Based on the boron isotopic composition of coral from the southwestern Pacific, Pelejero et al. (Reports, 30 September 2005, p. 2204) suggested that natural variations in pH can modulate the impact of ocean acidification on coral reef ecosystems. We show that this claim cannot be reconciled with other marine carbon chemistry constraints and highlight problems with the authors’ interpretation of the paleontologic data.
Matear and McNeil, 2006. Comment on “Preindustrial to Modern Interdecadal Variability in Coral Reef pH”. Science 314(5799), 595b. [DOI: 10.1126/science.1128198]. Article.
