A CRUSTAL MINERAL IN A MANTLE DIAMOND

RECENT studies of diamonds, inclusions in diamonds, and rock fragments from the Earth's mantle have shown the presence of minerals and rocks with a chemical composition that suggests a previous origin in the cr ust; presumably, this crustal material was transported into the mantle at a subduction zone. The chemical evidence of previous residence of mantle materials in the crust has come principally from determinations of the proportions of the isotopes of oxygen(1,2), sulphur(3,4), lead (4,5) and carbon(6), which typically show a much wider range of compos ition in the crust than in material of purely mantle origin. Here we r eport a less subtle crustal signature in a mantle-derived diamond: an inclusion of the mineral staurolite. Staurolite has never previously b een found in mantle diamonds or rocks, but is a common mineral in meta morphic rocks in the crust. The characteristics of the staurolite sugg est not only the probability that it formed in rocks with a crustal bu lk composition, but also the possibility that it formed by metamorphis m in the crust or in a subduction zone, before being incorporated in t he mantle and, eventually, in a growing diamond.