“…Previous studies suggested that the prismatic shapes of travertine calcite crystals are related to crystalline lattice and growth morphologies being affected by impurities, concentrations of Mg, phosphate or sulphate, high fluid supersaturation with respect to carbonates, and presence of microbial biofilms (Folk et al, 1985; Folk, 1993, 1994; Tracy et al, 1998; Bosak and Newman, 2005; Di Benedetto et al, 2011; Jones and Peng, 2014a; Jones, 2017a). Numerous experimental studies on the precipitation of carbonate crystals confirm that crystal morphology is influenced by the presence of impurities, hydrogels, polymers and various organic molecules (Gower and Tirrell, 1998; Falini et al, 2000; Meldrum and Hyde, 2001; Kato et al, 2002; Cölfen, 2003; Oaki and Imai, 2003; Chekroun et al, 2004; Tong et al, 2004; Bosak and Newman, 2005; Sand et al, 2011; Keller and Plank, 2013; Tobler et al, 2014; Kosanović et al, 2017). Konopacka-Lyskawa et al (2017) showed that calcite crystal morphology changes from scalenohedral to rhombo-scalenohedral elongated crystals and crystal size decreases at increasing organic compound concentrations.…”