Fungi in Biogeochemical Cycles: The oxalate–carbonate pathway in soil carbon storage: the role of fungi and oxalotrophic bacteria
By É. Verrecchia, Olivier Braissant, G. Cailleau. 2006
111 citations recorded by the source corpus.
Subfields: Atmospheric Science, Earth-Surface Processes, Ecology
View Paper: https://www.semanticscholar.org/paper/5ed8fd7e3e73b7dc223259e9081e05a685616fa4
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
In Earth-Surface Processes
In Ecology
- Geoffrey M. Gadd
- M. Fomina
- G. Cailleau
- S. Bindschedler
- C. Dupraz
- Olivier Braissant
- A. Decho
- R. Norman
Citations in the corpus
- Interactions of Fungi with Concrete: Significant Importance for Bio-Based Self-Healing Concrete (2017, background): “, a large amount of the secondary CaCO3 found in soils and surficial sediments originates by such a process [73].”
- Metals, minerals and microbes: geomicrobiology and bioremediation. (2010, unknown): “Calcium oxalate can also be degraded to calcium carbonate, and this may again cement pre-existing limestones (Verrecchia et al., 2006).”
- Geomycology: biogeochemical transformations of rocks, minerals, metals and radionuclides by fungi, bioweathering and bioremediation. (2007, unknown): “Calcite formation by fungi may occur through other indirect processes via the fungal excretion of oxalic acid and the precipitation of calcium oxalate (Verrecchia et al. 1990, 2006; Gadd 1999; Verrecchia 2000).”
- Experimental calcium-oxalate crystal production and dissolution by selected wood-rot fungi (2011, background): “Despite the fact that CaOx has multiple sources and is ubiquitous, surprisingly, it has not accumulated in the geological record (Verrecchia et al., 2006).”
- Reviews and syntheses: Biological weathering and its consequences at different spatial levels – from nanoscale to global scale (2020, background): “Since the oxalate is organic in origin, and half its C is transformed into mineral C with a much longer residence time, this process represents a potential major sink for sequestration of atmospheric C (Verrecchia et al., 2006).”
- Processes of carbonate precipitation in modern microbial mats (2009, background): “In the case of the acidic African forest soils, precipitation is due to the association between plants, fungi and oxalotrophic bacteria (Cailleau et al., 2004, 2005; Verrecchia et al., 2006).”
- Role of Fungi in the Biomineralization of Calcite (2016, background): “, through translocation within the fungal network), physicochemical degassing of fungal respired CO2, organic acid oxidation [75,76], urea mineralization [77,78] and nitrate assimilation [79].”
- Oxalate production by fungi: significance in geomycology, biodeterioration and bioremediation (2014, background): “(3) Oxalateecarbonate cycle Degradation of calcium oxalate by oxalotrophic bacteria resulting in CaCO3 formation is part of the oxalateecarbonate cycle (Verrecchia et al., 2006; Martin et al., 2012).”