Calcification, a physiological process to be considered in the context of the whole organism

H. S. Findlay, H. L. Wood, M. A. Kendall, J. I. Spicer, R. J. Twitchett, S. Widdicombe
2009 Biogeosciences Discussions  
Marine organisms that produce calcium carbonate structures are predicted to be most vulnerable to a decline in oceanic pH (ocean acidification) based on the understanding that calcification rates will decrease as a result of changes in the seawater carbonate chemistry thereby reducing carbonate ion concentration (and associated satura-5 10
doi:10.5194/bgd-6-2267-2009 fatcat:wr2iyrpwlfgpbbfia7kxdusvnq