Liu Jiwen, Huang Fuyan, Liu Jiao, Liu Xiaoyue, Lin Ruiyun, Zhong Xiaosong, Austin Brian, Zhang Xiao-Hua
Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences, Ocean University of China, Qingdao, 266100 China.
Laboratory for Marine Ecology and Environmental Science, Laoshan Laboratory, Qingdao, 266237 China.
Mar Life Sci Technol. 2023 Apr 7;5(2):257-270. doi: 10.1007/s42995-023-00169-y. eCollection 2023 May.
UNLABELLED: The majority of marine ammonia oxidizers belong to , a phylum of Archaea, which is distributed throughout the water column. Marine surface waters contain distinct thaumarchaeotal phylotypes compared to the deeper ocean, but spatial dynamics of the surface-associated lineages are largely unsolved. This study of 120 seawater samples from the eastern Chinese marginal seas identified contrasting distribution and association patterns among thaumarchaeotal phylotypes across different dimensions. Horizontally, -like and -like phylotypes dominated the surface water (3 m) of the Yellow Sea (YS) and East China Sea (ECS), respectively, along with increased abundance of total free-living in ECS. Similar compositional changes were observed in the surface microlayer. The spatial heterogeneity of particle-attached was less clear in surface microlayers than in surface waters. Vertically, the -like phylotype increased in abundance from surface to 90 m in ECS, which led to an increase in the proportion of relative to total prokaryotes. This occurred mainly in the free-living fraction. These results indicate a clear size-fractionated niche partitioning, which is more pronounced at lower depths than in the surface water/surface microlayer. In addition, associations of with other microbial taxa varied between phylotypes and size fractions. Our results show that a phylotype-resolved and size-fractionated spatial heterogeneity of the thaumarchaeotal community is present in surface oceanic waters and a vertical variation of the -like phylotype is present in shallow shelf waters. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s42995-023-00169-y.
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