Numerous experiments have shown that ocean acidification impedes coral
calcification, but knowledge about in situ reef ecosystem response to ocean
acidification is still scarce. Bahía Culebra, situated at the northern
Pacific coast of Costa Rica, is a location naturally exposed to acidic
conditions due to the Papagayo seasonal upwelling. We measured pH and
pCO2 in situ during two non-upwelling seasons (June 2012,
May–June 2013), with a high temporal resolution of every 15 and 30 min,
respectively, using two Submersible Autonomous Moored Instruments (SAMI-pH,
SAMI-CO2). These results were compared with published data from the 2009
upwelling season. Findings revealed that the carbonate system in Bahía
Culebra shows a high temporal variability. Incoming offshore waters drive
intra- and interseasonal changes. Lowest pH (7.8) and highest pCO2
(658.3 µatm) values measured during a cold-water intrusion event in
the non-upwelling season were similar to those minimum values reported from
upwelling season (pH = 7.8, pCO2 = 643.5 µatm),
unveiling that natural acidification also occurs sporadically in the
non-upwelling season. This affects the interaction of photosynthesis,
respiration, calcification and carbonate dissolution and the resulting diel
cycle of pH and pCO2 in the reefs of Bahía Culebra. During
the non-upwelling season, the aragonite saturation state (Ωa)
rises to values of > 3.3 and during the upwelling season falls below
2.5. The Ωa threshold values for coral growth were derived from
the correlation between measured Ωa and coral linear
extension rates which were obtained from the literature and suggest that
future ocean acidification will threaten the continued growth of reefs in
Bahía Culebra. These data contribute to building a better understanding of
the carbonate system dynamics and coral reefs' key response (e.g., coral
growth) to natural low-pH conditions, in upwelling areas in the eastern
tropical Pacific and beyond
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