Matches in SemOpenAlex for { <https://semopenalex.org/work/W3199255747> ?p ?o ?g. }
- W3199255747 endingPage "150425" @default.
- W3199255747 startingPage "150425" @default.
- W3199255747 abstract "Estuarine and coastal wetlands, which act as large sources of methane (CH 4 ) and undergo substantial loading of anthropogenic nitrogen (N), provide ideal conditions for denitrifying anaerobic methane oxidation (DAMO) to occur. Yet the microbial mechanisms governing DAMO and the main driving factors in estuarine and coastal ecosystems remain unclear. This study investigated the spatiotemporal distribution and associated activity of DAMO microorganisms along a wide swath of China's coastline (latitudinal range: 22–41°N) using molecular assays and isotope tracing techniques. We uncovered significant spatial and seasonal variation in DAMO bacterial community structure, whereas DAMO archaeal community structure exhibited no seasonal differences. The abundance of DAMO bacterial pmoA gene (2.2 × 10 5 –1.0 × 10 7 copies g −1 ) was almost one order of magnitude higher than that of DAMO archaeal mcrA gene (8.7 × 10 4 –1.8 × 10 6 copies g −1 ). A significant positive correlation between pmoA and mcrA gene abundances ( p < 0.01) was observed, indicating that DAMO bacteria and archaea may cooperate closely and thus complete nitrate elimination. Potential DAMO rates, in the range of 0.09–23.4 nmol 13 CO 2 g −1 day −1 for nitrite-DAMO and 0.03–43.7 nmol 13 CO 2 g −1 day −1 for nitrate-DAMO, tended to be greater in the relatively warmer low-latitudes. Potential DAMO rates were weakly positively correlated with gene abundances, suggesting that DAMO microbial activity could not be predicted directly by gene abundance alone. The heterogeneous variability of DAMO was shaped by interactions among key environmental characteristics (sediment texture, N availability, TOC, Fe 3+ , salinity of water, and temperature). On a broader continental scale, potential N removal rates of 0.1–11.2 g N m −2 yr −1 were estimated via nitrite-DAMO activity in China's coastal wetlands. Overall, our results highlight the widespread distribution of DAMO microbes and their potential role in eliminating excess N inputs and reducing CH 4 emissions in estuarine and coastal ecosystems, which could help mitigate global warming. • Denitrifying anaerobic CH 4 oxidation (DAMO) was quantified along the coast of China. • Higher DAMO rates appeared in the relatively low-latitude estuarine sites. • DAMO intensity was weakly positively correlated with microbial gene abundance. • Water temperature, salinity, sediment nutrients, and texture jointly regulated DAMO activity. • DAMO contributed 6.9 × 10 3 –6.4 × 10 5 t N yr -1 to N removal in China's coastal wetlands." @default.
- W3199255747 created "2021-09-27" @default.
- W3199255747 creator A5001318956 @default.
- W3199255747 creator A5014352132 @default.
- W3199255747 creator A5017353282 @default.
- W3199255747 creator A5027034753 @default.
- W3199255747 creator A5043528213 @default.
- W3199255747 creator A5046010230 @default.
- W3199255747 creator A5073792441 @default.
- W3199255747 creator A5089736720 @default.
- W3199255747 date "2022-02-01" @default.
- W3199255747 modified "2023-10-16" @default.
- W3199255747 title "Microbial dynamics and activity of denitrifying anaerobic methane oxidizers in China's estuarine and coastal wetlands" @default.
- W3199255747 cites W1542152274 @default.
- W3199255747 cites W1849498483 @default.
- W3199255747 cites W1890617200 @default.
- W3199255747 cites W1970887361 @default.
- W3199255747 cites W1983799891 @default.
- W3199255747 cites W1984914485 @default.
- W3199255747 cites W1986730085 @default.
- W3199255747 cites W1998956722 @default.
- W3199255747 cites W1999261855 @default.
- W3199255747 cites W2003375930 @default.
- W3199255747 cites W2006692172 @default.
- W3199255747 cites W2018537997 @default.
- W3199255747 cites W2032195874 @default.
- W3199255747 cites W2033250793 @default.
- W3199255747 cites W2043551521 @default.
- W3199255747 cites W2056257661 @default.
- W3199255747 cites W2068931955 @default.
- W3199255747 cites W2070868107 @default.
- W3199255747 cites W2071436107 @default.
- W3199255747 cites W2079418224 @default.
- W3199255747 cites W2079798371 @default.
- W3199255747 cites W2089464458 @default.
- W3199255747 cites W2117350830 @default.
- W3199255747 cites W2124025296 @default.
- W3199255747 cites W2130174419 @default.
- W3199255747 cites W2133148691 @default.
- W3199255747 cites W2133613652 @default.
- W3199255747 cites W2147818114 @default.
- W3199255747 cites W2170270191 @default.
- W3199255747 cites W2307818078 @default.
- W3199255747 cites W2419068691 @default.
- W3199255747 cites W2508125256 @default.
- W3199255747 cites W2508694077 @default.
- W3199255747 cites W2510098554 @default.
- W3199255747 cites W2535859909 @default.
- W3199255747 cites W2576215656 @default.
- W3199255747 cites W2617460225 @default.
- W3199255747 cites W2789756375 @default.
- W3199255747 cites W2791343134 @default.
- W3199255747 cites W2793132503 @default.
- W3199255747 cites W2796328379 @default.
- W3199255747 cites W2797728581 @default.
- W3199255747 cites W2804910636 @default.
- W3199255747 cites W2883579735 @default.
- W3199255747 cites W2895094108 @default.
- W3199255747 cites W2896925343 @default.
- W3199255747 cites W2899302476 @default.
- W3199255747 cites W2901080452 @default.
- W3199255747 cites W2904188148 @default.
- W3199255747 cites W2912418946 @default.
- W3199255747 cites W2912573235 @default.
- W3199255747 cites W2918137318 @default.
- W3199255747 cites W2923597814 @default.
- W3199255747 cites W2965502795 @default.
- W3199255747 cites W2972156087 @default.
- W3199255747 cites W2982075883 @default.
- W3199255747 cites W3002243768 @default.
- W3199255747 cites W3003199063 @default.
- W3199255747 cites W3009107792 @default.
- W3199255747 cites W3016430089 @default.
- W3199255747 cites W3021255131 @default.
- W3199255747 cites W3021602739 @default.
- W3199255747 cites W3025376910 @default.
- W3199255747 cites W3109553556 @default.
- W3199255747 cites W3135963492 @default.
- W3199255747 cites W3157075330 @default.
- W3199255747 doi "https://doi.org/10.1016/j.scitotenv.2021.150425" @default.
- W3199255747 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/34560448" @default.
- W3199255747 hasPublicationYear "2022" @default.
- W3199255747 type Work @default.
- W3199255747 sameAs 3199255747 @default.
- W3199255747 citedByCount "18" @default.
- W3199255747 countsByYear W31992557472022 @default.
- W3199255747 countsByYear W31992557472023 @default.
- W3199255747 crossrefType "journal-article" @default.
- W3199255747 hasAuthorship W3199255747A5001318956 @default.
- W3199255747 hasAuthorship W3199255747A5014352132 @default.
- W3199255747 hasAuthorship W3199255747A5017353282 @default.
- W3199255747 hasAuthorship W3199255747A5027034753 @default.
- W3199255747 hasAuthorship W3199255747A5043528213 @default.
- W3199255747 hasAuthorship W3199255747A5046010230 @default.
- W3199255747 hasAuthorship W3199255747A5073792441 @default.
- W3199255747 hasAuthorship W3199255747A5089736720 @default.
- W3199255747 hasConcept C104577883 @default.
- W3199255747 hasConcept C107872376 @default.