Microbial biogeography at the soil pore scale
By L. Ruamps, N. Nunan, Claire Chenu. 2011
211 citations recorded by the source corpus.
Subfields: Ecology, Environmental Chemistry, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/89a14e7d7410df39fe1a7e2013b6134ae4b5afc9
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Ecology
- Y. Kuzyakov
- E. Blagodatskaya
- Sean Schaeffer
- J. Schimel
- A. Brauman
- G. Santoyo
- L. Passaglia
- A. Ambrosini
In Environmental Chemistry
In Molecular Biology
- Y. Kuzyakov
- J. Schimel
- E. Blagodatskaya
- P. Maron
- Rocheli de Souza
- Sean Schaeffer
- Claire Chenu
- G. Santoyo
Citations in the corpus
- Microbial hotspots and hot moments in soil: Concept & review (2015, background): “…hotspot identification Identifying hotspots in soil is very challenging because: i) identification should focus on process intensities (and not on contents or concentrations), ii) the processes should be traced in undisturbed soil, without mixing of hotspots with bulk soil (Ruamps et al., 2011).”
- Microbial control over carbon cycling in soil (2012, background): “…bacteria and fungi use as components of their cell walls (peptidoglycan and chitin, respectively) become important constituents in soil organic nitrogen pools (Dai et al., 2002; Kögel-Knabner, 2002; Joergensen and Wichern, 2008), yet are produced differentially by the different groups of organisms.”
- Plant growth-promoting bacteria as inoculants in agricultural soils (2015, background): “, 2013), and low pore connectivity due to low water potential increases the diversity of bacterial communities in the soil (Carson et al., 2010; Ruamps et al., 2011).”
- Dynamics of bacterial communities in relation to soil aggregate formation during the decomposition of 13C-labelled rice straw (2012, methodology): “and Stahl, 2004) and suggesting that there is a microscale biogeography in soil (Mummey et al., 2006; Ruamps et al., 2011).”
- Fungal communities are more sensitive indicators to non-extreme soil moisture variations than bacterial communities (2015, background): “Contrastingly, the lack of difference for the 257 bacterial community is unexpected as different pore or aggregate size classes support distinct 258 bacterial populations (Ruamps et al., 2011; Davinic et al., 2012).”
- The role of abiotic factors modulating the plant-microbe-soil interactions: toward sustainable agriculture. A review (2017, background): “Moreover, communities can also vary according to the size of the pore dwellings (Ruamps et al., 2011), which influences carbon mineralization (Ruamps et al., 2013).”