2002
DOI: 10.1002/jctb.736
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Metal sorption by biomass of melanin‐producing fungi grown in clay‐containing medium

Abstract: The sorption of toxic metals by fungal mycelia grown in clay-containing medium is reported in this work. Biomass of melanin-producing microfungi of the genus Cladosporium (C cladosporioides, C resinae and C herbarum) and Aureobasidium pullulans, clay minerals and fungal mycelia grown in clay-containing medium were compared for their equilibrium Cu and Cd uptake from pHbuffered solutions using experimental sorption isotherms. Bentonite (Cherkassy) in the natural form was shown to be the best Cu sorbent compared… Show more

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Cited by 62 publications
(37 citation statements)
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“…B. exigua, showed a strong melanization in these conditions. Melanization in fungi is a typical stress response [76] and, has been mentioned to be involved in metal biosorption as a strategy to immobilize toxic metals [77,78]. All four strains of the two BFI couples were confirmed as urea-positive and no inhibition effect was present in urea-containing media.…”
Section: Discussionmentioning
confidence: 99%
“…B. exigua, showed a strong melanization in these conditions. Melanization in fungi is a typical stress response [76] and, has been mentioned to be involved in metal biosorption as a strategy to immobilize toxic metals [77,78]. All four strains of the two BFI couples were confirmed as urea-positive and no inhibition effect was present in urea-containing media.…”
Section: Discussionmentioning
confidence: 99%
“…Direct biophysical effects have been shown where fungal hyphae attracted and oriented clay platelets because of surface charge phenomena, and acted as nucleation zones for the formation of narrow clay-lined channels (Ritz & Young, 2004). Interactions between clay minerals and microbes alter the adsorptive properties of both clays and biomass (Fomina & Gadd, 2002b). Under certain conditions, the sorption abilities of microbe-clay aggregates can be decreased due to blocking and masking of binding sites or increased due to modification of binding sites and emergence of new ones (Fomina & Gadd, 2002b;Tazaki, 2006).…”
Section: Bioweathering Of Rocks and Minerals: Soil Formationmentioning
confidence: 99%
“…Interactions between clay minerals and microbes alter the adsorptive properties of both clays and biomass (Fomina & Gadd, 2002b). Under certain conditions, the sorption abilities of microbe-clay aggregates can be decreased due to blocking and masking of binding sites or increased due to modification of binding sites and emergence of new ones (Fomina & Gadd, 2002b;Tazaki, 2006). As well as being important in stages of mineral soil and sediment formation and development, bioweathering mechanisms also effect structural decay of rock and mineral-based building materials, monuments and other structures.…”
Section: Bioweathering Of Rocks and Minerals: Soil Formationmentioning
confidence: 99%
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“…Because of its recalcitrance, its requirement for oxidative enzymes for degradation, and the large variation in concentrations across fungal species, melanin in fungal tissues may be analogous to lignin in plant tissues in biochemical control of necromass decomposition. Additionally, melanized hyphae also have higher sorption to soil mineral components compared to hyaline hyphae (Fomina and Gadd, 2003), which may result in physiochemical protection of necromass C, which would also result in increased incorporation into stable SOM (Fernandez and Kennedy, 2015).…”
Section: Melaninmentioning
confidence: 99%