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Responses of coral gastrovascular cavity pH during light and dark incubations to reduced seawater pH suggest species-specific responses to the effects of ocean acidification on calcification.

Authors :
Bove, Colleen B.
Whitehead, Robert F.
Szmant, Alina M.
Source :
Coral Reefs; 2020, Vol. 39 Issue 6, p1675-1691, 17p
Publication Year :
2020

Abstract

Coral polyps have a fluid-filled internal compartment, the gastrovascular cavity (GVC). Respiration and photosynthesis cause large daily excursions in GVC oxygen concentration (O<subscript>2</subscript>) and pH, but few studies have examined how this correlates with calcification rates. We hypothesized that GVC chemistry can mediate and ameliorate the effects of decreasing seawater pH (pH<subscript>SW</subscript>) on coral calcification. Microelectrodes were used to monitor O<subscript>2</subscript> and pH within the GVC of Montastraea cavernosa and Duncanopsammia axifuga (pH only) in both the light and the dark, and three pH<subscript>SW</subscript> levels (8.2, 7.9, and 7.6). At pH<subscript>SW</subscript> 8.2, GVC O<subscript>2</subscript> ranged from ca. 0 to over 400% saturation in the dark and light, respectively, with transitions from low to high (and vice versa) within minutes of turning the light on or off. For all three pH<subscript>SW</subscript> treatments and both species, pH<subscript>GVC</subscript> was always significantly above and below pH<subscript>SW</subscript> in the light and dark, respectively. For M. cavernosa in the light, pH<subscript>GVC</subscript> reached levels of pH 8.4–8.7 with no difference among pH<subscript>SW</subscript> treatments tested; in the dark, pH<subscript>GVC</subscript> dropped below pH<subscript>SW</subscript> and even below pH 7.0 in some trials at pH<subscript>SW</subscript> 7.6. For D. axifuga in both the light and the dark, pH<subscript>GVC</subscript> decreased linearly as pH<subscript>SW</subscript> decreased. Calcification rates were measured in the light concurrent with measurements of GVC O<subscript>2</subscript> and pH<subscript>GVC</subscript>. For both species, calcification rates were similar at pH<subscript>SW</subscript> 8.2 and 7.9 but were significantly lower at pH<subscript>SW</subscript> 7.6. Thus, for both species, calcification was protected from seawater acidification by intrinsic coral physiology at pH<subscript>SW</subscript> 7.9 but not 7.6. Calcification was not correlated with pH<subscript>GVC</subscript> for M. cavernosa but was for D. axifuga. These results highlight the diverse responses of corals to changes in pH<subscript>SW</subscript>, their varying abilities to control pH<subscript>GVC</subscript>, and consequently their susceptibility to ocean acidification. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
07224028
Volume :
39
Issue :
6
Database :
Complementary Index
Journal :
Coral Reefs
Publication Type :
Academic Journal
Accession number :
147104019
Full Text :
https://doi.org/10.1007/s00338-020-01995-7