2012
DOI: 10.1016/j.soilbio.2012.02.034
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Effect of calco-magnesian amendment on the mineral weathering abilities of bacterial communities in acidic and silicate-rich soils

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Cited by 21 publications
(10 citation statements)
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“…In our HSG experiments with pure cultures of R. aquatilis RA1, the nature and the concentration of organic acids produced reflected what can be found in soil compartments (e.g. the rhizosphere of podzolic soils) as shown elsewhere (Jones ; Balland‐Bolou‐Bi and Poszwa ). These authors measured micromolar concentrations of oxalic, acetic and formic acids, ranging from 0·1 to 1000 μmol l −1 , as well as traces of other acids such as malic, citric and succinic acids.…”
Section: Discussionsupporting
confidence: 76%
“…In our HSG experiments with pure cultures of R. aquatilis RA1, the nature and the concentration of organic acids produced reflected what can be found in soil compartments (e.g. the rhizosphere of podzolic soils) as shown elsewhere (Jones ; Balland‐Bolou‐Bi and Poszwa ). These authors measured micromolar concentrations of oxalic, acetic and formic acids, ranging from 0·1 to 1000 μmol l −1 , as well as traces of other acids such as malic, citric and succinic acids.…”
Section: Discussionsupporting
confidence: 76%
“…These differences in the biochemical processes in the soil and in experimental conditions can be explained by the fact that communities extracted from these soils are the only bacteria that are able to survive under our experimental conditions and that less than 1% of total soil bacteria are cultivable. These results are quite reproducible and agree with the preliminary work performed using other types of soils and bacterial strains studied (Balland et al, 2010;Balland-Bolou-Bi and Poszwa, 2012). In addition, the work of Vandevivereet al (1994) highlighted the existence of a "highly reactive zone" in the bacteria micro-environment, where extreme physico-chemical conditions (pH and metabolites gradients) could induce more mineral dissolution than would be expected from bulk solution.…”
Section: Link Between Global Soil Profiles Key Habitat Determinants supporting
confidence: 84%
“…among total cations, is significantly positively correlated with functional diversity ( p < 0.05, r 2 = 0.3676). Calcium and magnesium amendments have been shown to increase soil microbial diversity at soil horizon A1, which is within our sampling depth range (Balland‐Bolou‐Bi & Poszwa, 2012) suggesting base saturation as an important marker of soil microbial activity in the Point Loma Shaw's Agave habitat. The association between the plant and its microbiota is a critical aspect of plant fitness (Rodriguez & Durán, 2020; Rosenberg et al., 2010; Trivedi et al., 2020).…”
Section: Discussionsupporting
confidence: 72%