“…[6] Ge was confirmed (i)toi nduce the formation of octameric germanate ions (precursors of d4r units), (ii)to accelerate the crystallization of zeolites containing d4rs, and (iii)tostabilize such structures. [7] Several new germanosilicate zeolites with novel structures have been synthesized since BEC (ITQ-17) [8] was first prepared two decades ago,i ncluding the recently discovered SCM-14 (SOR) [9] and SCM-15 (SOV), [10] utilising the structure-directing effect of Ge.T he structure of an umber of germanosilicates synthesized thus far consists of silica parts, for example,layers,and mostly germanium-containing building blocks.I nz eolites UTL, IWW, UOV and SAZ-1, among others,silica layers are connected by d4r mostly composed of germanium ( Figure 1). Theformation of germanosilicates,the specificity of the distribution of Ge atoms in their lattice,and their potential for post-synthesis modification to new structures are discussed here from both experimental and theoretical points of view.…”