The new mineral ammoniomathesiusite (IMA 2017-077), (NH 4 ) 5 (UO 2 ) 4 (SO 4 ) 4 (VO 5 )·4H 2 O, was found in the Burro mine, San Miguel County, Utah, USA, where it occurs as a secondary phase on asphaltum/quartz matrix in association with ammoniozippeite (2017-073), gypsum, jarosite and natrozippeite. The mineral forms pale yellow to greenish-yellow prisms, up to about 0.3 mm long, with pale yellow streak and bright yellow-green fluorescence. Crystals are transparent and have vitreous luster. The mineral is brittle, with Mohs hardness of 2½, stepped fracture and two cleavages: excellent on {110} and good on {001}. The calculated density is 3.672 g/cm 3 . Ammoniomathesiusite is optically uniaxial (-) with ω = 1.653(2) and ε = 1.609(2) (white light). Pleochroism is O green yellow, E colourless; O > E. Electron microprobe analyses yielded the empirical formula [(NH 4 ) 4.75 (U 1.00 O 2 ) 4 (S 1.00 O 4 ) 4 (V 1.00 O 5 )·4(H 2.07 O). The five strongest X-ray powder diffraction lines are [d obs Å(I)(hkl. Ammoniomathesiusite is tetragonal, P4/n, a = 14.9405(9), c = 7.1020(5) Å, V = 1585.3(2) Å 3 and Z = 2. The structure of ammoniomathesiusite (R 1 = 0.0218 for 3427 I > 2I) contains heteropolyhedral sheets based on [(UO 2 ) 4 (SO 4 ) 4 (VO 5 )] 5clusters. The structure is identical to that of mathesiusite, with NH 4 + in place of K + .