Ammonia oxidation is a major process in nitrogen cycling, and it plays a key role in nitrogen limited soil ecosystems such as those in the arctic. Although mm-scale spatial dependency of ammonia oxidizers has been investigated, little is known about the field-scale spatial dependency of aerobic ammonia oxidation processes and ammonia-oxidizing archaeal and bacterial communities, particularly in arctic soils. The purpose of this study was to explore the drivers of ammonia oxidation at the field scale in cryosols (soils with permafrost within 1 m of the surface). We measured aerobic ammonia oxidation potential (both autotrophic and heterotrophic) and functional gene abundance (bacterial amoA and archaeal amoA) in 279 soil samples collected from three arctic ecosystems. The variability associated with quantifying genes was substantially less than the spatial variability observed in these soils, suggesting that molecular methods can be used reliably evaluate spatial dependency in arctic ecosystems. Ammoniaoxidizing archaeal and bacterial communities and aerobic ammonia oxidation were spatially autocorrelated. Gene abundances were spatially structured within 4 m, whereas biochemical processes were structured within 40 m. Ammonia oxidation was driven at small scales (<1m) by moisture and total organic carbon, whereas gene abundance and other edaphic factors drove ammonia oxidation at medium (1 to 10 m) and large (10 to 100 m) scales. In these arctic soils heterotrophs contributed between 29 and 47% of total ammonia oxidation potential. The spatial scale for aerobic ammonia oxidation genes differed from potential ammonia oxidation, suggesting that in arctic ecosystems edaphic, rather than genetic, factors are an important control on ammonia oxidation.A pproximately 13% of world's total land area is underlain by permafrost and in Canada permafrost-affected soils comprise 3.7 million km 2 or ca. 40% of the land mass (67). These soil ecosystems differ from others due to their low annual mean temperatures, long winters, short growing seasons, frequent cryoturbation (soil movement because of frost action), and gelifluction (slow downslope movement of waterlogged soil over permafrost layer and formation of lobe-shaped features). A key feature of these arctic ecosystems compared to temperate ecosystems is that substantial ammonia (as much as 14 mg m Ϫ2 NH 4 ϩ -N) is produced over the winter period and the fate of this ammonia is crucial to the productivity of the above ground ecosystems (8). Climate change will impact snow cover and mean annual temperatures, and this is going to significantly increase the over-winter nitrogen mineralization (8), yet we know very little about fieldscale ammonia oxidation processes in arctic ecosystems. The oxidation of ammonia to nitrite is the first and rate-limiting step of nitrification. In soil, ammonia oxidation is regulated by a combination of the ammonia-oxidizing communities (59) and soil physicochemical properties (7). The purpose of this investigation was to characterize how the biol...