Genomics insights into ecotype formation of ammonia‐oxidizing archaea in the deep ocean

Summary Various lineages of ammonia‐oxidizing archaea (AOA) are present in deep waters, but the mechanisms that determine ecotype formation are obscure. We studied 18 high‐quality genomes of the marine group I AOA lineages (alpha, gamma and delta) from the Mariana and Ogasawara trenches. The genomes...

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Published inEnvironmental microbiology Vol. 21; no. 2; pp. 716 - 729
Main Authors Wang, Yong, Huang, Jiao‐Mei, Cui, Guo‐Jie, Nunoura, Takuro, Takaki, Yoshihiro, Li, Wen‐Li, Li, Jun, Gao, Zhao‐Ming, Takai, Ken, Zhang, Ai‐Qun, Stepanauskas, Ramunas
Format Journal Article
LanguageEnglish
Published Hoboken, USA John Wiley & Sons, Inc 01.02.2019
Wiley Subscription Services, Inc
Wiley-Blackwell
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Summary:Summary Various lineages of ammonia‐oxidizing archaea (AOA) are present in deep waters, but the mechanisms that determine ecotype formation are obscure. We studied 18 high‐quality genomes of the marine group I AOA lineages (alpha, gamma and delta) from the Mariana and Ogasawara trenches. The genomes of alpha AOA resembled each other, while those of gamma and delta lineages were more divergent and had even undergone insertion of some phage genes. The instability of the gamma and delta AOA genomes could be partially due to the loss of DNA polymerase B (polB) and methyladenine DNA glycosylase (tag) genes responsible for the repair of point mutations. The alpha AOA genomes harbour genes encoding a thrombospondin‐like outer membrane structure that probably serves as a barrier to gene flow. Moreover, the gamma and alpha AOA lineages rely on vitamin B12‐independent MetE and B12‐dependent MetH, respectively, for methionine synthesis. The delta AOA genome contains genes involved in uptake of sugar and peptide perhaps for heterotrophic lifestyle. Our study provides insights into co‐occurrence of cladogenesis and anagenesis in the formation of AOA ecotypes that perform differently in nitrogen and carbon cycling in dark oceans.
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USDOE
ISSN:1462-2912
1462-2920
DOI:10.1111/1462-2920.14518