The crystal structures of two unusual varieties of cancrinite-group minerals—oxalate-bearing cancrinite from the Kovdor massif (Kola Peninsula) and the sulfate end member of the davyne series from the Sar-e Sang mine (Badakhshan, Afghanistan)—were studied by single-crystal X-ray diffraction. The unit-cell parameters of the hexagonal cells are a = 12.688(4) Å, c = 5.189(1) Å and a = 12.773(1) Å, c = 5.334(1) Å, sp. gr. P6₃; the R factors are 0.034 and 0.035, respectively. The presence of oxalate groups in cancrinite as admixtures is one of the factors responsible for the shift of CO₃ groups in wide channels.