1994
DOI: 10.1016/0964-8305(94)90006-x
|View full text |Cite
|
Sign up to set email alerts
|

Excretion of organic acids by fungal strains isolated from decayed sandstone

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
20
0

Year Published

2003
2003
2020
2020

Publication Types

Select...
3
3
1

Relationship

0
7

Authors

Journals

citations
Cited by 53 publications
(20 citation statements)
references
References 10 publications
0
20
0
Order By: Relevance
“…As no direct physical attacks by fungal hyphae or cyanobacterial filaments were observable via microscopical methods (SEM, TEM, light microscopy) within mineral samples, an indirect process resulting from microbial metabolism is suggested. For example, production of organic acids or respiration-derived CO 2 would lower the pH, which is a possible factor in biodeterioration of minerals (Delatorre et al, 1993;Gómez-Alarcón et al, 1994;Machill et al, 1997;Weber et al, 2011). The fact that pH decreased only slightly and in the same way in all experiments despite varying extent of dissolution (Figure 3) is not contradictory with this explanation as pH values in the direct micro-environment of cells between a biofilm and its substrate can differ significantly from those in the macro-environment (Bonneville et al, 2011).…”
Section: Discussionmentioning
confidence: 56%
See 1 more Smart Citation
“…As no direct physical attacks by fungal hyphae or cyanobacterial filaments were observable via microscopical methods (SEM, TEM, light microscopy) within mineral samples, an indirect process resulting from microbial metabolism is suggested. For example, production of organic acids or respiration-derived CO 2 would lower the pH, which is a possible factor in biodeterioration of minerals (Delatorre et al, 1993;Gómez-Alarcón et al, 1994;Machill et al, 1997;Weber et al, 2011). The fact that pH decreased only slightly and in the same way in all experiments despite varying extent of dissolution (Figure 3) is not contradictory with this explanation as pH values in the direct micro-environment of cells between a biofilm and its substrate can differ significantly from those in the macro-environment (Bonneville et al, 2011).…”
Section: Discussionmentioning
confidence: 56%
“…Excreted organic acids and respiration-derived CO 2 are often active in these processes (Silverman and Munoz, 1970;Delatorre et al, 1993;Gómez-Alarcón et al, 1994;Machill et al, 1997;Landeweert et al, 2001;Abdulla, 2009;Weber et al, 2011), although fungal hyphae can directly penetrate and widen fissures in rocks (Sterflinger, 2000;Gorbushina et al, 2003;Chertov et al, 2004). The extreme microbial diversity of soil organisms (Jongmans et al, 1997;Landeweert et al, 2001;Schöll et al, 2008;Abdulla, 2009;Bonneville et al, 2009;Rosling et al, 2009;Taylor et al, 2009) and accompanying macroscopic vegetation results in high rates of weathering.…”
Section: Introductionmentioning
confidence: 99%
“…Under drier conditions, the biofilms are generally grey in colour, whereas more humid areas are more frequently green [2]. Cyanobacteria were found on several materials types: concrete and stones, metals, painted surfaces and plastic [5,26,31,[38][39][40][41]. Table 1 shows the main species isolated from disfigured buildings or those that have been shown to be capable of biodeterioration.…”
Section: Cyanobacteria and Algaementioning
confidence: 99%
“…Non-biological weathering processes are increasing in last decades, especially in urban areas, owing to the higher incidence of environmental and anthropogenic pollution [3,4]. These deleterious effects on buildings and monuments are well documented [5,6]. In addition to physical and chemical problems due to weathering and soiling, the biological growth accelerates the fouling process of outdoor materials, as shown in Figs 1 and 2.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation