: Implications for the effects of ocean acidification
topic_facet Climate Change
pH
ocean acidification
CO2
coral reefs
Coral calcification
Science
Q
General. Including nature conservation
geographical distribution
QH1-199.5
description 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 modelling 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 Neil C. S. Chan
Daniel eWangpraseurt
Michael eKühl
Sean eConnolly
author_facet Neil C. S. Chan
Daniel eWangpraseurt
Michael eKühl
Sean eConnolly
author_sort Neil C. S. Chan
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 Media S.A.
publishDate 2016
url https://doi.org/10.3389/fmars.2016.00010
https://doaj.org/article/87888e78bb9943d081c93e899409e6eb
genre Ocean acidification
genre_facet Ocean acidification
op_source Frontiers in Marine Science, Vol 3 (2016)
op_relation http://journal.frontiersin.org/Journal/10.3389/fmars.2016.00010/full
https://doaj.org/toc/2296-7745
2296-7745
doi:10.3389/fmars.2016.00010
https://doaj.org/article/87888e78bb9943d081c93e899409e6eb
op_doi https://doi.org/10.3389/fmars.2016.00010
container_title Frontiers in Marine Science
container_volume 3
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