In this study, we used miTAG approach to analyze the distributional pattern and fine‐scale genetic diversity of the ammonia oxidizing archaea (AOA) lineages in the global oceans with the metagenomics data sets of the Tara Oceans global expedition (2009–2013). Using the ammonium monooxygenase alpha subunit gene as a biomarker, the AOA communities in the global oceans were recovered with highly diverse operational taxonomic units that affiliated to previously defined clades, including water column A (WCA), water column B (WCB), and SCM1‐like clades. In general, the AOA communities were obviously segregated with depth (except the upwelling regions), and the communities in the euphotic zones were more heterogeneous than in the mesopelagic zones (MPZs). The WCA distributed more evenly and widely in the euphotic zone and MPZs, while WCB and SCM1‐like clade mainly distributed in MPZ and high‐latitude waters, respectively. At fine‐scale genetic diversity, SCM1‐like and 2 WCA subclades showed distinctive niche separations of distributional pattern. We further divided the AOA subclades into ecological significant taxonomic units (ESTUs), which were delineated from the distribution pattern of their corresponding subclades. For example, ESTUs of WCA have different correlations with depth, nitrate to silicate ratio, and salinity; SCM1‐like A was negatively correlated with irradiation, whereas other SCM1‐like ESTUs preferred low‐temperature and high‐nutrient conditions. Our result showed that the previously defined AOA clades and ecotypes consist of highly diverse sublineages, whose diversity might be overlooked in the past. The distribution patterns of different ESTUs imply their ecophysiological characteristics and potential roles in biogeochemical cycling.
Phytoplankton are diverse and abundant as primary producers in the ocean, with diversity and community compositions varying spatially. How fundamental processes (e.g., selection, dispersal, and drift) regulate their global biogeography remains to be comprehensively explored.
Recognizing the prokaryotic community and its functions in hypoxic (>5 to ≤60 μM O
2
) environments before further expansion of OMZs is critical. We demonstrate the prokaryotic community and its potential functions in nitrogen metabolism in the Bay of Bengal (BoB), where oxygen concentration is barely above suboxic level.
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