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A B S TR A CT Rare earth element (REE) and yttrium concentrations of coexisting monazite and xenotime were determined from a suite of seven metapelites from the Variscan fold belt in NE Bavaria, Germany. The metapelites include a continuous prograde, mainly low-P (3-5 kbar) metamorphic profile from greenschist (c. 400°C) to lower granulite facies conditions (c. 700°C). The LREE (La-Sm) are incorporated preferentially in monoclinic monazite (REO 9 polyhedron), whereas the HREE plus Y are concentrated in tetragonal xenotime (REO 8 polyhedron). The major element concentrations of both phases in all rocks are very similar and do not depend on metamorphic grade. Monazite consists mainly of La, Ce and Nd (La 0.20-0.23 , Ce 0.41-0.45 , Nd 0.15-0.18 )PO 4 , all other elements are below 6 mol%. Likewise, xenotime consists mainly of YPO 4 with some Dy and Gd solid solutions (Y 0.76-0.80 , Dy 0.05-0.07 , Gd 0.04-0.06). In contrast, the minor HREE concentrations in monazite increase strongly with increasing metamorphic grade: Y, Dy and Gd increase by a factor of 3-5 from greenschist to granulite facies rocks. Monazite crystals often show zonation with cores low in HREE and rims high in HREE that is interpreted as growth zonation attained during prograde metamorphism. Similarly, Sm and Nd in xenotimes increase by a factor of 3-4 with increasing metamorphic grade. Prograde zonation in single crystals of xenotime was not observed. The X HREE+Y in monazite and X LREE in xenotime of the seven rocks define two limbs along the strongly asymmetric miscibility gap from c. 400°C to 700°C. The empirical calibration of the monazite miscibility gap limb coexisting with xenotime is appropriate for geothermometry. Due to its contents of U and Th, monazite has often been used for U-Pb age determination. The combination of our empirical thermometer on prograde zoned monazite along with possible age determination of zoned single crystals may provide information about prograde branches of temperature-time paths.