Previous studies have indicated that bacterial polyamine patterns may be useful for chemotaxonomic evaluations (6). In the course of investigations on the possible existence of unusual polyamines in extremely halophilic archaebacteria, we detected agmatine as the major polyamine and arginine decarboxylase (ADC) activity which produces agmatine from arginine in the cells of some strains of Halobacterium and Halococcus (5,8). These extreme halophiles were devoid of any other polyamines and of lysine decarboxylase (LDC) and ornithine decarboxylase (ODC) activities which produce cadaverine and putrescine, respectively (5, 8). Extremely halophilic, nonmethanogenic archaebacteria are comprised of essentially two groups: extreme halophiles that grow at neutrality include the genera Halobacterium, Haloarcula, Haloferax and Halococcus and extremely haloalkaliphilic isolates that grow only at high pH include the genera Natronobacterium and Natronococcus (3,10,13). In the present study, polyamines of 41 strains of the published species of extremely halophilic, nonmethanogenic archaebacteria listed in Table 1 were analyzed to evaluate polyamine type as a chemotaxonomic marker.Organisms belonging to the genera Halobacterium, Haloarcula, Haloferax and Halococcus were grown in the synthetic Onishi-McCance-Gibbons medium (OMG medium), pH 6.2 (11). Natronobacterium pharaonis was grown in OMG medium adjusted pH at 9.0. The medium contains 15 amino acids including arginine and lysine, AMP, UMP, trisodium citrate, glycerol, various inorganic salts, 2% MgSO4 7H20 and 25% NaCI but not ornithine and polyamines. Three other species of Natronobacterium and Natronococcus occultus which did not grow in