The DOI matches its Crossref record; 234 of the 236 references it cites were found in a registry or an index.
Fungal involvement in bioweathering and biotransformation of rocks and minerals
Abstract
Abstract In the Earth’s lithosphere, fungi are of fundamental importance as decomposer organisms, animal and plant pathogens and symbionts (e.g. lichens and mycorrhizas), being ubiquitous in sub-aerial and subsoil environments. The ability of fungi to interact with minerals, metals, metalloids and organic compounds through biomechanical and biochemical processes, makes them ideally suited as biological weathering agents of rock and building stone. They also play a fundamental role in biogeochemical cycling of nutrients, (e.g. C, N, P and S) and metals (e.g. Na, Mg, Ca, Mn, Fe, Cu, Zn, Co and Ni) essential for the growth of living organisms in the biosphere. In addition they play an integral role in the mobilization and immobilization of non-essential metals (e.g. Cs, Al, Cd, Hg and Pb). Most studies on mineral-microbe interactions and microbial involvement in geological processes have concentrated on bacteria and archaea (Prokaryota): fungi (Eukaryota) have, to a certain extent, been neglected. This article addresses the role of fungi in geomicrobiological processes, emphasizing their deteriorative potential on rock, building stone and mineral surfaces and involvement in the formation of secondary mycogenic minerals. Such roles of fungi are also of importance for the global carbon reservoir and have potential biotechnological applications, e.g. in the bioremediation of xenobiotic-, metal- and/or radionuclide-contaminated soils and wastes, and metal/radionuclide recovery.
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“Several studies have demonstrated enhanced dissolution of serpentine and olivine by microbes mainly through the production of organic acids (e.g., [56][57][58]).”
From Strategizing carbon-neutral mines: A case for pilot projects (2014) · cites this paper as [58]
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Gadd, G. M. (2010) · Microbiology · doi:10.1099/mic.0.037143-0 · Cited by 2,013
“Microbe–clay mineral interactions are therefore important in soil evolution, as well as aggregation and stabilization (Burford et al., 2003a; Tazaki, 2006; Theng & Yuan, 2008).”
InfluentialSelf-citationMineral–Organic Associations: Formation, Properties, and Relevance in Soil Environments
Kleber, M., Eusterhues, K., Keiluweit, M., Mikutta, C., Mikutta, R., & Nico, P. (2014) · Advances in agronomy · doi:10.1016/bs.agron.2014.10.005 · Cited by 1,683
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“Since that time fungi have been ubiquitous components of the microbial communities of any terrestrial environment (Hawksworth 2001), including such hostile habitats as the arctic and Antarctic, hot deserts, and metal-rich and hypersaline soils (Burford et al. 2003a).”
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Metadata
- Authors
- Burford, E. P., Fomina, M., & Gadd, G. M.
- Affiliations
- University of Dundee (GB)
- Venue
- Mineralogical Magazine
- Publisher
- Mineralogical Society
- Published
- 2003-12
- Volume
- 67
- Issue
- 6
- Pages
- 1127-1155
- ISSN
- 0026-461X (ISSN-L)
- 1471-8022
- OpenAlex
- W2106222412
- Cited by
- 392
- References
- 236
- Citations by year
- 2026: 15 · 2025: 12 · 2024: 12 · 2023: 12 · 2022: 20 · 2021: 21 · 2020: 26 · 2019: 21 · 2018: 14 · 2017: 24 · 2016: 14 · 2015: 13 · 2014: 30 · 2013: 27 · 2012: 17
- FWCI
- 19.39
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Mineralogical Magazine (publishedVersion)
- Discovery Research Portal (University of Dundee) (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Building materials and conservation
- Physical Sciences › Materials Science › Metals and Alloys › Metal Extraction and Bioleaching
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- fungi, bioweathering, biotransformation, rock weathering, building stone deterioration, mineral-microbe interactions, metal mobilization, metal immobilization, biogeochemical cycles, bioremediation, radionuclide recovery, metal recovery, geomicrobiology
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