A method was developed to determine the contributions of ammonia-oxidizing archaea (AOA) and ammoniaoxidizing bacteria (AOB) to the nitrification potentials (NPs) of soils taken from forest, pasture, cropped, and fallowed (19 years) lands. Soil slurries were exposed to acetylene to irreversibly inactivate ammonia monooxygenase, and upon the removal of acetylene, the recovery of nitrification potential (RNP) was monitored in the presence and absence of bacterial or eukaryotic protein synthesis inhibitors. For unknown reasons, and despite measureable NPs, RNP did not occur consistently in forest soil samples; however, pasture, cropped, and fallowed soil RNPs commenced after lags that ranged from 12 to 30 h after acetylene removal. Cropped soil RNP was completely prevented by the bacterial protein synthesis inhibitor kanamycin (800 g/ml), whereas a combination of kanamycin plus gentamicin (800 g/ml each) only partially prevented the RNP (60%) of fallowed soils. Pasture soil RNP was completely insensitive to either kanamycin, gentamicin, or a combination of the two. Unlike cropped soil, pasture and fallowed soil RNPs occurred at both 30°C and 40°C and without supplemental NH 4 ؉ (<10 M NH 4 ؉ in solution), and pasture soil RNP demonstrated ϳ50% insensitivity to 100 M allyl thiourea (ATU). In addition, fallowed and pasture soil RNPs were insensitive to the fungal inhibitors nystatin and azoxystrobin. This combination of properties suggests that neither fungi nor AOB contributed to pasture soil RNP and that AOA were responsible for the RNP of the pasture soils. Both AOA and AOB may contribute to RNP in fallowed soil, while RNP in cropped soils was dominated by AOB.Until 2005 the majority of ammonia (NH 3 ) oxidation in natural environments was thought to be carried out by a phylogenetically distinct group of NH 3 -oxidizing bacteria (AOB). This nitrification paradigm was challenged by reports that thaumarchaeota carry the genes that encode the enzyme ammonia monooxygenase (AMO) (55); the isolation of "Candidatus Nitrosopumilus maritimus" strain SCM1, an obligate autotrophic thaumarchaeal NH 3 oxidizer (35); the detection of archaeal amoA gene transcripts in soil (54, 55); and the realization that ammonia-oxidizing archaea (AOA) were widely distributed (19) and often more numerous than AOB in soil (36), marine (40), and hot spring (52, 57) ecosystems. Others have correlated either the AOA (7,46,58) or AOB amoA gene copy abundance (17, 32) with nitrification activity and detected the expression of AOA amoA mRNA (43, 60). To our knowledge there is no published work that has directly distinguished NH 3 -oxidizing activity by AOA from NH 3 -oxidizing activity by AOB in soils.As yet, it is unknown what factors determine whether AOA or AOB nitrify in an environment. We hypothesized that AOA and AOB might contribute differentially to nitrification in diverse soils across a landscape with different physical and chemical characteristics, plant community compositions, and management practices. We know that nitrification by AOA a...