Abstract

PurposeThe abundance and composition of nitrogen transformation-related microbes with certain environmental parameters for living conditions provide information about the nitrogen cycle in the Yangtze Estuary. The aim of this study was to explore the impacts of salinity on four N-related microbes and reveal the phylogenetic characteristics of microorganisms in the Yangtze Estuary ecosystem. A molecular biology method was used for the quantitation and identification of four microbes in the Yangtze River: ammonia-oxidizing bacteria (AOB), ammonia-oxidizing archaea (AOA), denitrifying microbes (nirS-type), and anaerobic ammonia-oxidizing (anammox) bacteria. Sequence identification was performed on the levels of phylum, class, order, family, and genus, and the sequences were then matched to species.ResultThe results showed that the dominant species of AOA were crenarchaeote enrichment cultures, thaumarchaeote enrichment cultures, and Nitrosopumilus maritimus cultures, and the dominant AOB species were betaproteobacterium enrichment cultures and Nitrosomona sp. The denitrifying microbes were identified as the phylum Proteobacteria, classes Alphaproteobacteria, Betaproteobacteria, and Gammaproteobacteria, and the species Thauera selenatis. The dominant species of the anammox bacteria was Candidatus Brocadia sp. In the estuarine sediments of the Yangtze River, the nirS gene abundance (1.31 × 107–9.50 × 108 copies g−1 sediments) was the highest among all the detected genes, and the abundance of bacterial amoA, archaeal amoA, and nirS was significantly correlated. Closely correlated with the abundance of the bacterial amoA gene, salinity was an important factor in promoting the abundance and restraining the community diversity of AOB. Moreover, the distribution of the AOB species exhibited regional patterns in the estuarine zone.ConclusionsThe results indicated that salinity might promote abundance while limiting the diversity of AOB and that salinity might have reverse impacts on AOA. Denitrifying microbes, which showed a significant correlation with the other genes, were thought to interact with the other genes during nitrogen migration. The results also implied that AOA has a lower potential nitrification rate than AOB and that both the anammox and denitrification processes (defined by nirS gene) account for N2 production.

Highlights

  • Nitrogen is a key element for living organisms but is one of the main causes of eutrophication in aquatic ecosystems (Bowen and Valiela 2001)

  • Result: The results showed that the dominant species of ammoniaoxidizing archaea (AOA) were crenarchaeote enrichment cultures, thaumarchaeote enrichment cultures, and Nitrosopumilus maritimus cultures, and the dominant ammonia-oxidizing bacteria (AOB) species were betaproteobacterium enrichment cultures and Nitrosomona sp

  • The results indicated that salinity might promote abundance while limiting the diversity of AOB and that salinity might have reverse impacts on AOA

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Summary

Introduction

Nitrogen is a key element for living organisms but is one of the main causes of eutrophication in aquatic ecosystems (Bowen and Valiela 2001). Because of the strong interaction between land and sea, the gradients of various physical, chemical, and biological factors have changed sharply (Kirwan and Megonigal 2013), and the processes of the nitrogen cycle in estuary areas have become more complex. Estuaries are typically environmentally vulnerable and sensitive zones in which the stability of ecosystems is disturbed and destroyed by natural and artificial factors. Environmental parameter gradients such as salinity are formed; as a result, the microbial community structure of estuaries is unique, as these areas contain abundant information about unknown genetics and ecology (Delgado-Baquerizo et al 2016). Studying the distribution and community composition of microbial flora in estuarine water is of great significance for the nitrogen cycle in ecotones

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