Archaeal and bacterial ammonia monooxygenase genes (amoA) had similar low relative abundances in freshwater sediment. In the rhizosphere of the submersed macrophyte Littorella uniflora, archaeal amoA was 500-to >8,000-fold enriched compared to bacterial amoA, suggesting that the enhanced nitrification activity observed in the rhizosphere was due to ammonia-oxidizing Archaea.In shallow aquatic ecosystems, rhizosphere-associated nitrogen transformations are central to understanding nutrient cycling (29). Oxygen release from the roots of freshwater macrophytes like Littorella uniflora, Lobelia dortmanna, and Glyceria maxima stimulates nitrification and coupled nitrificationdenitrification in freshwater sediments (4,29,34). However, the nitrifying community responsible for the increase in the rate has rarely been investigated (4, 21). The recent discovery of ammonia-oxidizing Archaea (AOA) (19, 41), the widespread distribution of these organisms (2,3,9,14,31,35), and their predominance in soils (24) and oceans (22,27,42) led to the hypothesis that AOA might also be important for nitrification in freshwater environments, including in the rhizosphere of freshwater macrophytes. The goals of this study were therefore (i) to test for the occurrence of AOA in freshwater sediment and in the rhizosphere of the macrophyte Littorella uniflora, (ii) to compare AOA diversity and abundance to the diversity and abundance of ammonia-oxidizing bacteria (AOB), and (iii) to compare the ammonia oxidizer communities in bulk and rhizosphere sediments.Sampling and chemical analysis. Sediment cores were obtained in triplicate from within monospecies stands of L. uniflora and from unvegetated sediment that was Ն5 m from the plant stands at a water depth of 20 to 30 cm in oligomesotrophic Lake Hampen, Jutland, Denmark (7). The distances between replicate cores were 2 to 70 m for vegetated sediment and 10 to 40 m for unvegetated sediment. For molecular (September 2005 and June 2006) and pore water (June 2006) analyses, the upper 1.5 cm of unvegetated sediment and L. uniflora rhizosphere sediment (depth, 1 to 6 cm) were transferred in the field to sterile 50-ml Falcon tubes and kept on ice during transport. In the laboratory, pore water was extracted within 24 h for analyses of pH, NO 2 Ϫ plus NO 3 Ϫ (6), NO 2 Ϫ (15), and NH 4 ϩ (5), and samples for DNA extraction were frozen at Ϫ80°C.To determine potential nitrification rates (June 2006), intact sediment cores were transported to the laboratory at ambient temperature (22 to 24°C). Rhizosphere and surface sediment samples were obtained and homogenized separately for each replicate core, and incubations at room temperature and 120 rpm were immediately set up with 20-g (fresh weight) subsamples in 40 ml of sterile lake water containing 100 M NH 4 ϩ . Apparent potential nitrification rates were calculated from the linear increase in concentrations of NO 2 Ϫ plus NO 3 Ϫ during the first 6 h, and the values were about eight times higher for the rhizosphere than for the unvegetated sediment.