Original Research ARTICLE
Species-specific coral calcification responses to the extreme environment of the southern Persian Gulf
- 1Center for Genomics and Systems Biology, New York University Abu Dhabi, United Arab Emirates
- 2Ecological Marine Services, Australia
- 3University of Copenhagen, National Museum of Natural History, Faculty of Natural and Life Sciences, University of Copenhagen, Denmark
- 4NOAA Coral Reef Watch, United States
- 5Marine Geophysical Laboratory, Physics Department, College of Science, Technology and Engineering, James Cook University, Australia
- 6ARC Centre of Excellence for Coral Reef Studies, James Cook University, Australia
- 7Experimental Marine Ecology Laboratory, Department of Biological Sciences, National University of Singapore, Singapore
Sustained accretion of calcium carbonate (mostly by scleractinian corals) is fundamental for maintaining the structure and function of coral reef ecosystems, but may be greatly constrained by extreme and rapidly changing environmental conditions. Corals in the southern Persian Gulf already experience extreme temperature ranges (<20C to >34C), chronic hypersalinity (>43 psu) and frequent light limitation (<100 μmol photons m-2 s-1). We compared annual rates of calcification for two of the most common massive coral species in the region (Platygyra daedalea and Cyphastrea microphthalma) along marked gradients in environmental conditions in the southern Persian Gulf and into the Oman Sea. Overall calcification rates were 32% higher in P. daedalea colonies (x̅ = 1.103 g cm-2 y-1, n = 46) than in C. microphthalma (x̅ = 0.835 g cm-2 y-1, n = 37), probably reflecting inter-specific differences in energy allocation and skeletal density. There was also considerable variation in calcification rates among individual colonies from the same locations that was unrelated to depth or photosymbiont type. However, most interestingly, P. daedalea and C. microphthalma exhibited contrasting trends in mean annual calcification rates across locations. For P. daedalea, calcification rates were lowest at Delma, where the minimum temperatures were lowest and salinity was highest, and increased across the southern Persian Gulf with increases in minimum temperatures and decreases in salinity. These data suggest that calcification rates of P. daedalea are most constrained by minimum temperatures, which is consistent with the strong relationship between annual calcification rates and minimum local temperatures recorded across the Indo-Pacific. Conversely, linear extension and calcification of C. microphthalma in the southern Persian Gulf was lowest at Ras Ghanada, where there was lowest light and highest maximum temperatures. These data reveal striking taxonomic differences in the specific environmental constraints on coral calcification, which will further reinforce changes in the structure of coral assemblages with ongoing global climate change.
Keywords: Coral calficication, Coral growth, extreme environments, Persian Gulf, Arabian Gulf, Gulf of Oman, Platygyra, Cyphastrea
Received: 30 Oct 2017;
Accepted: 06 Feb 2018.
Edited by:Jessica Carilli, University of Massachusetts Boston, United States
Reviewed by:Andrew A. Shantz, Pennsylvania State University, United States
Colleen B. Bove, University of North Carolina at Chapel Hill, United States
Copyright: © 2018 Howells, Dunshea, McParland, Vaughan, Heron, Pratchett, Burt and Bauman. 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) and the copyright owner 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: Dr. Emily J. Howells, New York University Abu Dhabi, Center for Genomics and Systems Biology, Abu Dhabi, United Arab Emirates, email@example.com