Ammonia concentration determines differential growth of ammonia-oxidising archaea and bacteria in soil microcosms

By D. Verhamme, J. Prosser, G. Nicol. The ISME Journal, 2011

669 citations recorded by the source corpus.

Subfields: Ecology, Environmental Engineering, Pollution

View Paper: https://www.semanticscholar.org/paper/8504e2006d85e9c1a8e51e044cb020b71bd7cc1c

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Ecology

1. Ji‐Zheng He
2. Hangwei Hu
3. Li‐Mei Zhang
4. Ju-Pei Shen
5. David J. Levy-Booth
6. C. Prescott
7. Yongfei Bai
8. G. Du

In Environmental Engineering

1. David J. Levy-Booth
2. C. Prescott
3. Ju-Pei Shen
4. Ji‐Zheng He
5. Li‐Mei Zhang
6. S. Grayston
7. Hangwei Hu

In Pollution

1. Ji‐Zheng He
2. Hangwei Hu
3. Li‐Mei Zhang
4. Ju-Pei Shen
5. David J. Levy-Booth
6. C. Prescott
7. S. Grayston

Citations in the corpus

• Responses of ammonia-oxidizing bacteria and archaea to nitrogen fertilization and precipitation increment in a typical temperate steppe in Inner Mongolia (2013, background): “In a series of soil microcosms, AOB abundance responded positively to the addition of N fertilizers, whereas the AOA abundance remained stable or was even decreased by high levels of N amendment (Di et al., 2009, 2010; Verhamme et al., 2011).”
• Ammonia-oxidizing archaea have more important role than ammonia-oxidizing bacteria in ammonia oxidation of strongly acidic soils (2011, background): “A recent study found available ammonia concentrations determined the niche separation of AOA and AOB in soil microcosms with AOA preferring low levels of ammonia supply (Verhamme et al., 2011), and growth of AOA has been presumably correlated with high rates of nitrification in an acetylene inhibiti”
• Current insights into the autotrophic thaumarchaeal ammonia oxidation in acidic soils (2012, background): “We do not knowwhether pH itself has directly shaped the ecological niches of AOA and AOB in acidic soils, or whether the differences are due to indirect influences induced by low pH.”
• 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, background): “The effects of fertilization on the activity and community structure of soil ammonia-oxidizing bacteria (AOB) and ammonia-oxidizing archaea (AOA), which are ubiquitous in soils and aquatic environments, has recently been emphasized (Cavagnaro et al., 2008; Shen et al., 2008; Verhamme et al., 2011; W”
• Identifying response groups of soil nitrifiers and denitrifiers to grazing and associated soil environmental drivers in Tibetan alpine meadows (2014, background): “This discrepancy could be due to the fact that, on average, the growth of AOB is likely better under high N concentrations, while the growth of AOAwould be favored for lower N concentrations (Di et al., 2010; Verhamme et al., 2011).”
• Contrasting effects of nitrogen forms and soil pH on ammonia oxidizing microorganisms and their responses to long-term nitrogen fertilization in a typical steppe ecosystem (2017, background): “…2011; He et al., 2012; Isobe et al., 2012; Zhang et al., 2012; Lu and Jia, 2013) or in pH neutral soils without heavy N addition (Di et al., 2010; Verhamme et al., 2011), while AOB were more active than AOA in some non-acidic soils receiving N inputs (Shen et al., 2008; Di et al., 2009; Jia and…”
• Linking microbial communities, functional genes and nitrogen-cycling processes in forest floors under four tree species (2016, positive): “Although archaea are considered to contribute little to soil microbial biomass 417 (Gattinger et al., 2002; Bardgett and Griffiths, 1997), archaea in forest soils can have a functional 418 role in N cycling akin to a keystone species (Prosser and Nicol, 2008; Verhamme et al., 2011).”