Neustädtelite and cobaltneustädtelite, two new minerals related to medenbachite, were found on samples from the dumps of the Güldener Falk mine near Schneeberg-Neustädtel, Saxony, Germany. The general appearance of the two new minerals is very similar: small tabular crystals up to 0.2 mm in diameter, transparent to translucent, with a brown color and a light brown streak; the lustre is adamantine. Both minerals are optically biaxial negative, 2V = 65(5)°, n x = 2.02(2), n y = 2.09 (calc.), n z = 2.12(2); pleochroism is strong with X = brown to opaque, Y = yellow, Z = pale yellow. Mohs’ hardness is 4.5. The cleavage parallel to {001} is good. The chemical compositions were derived by means of electron-microprobe analyses. Average contents for neustädtelite/cobaltneustädtelite are (in wt%): Bi 2 O 3 52.58/51.54, PbO 0.08/0.08, CaO 0.15/0.32, Fe 2 O 3 13.92/10.90, Al 2 O 3 0.29/0.07, CoO 3.35/5.47, NiO 0.34/1.61, ZnO 0.09/0.39, CuO 0.07/0.00, As 2 O 5 26.82/25.91, P 2 O 5 0.23/0.43, H 2 O (calc.) 2.56/3.01, total 100.48/99.73. Mössbauer spectra of cobaltneustädtelite and medenbachite confirmed that all of the iron is trivalent. Based on 12 O atoms, the empirical formulae for the neustädtelite and cobaltneustädtelite type materials are (Bi 1.94 Ca 0.02 ) ∑1.96 Fe 1.00 (Fe 0.50 Co 0.38 Ni 0.04 Al 0.05 Zn 0.01 Cu 0.01 ) ∑0.99 [(OH) 2.44 O 1.40 ] ∑3.84 [(AsO 4 ) 2.01 (PO 4 ) 0.03 ] ∑2.04 and (Bi 1.91 Ca 0.05 ) ∑1.96 Fe 1.02 (Co 0.63 Fe 0.16 Ni 0.19 Zn 0.04 Al 0.01 ) ∑1.03 [(OH) 2.88 O 1.12 ] ∑4.00 [(AsO 4 ) 1.95 (PO 4 ) 0.05 ] ∑2.00 , respectively. As derived from chemical analyses and crystal-structure investigations the ideal end-member compositions are Bi 2 Fe 3+ Fe 3+ O 2 (OH) 2 (AsO 4 ) 2 (neustädtelite) and Bi 2 Fe 3+ Co 2+ O(OH) 3 (AsO 4 ) 2 (cobaltneustädtelite). Extensive solid solution is observed between these two minerals. Neustädtelite and cobaltneustädtelite crystallize in space group P1̅; the cell parameters refined from powder data are a = 4.556(1)/9.156(1), b = 6.153(2)/6.148(1), c = 8.984(2)/9.338(1) Å, α = 95.43(2)/83.24(1), β = 99.22(2)/70.56(1), γ = 92.95(3)/86.91(1)°, V = 246.9/492.2 Å 3 , Z = 1/2, density (calc.) 5.81/5.81 g/cm 3 . Structure investigations were performed using single-crystal X-ray data. In both minerals edge-sharing alternating Fe 3+ Ø 6 and (Fe 3+ ,Co 2+ )Ø 6 /(Co 2+ ,Fe 3+) Ø 6 octahedra (Ø = O,OH) form chains parallel to [010] that are corner-linked by arsenate tetrahedra to layers parallel to (001). The Bi atoms are linked by O atoms to form columns parallel to [100]; these are sandwiched between layers of composition [6] M 2 (OH) 2 (AsO 4 ) 2 (M = Fe 3+ ,Co 2+ ). In neustädtelite the Bi atoms are site disordered; in cobaltneustädtelite half of the Bi atoms are ordered and half are on a split position. The partial ordering is induced by the presence of three OH groups, as compared to two in neustädtelite. A structural reinvestigation of medenbachite, Bi 2 Fe 3+ (Cu 2+ ,Fe 3+ )(O,OH) 2 (OH) 2 (AsO 4 ) 2 , proved isotypy with cobaltneustädtelite; the new cell parameters for medenbachite (refined from X-ray powder data) are: a = 9.162(2), b = 6.178(1), c = 9.341(2) Å, α = 83.50(2), β = 71.04(2), γ = 85.15(2)∞, V = 496 Å 3 , Z = 2.