Corrigendum: Flow and Coral Morphology Control Coral Surface pH: Implications for the Effects of Ocean Acidification
Neil C. S. Chan
Daniel Wangpraseurt
Michael Kühl
Sean R. Connolly- 1Department of Marine Biology, College of Marine and Environmental Sciences, James Cook University, Townsville, QLD, Australia
- 2Department of Ocean Microbiology, Plant Functional Biology and Climate Change Cluster, University of Technology Sydney, Sydney, NSW, Australia
- 3Marine Biology Section, Department of Biology, University of Copenhagen, Helsingor, Denmark
- 4ARC Centre of Excellence for Coral Reef Studies, James Cook University, Townsville, QLD, Australia
A corrigendum on
Flow and Coral Morphology Control Coral Surface pH: Implications for the Effects of Ocean Acidification
by Chan, N. C. S., Wangpraseurt, D., Kühl, M., and Connolly, S. R. (2016). Front. Mar. Sci. 3:10. doi: 10.3389/fmars.2016.00010
In the original article there was a mistake in the units of the y axis and corresponding legend of Figure 1 as published. The correct version of Figure 1 appears below. The authors apologize for the mistake. This error does not change the scientific conclusions of the article in any way.
Figure 1. (A) DBL thickness (μm) vs. flow (cm s−1) for Favites (blue circles), Favites under acidified conditions (blue triangles) and P. damicornis (green circles). Symbols and error bars represent the mean ± 1.96*SE (n = 2–6). Lines represent the relationship between DBL thickness and flow from fitted power functions (blue solid—DBLFavites = 767 flow−0.738, blue dashed—DBLFavites acidified = 691 flow−0.399, green solid—DBLP.damicornis = 432 flow −0.99). (B) Net photosynthesis (μmol O2 cm−2 h−1) at various flows (cm s−1) for Favites (blue circles), Favites under acidified conditions (blue triangles) and P. damicornis (green circles). Symbols with error bars represent the mean ± 1.96*SE (n = 2–6).
Conflict of Interest Statement
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
Keywords: climate change, carbonate chemistry, calcification, diffusive boundary layer
Citation: Chan NCS, Wangpraseurt D, Kühl M and Connolly SR (2017) Corrigendum: Flow and Coral Morphology Control Coral Surface pH: Implications for the Effects of Ocean Acidification. Front. Mar. Sci. 4:226. doi: 10.3389/fmars.2017.00226
Received: 06 April 2017; Accepted: 06 July 2017;
Published: 25 July 2017.
Edited by:
Tamotsu Oomori, University of the Ryukyus, JapanReviewed by:
Sylvain Agostini, Shimoda Marine Research Center, JapanCopyright © 2017 Chan, Wangpraseurt, Kühl and Connolly. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
*Correspondence: Neil C. S. Chan, nchancs@gmail.com