Calcification and organic production on a Hawaiian coral reef

By K. Shamberger, R. Feely, C. Sabine, Marlin J. Atkinson, E. H. Decarlo, F. Mackenzie, P. Drupp, D. Butterfield. 2011

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Ocean acidification and warming decrease calcification in the crustose coralline alga Hydrolithon onkodes and increase susceptibility to grazing (2012, background): “Due to seasonal effects on reef metabolism and calcification and the prolonged residence time of water in Kaneohe Bay (Fagan and Mackenzie, 2007; Lowe et al., 2009; Shamberger et al., 2011), ambient reef water was elevated naturally above the average global pCO2 of 388 μatm.”
Diverse coral communities in naturally acidified waters of a Western Pacific reef (2014, result): “As shown by previous studies [Gattuso et al., 1993; Silverman et al., 2007a, 2007b; Shamberger et al., 2011], diurnal extremes in reef carbonate chemistry occur 0–2 h after sunrise and before sunset.”
Macroalgae may mitigate ocean acidification effects on mussel calcification by increasing pH and its fluctuations (2018, background): “…cycles in, e.g., tide or rock pools (Truchot and Duhamel-Jouve 1980; Bjork et al. 2004; Beer et al. 2006; Wootton et al. 2008), coral reefs (Shamberger et al. 2011; Gray et al. 2012; Price et al. 2012; Smith et al. 2013), seagrass meadows (Invers et al. 1997; Semesi et al. 2009; Unsworth…”