Cesanite

A variety of Minerals

What is Cesanite?

Cesanite is the end member of the apatite-wilkeite-ellestadite series that substitutes all of apatite's phosphate ions with sulfate ions and balances the difference in charge by replacing several calcium ions with sodium ions. Currently very few sites bearing cesanite have been found and are limited to a geothermal field in Cesano, Italy from which its name is derived, Măgurici Cave in Romania, and in the San Salvador Island caves in the Bahamas.

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Cesanite Localities Map

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North ZoneCentral RidgeSouth Basin

Key Characteristics

Characteristics of Cesanite

Cesanite veins are massive in habit and appear white in color with a silky luster. Individual crystals are colorless and transparent to translucent with a greasy luster. These crystals are elongated and begin with a pyramid on {101*0} that is distorted by a flatting that occurs down the length of the crystal which then extends down with two parallel faces until they are cut off by either a pinacoid or another pyramid. According to the newest sources the cells spacings for cesanite are 9.4630 along its a-axises and 6.9088 along its c-axis. In thin section cesanite remains transparent and has moderate birefringence. In addition to is structure at room temperature Cesanite exhibits different crystal structures at different temperatures. Polymorphs occur at 425, 625, and 740 °C. These different forms are cause by expansion along the crystallographic axises as cesanite is heated.

Composition of Cesanite

Cesanite was originally determined by Tazzoli (1983) to be isotypic to that of hydroxylapatite. This was determined by refining the original unit cell dimensions and comparing them to the atomic coordinates of Holly Springs hydroxylapatite. From this it was extrapolated that although different elements are substituted for cesanite, the structure and cell parameters are nearly the same with some differences in the bond lengths of the tetrahedra. This similarity was to confirm the space group 63/m previously assigned to cesanite, this changed in 2002 after a reexamination of cesanite by Piotrowski et al. was prompted by its similarities to a synthetically produced analog. After this study it was found that the crystal structure of cesanite to be isostructural to this synthetic analog with the chemical formula Ca2Na3[(OH)(SO4)3]. What can be inferred from this is that while hydroxylapatite remains similar in its chemical formula it is not longer to be considered a structural analog. The new correct space group is 6. It can be inferred that the reason the mistake went unnoticed for so long is that cesanite retains pseudo-symmetry in the array of its tetrahedra that closely mimics 63/m. Cesanite's crystal structure is made up of tetrahedra of sulfide cations surrounded by oxygen anions distributed along with hydroxide ions around the Ca and Na ions occupying the M1 through four sites. The M1 and M2 cites create distorted pentagonal bipyramids while the M3 and M4 create tricapped trigonal prisms. The M3 and M4 polyhedra share faces when they are next to each other and form columns parallel to [001] while isolated sulfate tetrahedra alternate along the c axis.