“…Repeatedly we can observe the evolution of similar morphologies in distantly related taxa, such as micropores in the siliceous components of choanoflagellates (Leadbeater, 2015), chrysophytes (Sandgren et al, 1996), diatoms (Finkel and Kotrc, 2010), and haptophytes (Yoshida et al, 2006); spines and spicules in radiolarians (Kunitomo et al, 2006), dictyochophytes (Preisig, 1994), centrohelids (Zlatogursky, 2016), and sponges (Weaver et al, 2007); or tablets and scales in haptophytes (Yoshida et al, 2006), rhizarians (Nomura and Ishida, 2016), synurophytes (Sandgren et al, 1996), amoebozoans (Lahr et al, 2013), and brachiopods (Williams et al, 2001). Though the genes governing the production of these silica patterns are not fully understood, many parallels with the molecular biology of diatom silicification are emerging, such as a role for glycoproteins in choanoflagellates (Gong et al, 2010) and synurophytes (Ludwig et al, 1996), cytoskeleton-mediated shaping of the growing silica structure in multiple taxa (Leadbeater, 2015;Nomura and Ishida, 2016) and the presence of post-translationally modified LCPAs in haptophyte (Durak et al, 2016) and sponge (Matsunaga et al, 2007) silica. These polymerization mechanisms have apparently evolved independently from those in diatoms, suggesting repeated recruitment of similar molecules for silica formation and patterning, and therefore a similar role for silicification-related evolutionary competition and speciation as diatoms.…”