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The newly discovered complete ammonia-oxidizing (comammox) has been identified in different environments, including coastal environments, where salinity is one of the most important factors for the abundance and activity of nitrifiers. Here, we demonstrate the effect of salinity on comammox , canonical ammonia-oxidizing bacteria (AOB), and ammonia-oxidizing archaea (AOA) in the intertidal sediments of the Yangtze River estuary based on microcosm experiments, DNA stable-isotope probing (DNA-SIP), and potential ammonium-oxidation rate (PAR) tests for different groups of ammonia oxidizers with selective inhibitors. During microcosm incubations, the abundance of comammox was more sensitive to increased salinity than that of other ammonia oxidizers. The results obtained with DNA-SIP heavy fractions showed that the dominant phylotype in clade A.2 (containing genes involved in the adaptation to haloalkaline environments) had high proportions in comammox community under both freshwater (0.06% salinity) and highly saline water (3% salinity) conditions. In contrast, another phylotype of clade A.2 (which lacks these genes) was dominant only under freshwater conditions. The PARs confirmed that comammox presented greater contributions to nitrification under freshwater conditions with a PAR of 4.37 ± 0.53 mg N·day·kg soil (54%) than under saline water conditions with a PAR of 0.60 ± 0.94 mg N·day·kg soil (18%). Moreover, AOA were specific to saline water conditions, whereas AOB were common under both freshwater and saline water conditions (44% and 52%, respectively). The present study provided evidence that salinity markedly affects the activity of comammox and that the salt sensitivity of different phylotypes varies. IMPORTANCE Complete ammonia oxidation (comammox) is a newly discovered type of nitrification through which ammonia is oxidized to nitrate in an organism. Comammox were abundantly found in coastal ecosystems and demonstrated high community diversity. Changes in salinity are considered one of the most important factors to comammox in coastal ecosystems; however, reports on the correlation between them remain inconsistent. Therefore, it is critical to experimentally determine the influence of salinity on comammox in the coastal ecosystem. This study demonstrated a clear effect of salinity on the abundance, activity, and relative contribution of different ammonia oxidizers, especially for comammox . To the best of our knowledge, this is the first study demonstrating comammox activity at seawater salinities, implying the existence of a salt-tolerant type comammox , despite its activity being much lower than in freshwater conditions. The indicated correlation between the activity of specific comammox and salinity is anticipated to provide insights into the distribution of comammox and their potential contributions in estuaries and coastal ecosystems.
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http://dx.doi.org/10.1128/msystems.01026-22 | DOI Listing |
Environ Res
August 2025
Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China; University of Chinese Academy of Sciences, Beijing, 100049, China. Electronic address:
Artificial wetlands have long been regarded as well-developed eco-engineering for nitrogen removal in aquatic ecosystems. Furthermore, they are also the biogeochemical hotspots of NO emissions. Recent studies indicate that ammonia-driven ammonia oxidation and NO production are even more important than the nitrate-driven heterotrophic denitrification for nitrogen removal.
View Article and Find Full Text PDFJ Hazard Mater
August 2025
School of Life Science and Environment Sciences, Shaoxing University, Shaoxing 312000, PR China; Jiangsu Provincial Key Lab for Organic Solid Waste Utilization, Jiangsu Collaborative Innovation Center for Solid Organic Waste Resource Utilization, Nanjing Agricultural University, Nanjing 210095, PR C
Emerging ecological risks of Per - and polyfluoroalkyl substances (PFASs) in terrestrial environments have received extensive attention. Yet, their impact on microbially-mediated nitrification processes in soils remains insufficiently investigated. Through a 42-day microcosm incubation experiment, we examined how two representative PFASs exposure, i.
View Article and Find Full Text PDFWater Res
July 2025
National Engineering Research Center of Eco-Environment in the Yangtze River Economic Belt, China Three Gorges Corporation, Wuhan Hubei 430014, PR China. Electronic address:
Managed aquifer recharge (MAR) is a critical technology for water resource management and purification, yet its capacity to remove antibiotics remains limited. Understanding the response of ammonia-oxidizing microorganisms (AOMs) to antibiotics exposure is essential for optimizing MAR-based antibiotic mitigation strategies. This study investigated the long-term effects of sulfamethoxazole (SMX, ∼500 ng/L) on AOM communities through a 20-month controlled MAR column experiment.
View Article and Find Full Text PDFEnviron Microbiol Rep
August 2025
Centre for Microbiology and Environmental Systems Science, University of Vienna, Vienna, Austria.
Isoprenoid quinones are important compounds in most organisms. They are essential in electron and proton transport in respiratory and photosynthetic electron transport chains, and additional functions include oxidative stress defence. The biologically most relevant quinones are naphthoquinones including menaquinone and benzoquinones including ubiquinone and plastoquinone.
View Article and Find Full Text PDFEnviron Res
July 2025
State Key Laboratory of Water Pollution Control and Green Resources Recycling, Shanghai Institute of Pollution Control and Ecological Security, College of Environmental Science and Engineering, Tongji University, Siping Road, Shanghai, 200092, China. Electronic address:
Nitrous oxide (NO) is a stringent greenhouse gas emitted from nitrogen removal processes in wastewater treatment plants (WWTPs), with emission factors (EFs) varying widely due to multi-dimensional factors like water quality, operational parameters, and biological processes. Current estimations often rely on the IPCC 2019 default EF of 1.1 ± 0.
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