Mineral weathering by bacteria: ecology, actors and mechanisms.

By S. Uroz, C. Calvaruso, M. Turpault, P. Frey-Klett. Trends in Microbiology, 2009

641 citations recorded by the source corpus.

Subfields: Biomedical Engineering, Ecology, Health, Toxicology and Mutagenesis

View Paper: https://www.semanticscholar.org/paper/0406e33fc59ccfdceeae020489cf9b1ce25281d3

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Citations in the corpus

Mineral-microbe interactions: a review (2010, background): “, 2009), oxidation of reduced minerals and reduction of oxidized minerals (Santelli et al., 2001; Uroz et al., 2009).”
The role of abiotic factors modulating the plant-microbe-soil interactions: toward sustainable agriculture. A review (2017, background): “…including bacteria, fungi, and viruses (Hättenschwiler et al., 2005), may have important ecological roles because of their participation in the cycle of nutrients through the degradation of organic matter and minerals, which in turn provides essential nutrients for plant growth (Uroz et al., 2009).”
Potassium solubilizing bacteria (KSB):: Mechanisms, promotion of plant growth, and future prospects A review (2017, background): “For example, the amount of K solubilization by B. edaphicus in the liquid media was more and a better growth was detected on illite than feldspar (Uroz et al., 2009).”
Alteration of the soil bacterial community during parent material maturation driven by different fertilization treatments (2016, background): “Moreover, during the early period of soil formation, microorganisms enhance weathering through the production of organic acids, promotion of hydrolysis reactions, and the release of nutrients such as phosphorus and potassium from soil minerals (Lian et al., 2008; Uroz et al., 2009).”
Perspectives of plant-associated microbes in heavy metal phytoremediation. (2012, background): “, organic acids, siderophores), oxidation/reduction reactions (Gadd, 2000; Khan et al., 2009; Kidd et al., 2009; Uroz et al., 2009; Wenzel, 2009; Rajkumar et al., 2010; Ma et al., 2011a).”
Microbiology is the basis of sustainable agriculture: an opinion (2011, background): “Because of these mycorrhiza–rhizosphere interactions, bacteria are able to withdraw nutritional elements from soil organic compounds and primary minerals, thus ensuring a high trophic potential of plant-associated communities (Uroz et al., 2009).”
Bacteria and fungi can contribute to nutrients bioavailability and aggregate formation in degraded soils. (2016, positive): “Production of protons (H+) and organic acids anions not only enhances the chelation of cations which are bound to K but also helps for acidolysis of surrounding environment of microbes (Uroz et al., 2009; Keshavarz Zarjani et al., 2013; Parmar and Sindhu, 2013).”
Copper Metallurgical Slags – Current Knowledge and Fate: A Review (2015, background): “Microorganisms may attach to the solid surface as biofilm or microcolony and use the mineral surfaces as a source of nutrients (Gadd, 2007; Braud et al., 2009; Uroz et al., 2009; Flemming, 2011; Konhauser et al., 2011; Southam, 2012).”
Forest microbiome: diversity, complexity and dynamics. (2016, background): “Both fungi and bacteria contribute to the weathering of mineral surfaces (Hoffland et al. 2004; Uroz et al. 2009).”
The interplay between microbial communities and soil properties (2023, positive): “In particular, the microbial release of protons, organic acids (such as citrate or oxalate) or metal-complexing sidero-phores can contribute to biological weathering of minerals including granitic bedrock and silicates 10,40–43 .”