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
Coral polyps have a fluid-filled internal compartment, the gastrovascular cavity (GVC). Respiration and photosynthesis cause large daily excursions in GVC oxygen concentration (O 2 ) and pH, but few studies have examined how this correlates with calcification rates. We hypothesized that GVC chemistr...
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Veröffentlicht in: | Coral reefs 2020-12, Vol.39 (6), p.1675-1691 |
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Zusammenfassung: | Coral polyps have a fluid-filled internal compartment, the gastrovascular cavity (GVC). Respiration and photosynthesis cause large daily excursions in GVC oxygen concentration (O
2
) 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
SW
) on coral calcification. Microelectrodes were used to monitor O
2
and pH within the GVC of
Montastraea cavernosa
and
Duncanopsammia axifuga
(pH only) in both the light and the dark, and three pH
SW
levels (8.2, 7.9, and 7.6). At pH
SW
8.2, GVC O
2
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
SW
treatments and both species, pH
GVC
was always significantly above and below pH
SW
in the light and dark, respectively. For
M. cavernosa
in the light, pH
GVC
reached levels of pH 8.4–8.7 with no difference among pH
SW
treatments tested; in the dark, pH
GVC
dropped below pH
SW
and even below pH 7.0 in some trials at pH
SW
7.6. For
D. axifuga
in both the light and the dark, pH
GVC
decreased linearly as pH
SW
decreased. Calcification rates were measured in the light concurrent with measurements of GVC O
2
and pH
GVC
. For both species, calcification rates were similar at pH
SW
8.2 and 7.9 but were significantly lower at pH
SW
7.6. Thus, for both species, calcification was protected from seawater acidification by intrinsic coral physiology at pH
SW
7.9 but not 7.6. Calcification was not correlated with pH
GVC
for
M. cavernosa
but was for
D. axifuga.
These results highlight the diverse responses of corals to changes in pH
SW
, their varying abilities to control pH
GVC
, and consequently their susceptibility to ocean acidification. |
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ISSN: | 0722-4028 1432-0975 |
DOI: | 10.1007/s00338-020-01995-7 |