Toward an ecological classification of soil bacteria.
By Noah Fierer, M. Bradford, R. B. Jackson. Ecology, 2007
4,535 citations recorded by the source corpus.
Subfields: Ecology, Molecular Biology, Soil Science
View Paper: https://www.semanticscholar.org/paper/8e3928b58bbd666fb2a95b6afad39572b72e66f6
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In Ecology
In Molecular Biology
- Rob Knight
- Noah Fierer
- C. Lauber
- J. Gregory Caporaso
- Micah Hamady
- Haiyan Chu
- Catherine A. Lozupone
- Ruth E. Ley
In Soil Science
Citations in the corpus
- Effects of straw amendment and moisture on microbial communities in Chinese fluvo-aquic soil (2014, background): “…thrive under conditions where substrate availability is high, while oligotrophic (or K-selected) populations (e.g., Acidobacteria, Gemmatimonadetes, and Basidiomycota) are relatively more abundant under substrate-limited conditions (Fierer et al. 2007; Bastian et al. 2009; Pascault et al. 2013).”
- Assessment of 10 years of CO2 fumigation on soil microbial communities and function in a sweetgum plantation (2009, background): “Acidobacteria tend to prefer oligotrophic soils (Fierer et al., 2007), and they do not seem to be out competed in soils of high [CO2] plots despite the increased flux of C.”
- Climate change feedbacks to microbial decomposition in boreal soils (2011, background): “Fierer et al. (2007) have proposed a functional classification scheme for bacteria, but both oligotrophic and copiotrophic classes occur within the Gram-negative bacteria, so measurements of bacterial community composition must occur at finer taxonomic resolution than PLFA groups to be functionally…”
- Patterns and mechanisms of responses by soil microbial communities to nitrogen addition (2017, background): “The plausible interpretation is that copiotrophic bacteria require more N per unit biomass C accumulation than oligotrophic fungi (Fierer et al., 2007; Manzoni et al., 2012; Waring et al., 2013; Mooshammer et al., 2014; Zechmeister-Boltenstern et al., 2015).”
- Microbial stress-response physiology and its implications for ecosystem function. (2007, neutral): “…soil microbial community is comprised of drought-tolerant, but less active microbes, and a group of r -selected rapidly growing but drought sensitive microbes, with traits closely analogous to the stress tolerators and colonizers of Grime’s (1977) plant classification system (Fierer et al. 2007).”
- Soil carbon quality and nitrogen fertilization structure bacterial communities with predictable responses of major bacterial phyla (2014, neutral): “Earlier, Fierer et al. (2007)”
- The Black Queen Hypothesis: Evolution of Dependencies through Adaptive Gene Loss (2012, background): “It is also worth noting the parallels between these two alternative evolutionary trajectories and the ideas of r- and K-selected organisms (52) and of “copiotrophs” and “oligotrophs” (53); one could speculate that the dynamics implicit in the BQH have been important in promoting the division between”
- Forest Soil Bacteria: Diversity, Involvement in Ecosystem Processes, and Response to Global Change (2017, background): “for bacterial strains with rapid growth and low-affinity substrate enzymes (r-strategists) that are enriched in comparison to the bulk soil profile (73, 132).”
- Trends in soil microbial communities during secondary succession (2017, background): “Besides the fungi:bacteria ratio, the copiotrophic vs. oligotrophic spectrum also exists within bacteria (Fierer et al., 2007; Zechmeister-Boltenstern et al., 2015).”
- The effect of resource history on the functioning of soil microbial communities is maintained across time (2011, background): “Soil microbial communities play a pivotal role in ecosystems as drivers of biogeochemical processes, including carbon and nitrogen cycling (Allison and Martiny, 2008; Lauber et al., 2009; Bell et al., 2005; Fierer et al., 2007; Manzoni and Porporato, 2009; McGuire and Treseder, 2010; Wallenstein et ”
- Digging deeper to find unique microbial communities: The strong effect of depth on the structure of bacterial and archaeal communities in soil (2012, background): “and aremost abundant in soils that have relatively large amounts of labile organic carbon, including rhizosphere soils (Fierer et al., 2007).”