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Literature summary for 3.1.6.1 extracted from
- Controls on soil arylsulfatase activity at a regional scale (2019), Eur. J. Soil Biol., 90, 9-14 .
No PubMed abstract available
Organism
| Organism | UniProt | Comment | Textmining |
|---|---|---|---|
| uncultured soil bacterium | - |
- |
- |
General Information
| General Information | Comment | Organism |
|---|---|---|
| metabolism | in southwest China, soil arylsulfatase activity increases from cropland through to forest following post-agriculture succession, and is significantly lower in clasolite than in dolomite or limestone. Among 14 studied soil variables, soil pH, exchangeable calcium, organic carbon, clay and silt showed significant non-linear relationships with arylsulfatase activity. The activity of soil arylsulfatase is most controlled by soil pH and soil texture, but soil calcium and organic carbon only have indirect or spurious effects on arylsulfatase activity | uncultured soil bacterium |
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Release 2023.1 (January 2023)
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