Nitrification driven by bacteria and not archaea in nitrogen-rich grassland soils

By H. Di, K. Cameron, Ju-Pei Shen, C. Winefield, M. O’Callaghan, S. Bowatte, Ji‐Zheng He. 2009

862 citations recorded by the source corpus.

Subfields: Ecology, Molecular Biology, Pollution

View Paper: https://www.semanticscholar.org/paper/731ec456aea2958bb13c1bb72f21b42a484ed6f4

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Citations in the corpus

Microbial regulation of terrestrial nitrous oxide formation: understanding the biological pathways for prediction of emission rates. (2015, background): “2012), while DCD had more effective inhibition on AOB in nitrogenrich grassland soils (Di et al. 2009; Dai et al. 2013).”
Ammonia concentration determines differential growth of ammonia-oxidising archaea and bacteria in soil microcosms (2011, background): “However, growth of AOB, and not of AOA, has been linked to nitrification activity following amendment with high levels of ammonium, either directly as mineral fertiliser or as urea, which is rapidly hydrolysed to ammonium (Di et al., 2009; Jia and Conrad, 2009).”
Nitrososphaera viennensis, an ammonia oxidizing archaeon from soil (2011, neutral): “Upon amendment of fertilizer, growth of ammonia oxidizing bacteria (AOB) was reported to correlate with nitrification activity, whereas archaea did not seem to respond (20, 23, 24).”
Exotic invasive plants increase productivity, abundance of ammonia‐oxidizing bacteria and nitrogen availability in intermountain grasslands (2016, background): “5b) at our sites did not increase in invaded patches, indicating that AOB were likely drivers of increased nitrification and soil NO 3 in our system (see also Di et al. 2009).”
Ammonia-oxidizing archaea have more important role than ammonia-oxidizing bacteria in ammonia oxidation of strongly acidic soils (2011, background): “Previous studies found only AOB to be significantly affected by addition of DCD in grazed dairy pastures (Di et al., 2009, 2010; O’Callaghan et al., 2010) and, as far as we know, currently there is no published study demonstrating inhibition of AOA by DCD.”
Current insights into the autotrophic thaumarchaeal ammonia oxidation in acidic soils (2012, background): “…abundance responded positively to the amendment of nitrogen fertilizer and correlated well with nitrification activity in heavily fertilized soils (Di et al., 2009, 2010) or wetland (Levicnik-Höfferle et al., 2010), whereas AOA growth was suppressed by high levels of ammonium in soil microcosms…”
Responses of ammonia-oxidizing bacteria and archaea to nitrogen fertilization and precipitation increment in a typical temperate steppe in Inner Mongolia (2013, background): “In N-rich rassland soils, AOB abundance and activity increased whereas he AOA abundance and activity remain unchanged in response to additions (Di et al., 2009).”
Abundance and community structure of ammonia-oxidizing bacteria and archaea in a temperate forest ecosystem under ten-years elevated CO2 (2012, background): “Studies on the effect of N addition have shown an increasing in amoA gene abundance of soil AOB but not of AOA, with AOB being predominant over AOA in the N-rich environment (Di et al., 2009; Hallin et al., 2009).”
Different roles of rhizosphere effect and long-term fertilization in the activity and community structure of ammonia oxidizers in a calcareous fluvo-aquic soil (2013, result): “The predominance of bacterial nitrification is consistent with previous reports for a grassland soil in New Zealand (Di et al., 2009) and an agricultural soil in Germany (Jia and Conrad, 2009), but inconsistent with reports for most acidic soils (Gubry-Rangin et al.”
Abundance and community structure of ammonia-oxidizing archaea and bacteria in an acid paddy soil (2011, background): “Recently, some researchers found that archaea were not important for nitrification in their tested soils (Di et al. 2009; Jia and Conrad 2009).”