Fungi and Sediments

By É. Verrecchia. 2000

91 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Ecology, Environmental Engineering

View Paper: https://www.semanticscholar.org/paper/e75ad0431fec835968a46de49a189601ef86a9ff

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In Earth-Surface Processes

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Citations in the corpus

Microbial Interaction with Clay Minerals and Its Environmental and Biotechnological Implications (2020, background): “Epitiths, endoliths and actively burrowing cryptoendoliths were found among taxonomically diverse filamentous fungi of the phyla Ascomycota, Basidiomycota and Zygomycota (the latter is now divided to two phyla Mucoromycota and Zoopagomycota) [56,89,90].”
Fungal involvement in bioweathering and biotransformation of rocks and minerals (2003, background): “Calcite formation by fungi may occur through indirect processes via the fungal excretion of oxalic acid and the precipitation of calcium oxalate (Verrecchia et al., 1990; Gadd, 1999; Verrecchia, 2000).”
Mycotransformation of organic and inorganic substrates (2004, unknown): “oxalates, oxides and carbonates (Arnott, 1995; Verrecchia, 2000; Gadd, 1999; Grote & Krumbein, 1992; Gharieb & Gadd, 1999) and this can lead to formation of biogenic minerals (mycogenic precipitates).”
In vitro formation of Ca-oxalates and the mineral glushinskite by fungal interaction with carbonate substrates and seawater (2005, background): “The ﬁrst and the second modes of precipitation have been described in present day caliches layers, weathering of carbonate buildings or in plants litter (Arnott, 1995; Sterﬂinger, 2000; Verrecchia, 2000; Garvie, 2003).”
Geomycology: fungi in mineral substrata (2003, unknown): “Summary of previous studies showing evidence of mineralization of fungal hyphae and lichen thalli with different minerals (*denotes common biogenic minerals) (adapted from Grote & Krumbein 1992; de la Torre & Gomez-Alarcon 1994; Easton 1997; Verrecchia 2000).”
Geomycology: biogeochemical transformations of rocks, minerals, metals and radionuclides by fungi, bioweathering and bioremediation. (2007, unknown): “Fungal filaments mineralized with calcite, together with whewellite, have been reported in limestone and calcareous soils from a range of localities (Kahle 1977; Calvet 1982; Callot et al. 1985a, 1985b; Verrecchia et al. 1993; Monger & Adams 1996; Bruand & Duval 1999; Verrecchia 2000).”
Metals, minerals and microbes: geomicrobiology and bioremediation. (2010, unknown): “Microbes are effective biological weathering agents and many can tolerate extremes of light, salinity, pH and water potential as well as adopting a variety of growth, metabolic and morphological strategies (Gorbushina et al., 1993; Sterflinger, 2000; Verrecchia, 2000; Burford et al., 2003a, b; Gadd,”
Interactions of Fungi with Concrete: Significant Importance for Bio-Based Self-Healing Concrete (2017, background): “On the other hand, the excretion of organic acids, especially oxalic acid, by fungal filaments plays an important role in the reprecipitation of secondary calcium minerals in the CaCO3-rich environments [51].”
Role of Fungi in the Biomineralization of Calcite (2016, background): “Within the last few decades, numerous studies have been dedicated to the interaction of fungi with metals and minerals and have shown that fungi are able to resist high concentrations of toxic metals [50,51], are important players in mineral weathering [29,30,48,52,53] and are large producers of sec”