“…Once the island has fully crystallized and adopts the calcite structure, it does not grow further in height within the timescale of our experiments, which is consistent with expectation that the most stable surface of a given mineral (here the ð10 1 4Þ surface for calcite) grows the slowest. Non-classical pathways of crystallization via the formation of amorphous precursors have been reported, for example, for growth of biogenic calcite in the presence of a calcite seed crystal (Weiner et al, 2005;Politi et al, 2008;Killian et al, 2009), for calcite growth templated by self-assembled monolayers (Freeman et al, 2008;Pouget et al, 2009), and for homogeneous nucleation and growth of calcite in aqueous solutions (Gebauer et al, 2008;Meldrum and Sear, 2008;Raiteri and Gale, 2011). This idea is also supported by the Ostwald-Lussac law of phases, which states that the free energy barrier for nucleation leading to a more disordered state is less than the one leading to a more crystalline state (Nancollas, 1982).…”