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Abstract The ancylite supergroup has been approved by the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association, with the general crystal chemical formula ( M 3+ x M 2+ 2– x )(CO 3 ) 2 (OH) x ⋅(2– x )H 2 O (1 ≤ x ≤ 2, Z = 2). The ancylite supergroup can be divided into two groups defined by different proportions of the M cation and hydroxyl anion and/or water molecule: the ancylite group is defined for 1 ≤ x ≤ 1.5; the kozoite group is defined for 1.5 < x ≤ 2. The ancylite supergroup minerals are orthorhombic with space group Pmcn , or monoclinic with space group Pm 11, and have a crystal structure with species-defining trivalent and divalent M cations ( M = La 3+ , Ce 3+ , Nd 3+ , Ca 2+ , Sr 2+ and Pb 2+ ) which centre ten-vertex polyhedra formed by oxygen atoms at three independent O sites. Two vertices of the triangular (CO 3 ) 2– anion are oxygen atoms, whereas the third one, O(3), is statistically filled with (OH) – groups and H 2 O molecules. The triangular faces of three oxygen atoms of M O 10 coordination polyhedra join the chains of this ten-vertex polyhedron, which is extended along the c axis. The (CO 3 ) triangles connect chains in three dimensions. To date, eight valid mineral species with M 2+ = Sr 2+ , Ca 2+ and Pb 2+ belong to the ancylite group ancylite-(La), ancylite-(Ce), calcioancylite-(La), calcioancylite-(Ce), calcioancylite-(Nd), gysinite-(La), gysinite-(Ce) and gysinite-(Nd). Two hydroxyl carbonates with only rare earth elements as species-defining cations, kozoite-(La) and kozoite-(Nd) are members of the kozoite group.
Wang et al. (Mon,) studied this question.