Species-Specific Coral Calcification Responses to the Extreme Environment of the Southern Persian Gulf

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 experienc...

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Main Authors: Emily J. Howells, Glenn Dunshea, Dain McParland, Grace O. Vaughan, Scott F. Heron, Morgan S. Pratchett, John A. Burt, Andrew G. Bauman
Format: Article
Language:English
Published: Frontiers Media S.A. 2018-02-01
Series:Frontiers in Marine Science
Subjects:
Online Access:http://journal.frontiersin.org/article/10.3389/fmars.2018.00056/full
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author Emily J. Howells
Glenn Dunshea
Glenn Dunshea
Dain McParland
Grace O. Vaughan
Scott F. Heron
Scott F. Heron
Morgan S. Pratchett
John A. Burt
Andrew G. Bauman
author_facet Emily J. Howells
Glenn Dunshea
Glenn Dunshea
Dain McParland
Grace O. Vaughan
Scott F. Heron
Scott F. Heron
Morgan S. Pratchett
John A. Burt
Andrew G. Bauman
author_sort Emily J. Howells
collection DOAJ
description 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 (<20 to >34°C), 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 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 (x = 1.103 g cm−2 y−1, n = 46) than in C. microphthalma (x = 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.
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spelling doaj.art-1c4f698025044836adae44db7db84b3a2022-12-22T01:11:37ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452018-02-01510.3389/fmars.2018.00056324051Species-Specific Coral Calcification Responses to the Extreme Environment of the Southern Persian GulfEmily J. Howells0Glenn Dunshea1Glenn Dunshea2Dain McParland3Grace O. Vaughan4Scott F. Heron5Scott F. Heron6Morgan S. Pratchett7John A. Burt8Andrew G. Bauman9Center for Genomics and Systems Biology, New York University Abu Dhabi, Abu Dhabi, United Arab EmiratesEcological Marine Services, Millbank, QLD, AustraliaNatural History Museum of Denmark, University of Copenhagen, Copenhagen, DenmarkCenter for Genomics and Systems Biology, New York University Abu Dhabi, Abu Dhabi, United Arab EmiratesCenter for Genomics and Systems Biology, New York University Abu Dhabi, Abu Dhabi, United Arab EmiratesNOAA/NESDIS/STAR Coral Reef Watch, College Park, MD, United StatesMarine Geophysical Laboratory, Physics Department, College of Science and Engineering, James Cook University, Townsville, QLD, AustraliaARC Centre of Excellence for Coral Reef Studies, James Cook University, Townsville, QLD, AustraliaCenter for Genomics and Systems Biology, New York University Abu Dhabi, Abu Dhabi, United Arab EmiratesExperimental Marine Ecology Laboratory, Department of Biological Sciences, National University of Singapore, Singapore, SingaporeSustained 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 (<20 to >34°C), 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 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 (x = 1.103 g cm−2 y−1, n = 46) than in C. microphthalma (x = 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.http://journal.frontiersin.org/article/10.3389/fmars.2018.00056/fullcoral growthcoral calcificationextreme environmentsPersian GulfArabian GulfGulf of Oman
spellingShingle Emily J. Howells
Glenn Dunshea
Glenn Dunshea
Dain McParland
Grace O. Vaughan
Scott F. Heron
Scott F. Heron
Morgan S. Pratchett
John A. Burt
Andrew G. Bauman
Species-Specific Coral Calcification Responses to the Extreme Environment of the Southern Persian Gulf
Frontiers in Marine Science
coral growth
coral calcification
extreme environments
Persian Gulf
Arabian Gulf
Gulf of Oman
title Species-Specific Coral Calcification Responses to the Extreme Environment of the Southern Persian Gulf
title_full Species-Specific Coral Calcification Responses to the Extreme Environment of the Southern Persian Gulf
title_fullStr Species-Specific Coral Calcification Responses to the Extreme Environment of the Southern Persian Gulf
title_full_unstemmed Species-Specific Coral Calcification Responses to the Extreme Environment of the Southern Persian Gulf
title_short Species-Specific Coral Calcification Responses to the Extreme Environment of the Southern Persian Gulf
title_sort species specific coral calcification responses to the extreme environment of the southern persian gulf
topic coral growth
coral calcification
extreme environments
Persian Gulf
Arabian Gulf
Gulf of Oman
url http://journal.frontiersin.org/article/10.3389/fmars.2018.00056/full
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