Long-term fertilization affects the abundance of saprotrophic microfungi degrading resistant forms of soil organic matter
Language English Country United States Media print
Document type Journal Article, Research Support, Non-U.S. Gov't
PubMed
12744081
DOI
10.1007/bf02931280
Knihovny.cz E-resources
- MeSH
- Actinomyces isolation & purification metabolism MeSH
- Bacteria isolation & purification metabolism MeSH
- Benzopyrans metabolism MeSH
- Biodegradation, Environmental MeSH
- Fungi isolation & purification metabolism MeSH
- Microbiological Techniques MeSH
- Minerals MeSH
- Organic Chemicals metabolism MeSH
- Colony Count, Microbial MeSH
- Fertilizers * MeSH
- Soil analysis MeSH
- Soil Microbiology * MeSH
- Publication type
- Journal Article MeSH
- Research Support, Non-U.S. Gov't MeSH
- Names of Substances
- Benzopyrans MeSH
- fulvic acid MeSH Browser
- Minerals MeSH
- Organic Chemicals MeSH
- Fertilizers * MeSH
- Soil MeSH
The effect of mineral and organic fertilization on the occurrence of soil microorganisms was determined in a field experiment. The colony-forming unit counts of saprotrophic microfungi, when estimated on a silicate gel medium containing fulvic acid as a sole carbon source, increased significantly with increasing doses of mineral and organic fertilization. Partial correlation analysis indicated that, unlike bacteria and actinomycetes, microfungi utilizing fulvic acid were significantly associated with soil organic carbon. No significant effects on bacteria and microfungi counted on common microbiological media were observed but counts of actinomycetes increased in a manured soil extensively fertilized by a mineral fertilizer. Fulvic acid utilizing microfungi, which are associated with areas rich in organics, play possibly the main role in mineralization of resistant forms of soil organic matter.
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