“…However, until recently the dependence of calcite growth rates on the solution stoichiometry has received limited attention (Tai et al, 2005;Nehrke et al, 2007;Perdikouri et al, 2009;Larsen et al, 2010;Stack and Grantham, 2010). This is remarkable given that (a) the compositions of most natural waters are highly non-stoichiometric with respect to calcium carbonate, and (b) a large body of work has shown that growth and dissolution rates of ionic minerals are markedly affected by the anion to cation concentration ratio in solution (Davies and Jones, 1955;Davies and Nancollas, 1955;Christoffersen and Christoffersen, 1979;Stubičar et al, 1990;Devenyns, 1990, 1992;Zhang and Nancollas, 1992;Burke and Nancollas, 1999;Rashkovich et al, 2006;Kowacz et al, 2007).…”