Physicochemical Control of Caribbean Coral Calcification Linked to Host and Symbiont Responses to Varying <i>p</i>CO<sub>2</sub> and Temperature
2022
Robert A. Eagle | Maxence Guillermic | Illian De Corte | Blanca Alvarez Caraveo | Colleen B. Bove | Sambuddha Misra | Louise P. Cameron | Karl D. Castillo | Justin B. Ries
It is thought that the active physiological regulation of the chemistry of a parent fluid is an important process in the biomineralization of scleractinian corals. Biological regulation of calcification fluid pH (pH<sub>CF</sub>) and other carbonate chemistry parameters ([CO<sub>3</sub><sup>2−</sup>]<sub>CF</sub>, DIC<sub>CF</sub>, and Ω<sub>CF</sub>) may be challenged by CO<sub>2</sub> driven acidification and temperature. Here, we examine the combined influence of changing temperature and CO<sub>2</sub> on calcifying fluid regulation in four common Caribbean coral species—<i>Porites astreoides</i>, <i>Pseudodiploria strigosa</i>, <i>Undaria tenuifolia</i>, and <i>Siderastrea siderea</i>. We utilize skeletal boron geochemistry (B/Ca and δ<sup>11</sup>B) to probe the pH<sub>CF</sub>, [CO<sub>3</sub><sup>2−</sup>]<sub>CF</sub>, and DIC<sub>CF</sub> regulation in these corals, and δ<sup>13</sup>C to track changes in the sources of carbon for calcification. Temperature was found to not influence pH<sub>CF</sub> regulation across all <i>p</i>CO<sub>2</sub> treatments in these corals, in contrast to recent studies on Indo-Pacific pocilloporid corals. We find that [DIC]<sub>CF</sub> is significantly lower at higher temperatures in all the corals, and that the higher temperature was associated with depletion of host energy reserves, suggesting [DIC]<sub>CF</sub> reductions may result from reduced input of respired CO<sub>2</sub> to the DIC pool for calcification. In addition, δ<sup>13</sup>C data suggest that under high temperature and CO<sub>2</sub> conditions, algal symbiont photosynthesis continues to influence the calcification pool and is associated with low [DIC]<sub>CF</sub> in <i>P. strigosa</i> and <i>P. astreoides</i>. In <i>P. astreoides</i> this effect is also associated with an increase in chlorophyll a concentration in coral tissues at higher temperatures. These observations collectively support the assertion that physicochemical control over coral calcifying fluid chemistry is coupled to host and symbiont physiological responses to environmental change, and reveals interspecific differences in the extent and nature of this coupling.
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