“…It is interesting that the VT family had a higher porosity (see Methods, Computer-based calculations and simulations for detailed calculation) than zeolites (Supplementary Table 19), and most of them had over 50% porosity, which was higher than 90% of zeolites, including some widely used zeolites, such as FAU (46.86%), LTA (43.79%), MWW (42.05%), MOR (38.23%), and MFI (31.34%). There are also molecular type VT s, such as V(dien)) 4 [W 2 O 14 ] and V(dien)) 4 [W 4 O 20 ] (dien = diethylenetriamine, C 4 H 13 N 3 ) 30 , and V(dien)) 4 [W 4 O 20 ] is also composed of cubane unit and V ions. Formation energies (Δ H f ) of the zeolitic VT s are lower than those of the molecular type VT s (Supplementary Fig.…”