2006
DOI: 10.1080/01490450600964375
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Biomineralization of Fungal Hyphae with Calcite (CaCO3) and Calcium Oxalate Mono- and Dihydrate in Carboniferous Limestone Microcosms

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Cited by 119 publications
(85 citation statements)
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“…In the context of BIM, the organism modifies its local microenvironment to create appropriate physico-chemical conditions for the precipitation of minerals (Gadd, 2010;Gadd et al, 2012;Li et al, 2014Li et al, , 2015. Most microbial biomineralization processes therefore usually refer to biologically-induced mineralization (Burford, Hillier, & Gadd, 2006;Uroz et al, 2009;Gadd, 2010;Li, Csetenyi, & Gadd, 2014;Rhee, Hiller, & Gadd, 2015).…”
Section: Biomineralizationmentioning
confidence: 99%
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“…In the context of BIM, the organism modifies its local microenvironment to create appropriate physico-chemical conditions for the precipitation of minerals (Gadd, 2010;Gadd et al, 2012;Li et al, 2014Li et al, , 2015. Most microbial biomineralization processes therefore usually refer to biologically-induced mineralization (Burford, Hillier, & Gadd, 2006;Uroz et al, 2009;Gadd, 2010;Li, Csetenyi, & Gadd, 2014;Rhee, Hiller, & Gadd, 2015).…”
Section: Biomineralizationmentioning
confidence: 99%
“…Moreover, 13% of the total land surface of the Earth is occupied by the near-surface calcretes and dolocretes in the soil environment and they are important carbon reservoirs in the Earth's lithosphere (Ehrlich & Newman, 2009;Goudie, 1996). A significant proportion of such carbonate minerals at the Earth's surface is of biogenic origin, and many microorganisms, including bacteria and fungi, can deposit calcium carbonate extracellularly (Verrecchia, Dumont, & Rolko, 1990;Goudie 1996;Yamanaka, 1999;Verrecchia, 2000;Burford, Hillier, & Gadd, 2006;Navarathna et al, 2010;Barua et al, 2012;Li et al, 2014Li et al, , 2015. Calcium carbonate precipitation by bacteria is generally regarded to be inducible and the type of mineral produced is largely dependent on environmental conditions (Rivadeneyra et al, 1994;Ben Omar, Arias, & González-Muñoz, 1997;Brennan, Lowenstein, & Horita, 2004).…”
Section: Biomineralizationmentioning
confidence: 99%
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“…Vacuolation and compartmention are essential for metal detoxification (Gonzalez et al, 2008). Some fungi can precipitate metals in amorphous and crystalline forms, such as oxalates and other secondary mycogenic minerals (Burford et al, 2006). Copper (II) tolerance by fungi has been extensively investigated, and the ability to prevent cellular entry or reducing accumulation of Cu(II) has been reported as the main mechanism for tolerance (Gadd & White, 1989).…”
Section: Effect Of Cu(ii) On the Growth Of A Awamorimentioning
confidence: 99%
“…Recent studies have shown that certain bacteria, archaea as well as fungi, are able to precipitate and deposit crystalline and amorphous material in and around their cell walls and surface layers. These minerals of biogenic origin include carbonates, oxalates, hydroxides, phosphates and sulfides (Burford et al 2003a;Burford et al 2003b;Burford et al 2006;Benzerara et al 2011). Fungi and bacteria can effectively oxidize and precipitate Mn(II) and Fe(II) (de Rome and Gadd, 1987;Morley and Gadd, 1995;Spilde et al 2005;Barton and Northup, 2007).…”
Section: Introductionmentioning
confidence: 99%