Thalliomelane, a new member of the coronadite group (hollandite supergroup), was discovered at Zalas near Cracow in southern Poland (the southern margin of the Cracow-Silesia Monocline) in relics of a preglacial supergene mineralization disseminated in a fault breccia in Middle Jurassic sandy limestone. The mineralization formed at the expense of a sulfide assemblage, which was most likely the source of thallium, related to rejuvenation of Early-Paleozoic fault zones in the Sava phase of the Alpine orogeny. Thalliomelane occurs rarely, and exclusively in the form of fibrous and highly porous tiny aggregates < 50 µm in size that fill small fractures and voids in the sandy limestone host rock. Microprobe analyses based on 16 O and 8 octahedral cations per formula unit resulted in the mean empirical formula (Tl 0.77(10) Ba 0.21(3) K 0.03(1) Na 0.01(0) Pb 0.01(0) ) Σ1.03(7) (Mn 4+ 7.15(11) Cu 2+ 0.63(4) Co 2+ 0.08(3) Fe 3+ 0.06(3) Ni 2+ 0.03(1) Si 0. 03(2) Mg 0.01(1) ) Σ8 [O 15.67(24) (OH) 0.33(24) ], corresponding to the formula Tl(Mn 4+ 7.5 Cu 2+ 0.5 )O 16 for the thalliomelane end-member. The mineral crystallizes in the tetragonal system, space group I4/m, and has unit-cell parameters a = 9.8664(12), c = 2.8721(4) Å, V = 279.59(8) Å 3 , Z = 1. The crystal structure of thalliomelane, measured with 3D electron-diffraction, was refined to an R 1 index of 23.74%. Thalliomelane has the hollandite-type structure. The Mn 4+ cations, substituted by Cu 2+ at an amount of ~0.5 apfu, are octahedrally coordinated by oxygen atoms. Four double chains of edge-sharing (Mn,Cu)-O octahedra share corners with each other to form tunnels along the [001] direction. Tl + cations are located in the tunnels, occupying partially the origin and centre of the unit cell. The formation of thalliomelane was most probably connected to the weathering of a sulfide mineral assemblage under semi-arid to arid climate. It resulted in the release of Tl and other components of the mineralization into water under the influence of Cl-,This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America. The published version is subject to change. Cite as Authors (Year) Title. American Mineralogist, in press.