Ammonia oxidation is a critical process of estuarine nitrogen cycling involving ammonia-oxidizing archaea (AOA) and bacteria (AOB). However, the distribution patterns of ammonia-oxidizing microorganisms (AOMs) between different habitats in the same area remain unclear. The present study investigated the AOMs' abundance and community compositions in both sediment and water habitats of the Yellow River estuary. Quantitative PCR (qPCR) revealed that AOA showed significant higher abundance than AOB both in sediment and water samples. AOA and AOB abundance distribution trends were consistent in sediment but distinct in water along the sampling sites. Clone librarybased analyses showed that AOA sequences were affiliated with Nitrososphaera, Nitrosopumilus and Nitrosotalea clusters. Generally, Nitrososphaera was predominant in sediment, while Nitrosopumilus and Nitrosotalea dominated in water column. AOB sequences were classified into genera Nitrosospira and Nitrosomonas, and Nitrosospira dominated in both habitats. Principal coordinate analysis (PCoA) also indicated AOA community structures exhibited significant differences between two habitats, while AOB were not. Ammonium and carbon contents were the potential key factors to influence AOMs' abundance and compositions in sediment, while no measured variables were determined to have major influences on communities in water habitat. These findings increase the understanding of the AOMs' distribution patterns in estuarine ecosystems.Ammonia oxidation, the first and rate limiting step of nitrification process, which can remove a substantial percentage (10-80%) of anthropogenic nitrogen pollution and reduce the risk of eutrophication in estuaries when coupled with denitrification 1-3 . Ammonia-oxidizing bacteria (AOB) were thought to be largely responsible for the oxidation of ammonia to nitrite in the past time 4 . The known AOB are categorized into two distinct monophyletic, Betaproteobacteria (β-AOB) from the genera Nitrosomonas and Nitrosospira, and Gammaproteobacteria (γ-AOB) from the genus Nitrosococcus [5][6][7][8] . However, this long-held view has been changed since the first cultivated ammonia-oxidizing archaea (AOA), Nitrosopumilus maritimus, which was isolated from a marine aquarium tank 9 . The identification of ammonia monooxygenase (AMO) in Thaumarchaeota indicated that both the AOA and AOB can responsible for the conversion of ammonia to hydroxylamine 10,11 . From then on, large number of researches investigated on the abundance, diversity and community structure of AOA and AOB in various environments, indicating their widely distributions in both marine and terrestrial ecosystems 12,13 . The community structure and spatial variation of AOA and AOB are essential for assessing the nitrification process. It has been suggested that the distribution of AOA and AOB diversity could be dependent on the types of habitat 12 . Previous studies indicated that AOA showed more abundance than AOB in many ecosystems such as paddy soils 14 , acidic soils 15 , river sedime...