In residues of several iron meteorites, obtained by dissolution of a metal piece in 2M H2 SO4i isotopic ratio of 196Hg/2o2Hg has been measured by radiochemical neutron activation analysis in Hg frac tions, released by stepwise heating. Both positive and negative deviations relative to terrestrial composi tion, have been found. Anomalies are more frequently observed in the high temperature fractions (200