Fungi from Canadian coniferous forest soils

1973 ◽  
Vol 51 (12) ◽  
pp. 2275-2290 ◽  
Author(s):  
P. Widden ◽  
D. Parkinson

The fungus flora from four pine forest soils was investigated. Qualitative studies used a soil-washing method, whereas quantitative investigations were performed using a direct observation technique. Results indicate that the fungus populations on litter and humus from all four forest soils are fairly similar, with Cladosporium herbarum, Aureobasidium pullulans, Alternaria sp., and various members of the order Sphaeropsidales being common in the litter, and Trichoderma and Penicillium species increasing in frequency in the F and H layers. The fungi isolated from the mineral soil horizons were more varied in nature, but certain genera seemed to be found frequently; these included Mortierella, Chrysosporium, Oidiodendron, Paecilomyces, Cylindrocarpon, Torulomyces, and sterile dark fungi.A detailed investigation of a Pinus strobus forest at St. Williams, Ontario, revealed no distinct seasonal patterns in the relative frequencies of the species of fungi.Quantitative studies showed that, in all soils, mycelial content decreased with depth from the humus. A comparison of the four sites showed a wide variation in fungal mycelium, varying from 30 m/g dry soil under Pinus strobus (in the A1 horizon) to 1540 m/g under P. contorta during May. Seasonal data from the P. strobus forest indicate a peak in mycelial content during August.

2008 ◽  
Vol 40 (3) ◽  
pp. 669-678 ◽  
Author(s):  
Katherine E. Ludley ◽  
Clare H. Robinson ◽  
Sue Jickells ◽  
Paul M. Chamberlain ◽  
Jeanette Whitaker

1979 ◽  
Vol 57 (12) ◽  
pp. 1324-1331 ◽  
Author(s):  
Paul Widden

The fungal populations of four forest soils in southern Quebec were studied, using the soil-washing technique. Although the four forests were located on the same basal materials, the effects of planting different tree species were reflected by changes in the chemical properties of the soils. Of the fungi isolated from these soils, Gliocladium roseum, Paecilomyces carneus, P. fumosoroseus, Gliomastix murorum, Penicillium implication, P. spinulosum, P. thomii, Trichoderma hamatum, and two unidentified Trichoderma species preferred the more neutral, deciduous forest soils. However, Chrysosporium pannorum, Penicillium janthinellum, P. simplicissimum, Trichoderma viride, T. polysporum, and another unidentified Trichoderma preferred the more acidic coniferous forest soils. For other species of fungi no differences between populations in the four sites could be detected. It is concluded that a clearer understanding of the ecology of these fungi requires a more detailed analysis of the influence of seasonal and spatial changes in their physical and chemical environment on their population densities.


2015 ◽  
Vol 10 (4) ◽  
pp. 489-502
Author(s):  
Osamu TAKAHATA ◽  
Shojirou KUMADA ◽  
Junya ANDO ◽  
Shinji MIYAGUCHI ◽  
Koji ISHIYAMA ◽  
...  

1990 ◽  
Vol 128 (1) ◽  
pp. 31-44 ◽  
Author(s):  
K. Killham

1998 ◽  
Vol 78 (3) ◽  
pp. 477-479 ◽  
Author(s):  
C. J. Westman ◽  
S. Jauhiainen

Forest soil pH in southwest Finland was measured with identical sampling and analysing methods in 1970 and 1989. The acidity of the organic humus layer increased significantly as pH values measured on water and on salt suspensions decreased between the two sampling dates. For the mineral soil layers, no unambiguous trend was found. pH values measured on salt suspension tended to be unchanged or lower, while pH on water suspension in some soil layers were even higher in 1989 than in 1970. Key words: pH, repeated sampling


1980 ◽  
Vol 58 (15) ◽  
pp. 1704-1721 ◽  
Author(s):  
J. Bissett ◽  
D. Parkinson

The biomass, community composition, and metabolic activity of soil microorganisms were studied in adjacent burnt and unburnt areas of spruce–fir subalpine forest razed 6 years previously by a moderately severe natural fire. Similar levels of microbial biomass were observed at comparable burnt and unburnt sites, although the ratio of fungal to bacterial biomass was higher in the unburnt soils. The decreased acidity of the surface horizons in the burn probably tended to favor the development of a bacterial flora rather than a fungal flora. Microbial biomass in the burnt sites peaked earlier in the season than in the unburnt sites in response to the warmer soil temperatures and earlier thaw in the spring in the burn area.Significant differences in the species composition of the mycoflora in the organic soil horizons were observed between the burnt and unburnt sites. Apparently, these were related to qualitative differences in the recent litter. Phoma, Cladosporium, and Botrytis, which are usually associated with early stages of decomposition of herbaceous litter, were more common in the burnt soil. The mycoflora of the mineral soil horizons varied considerably from one burn site to another, possibly reflecting the geographical variation in the intensity of the burn. In overall composition, however, the mycoflora in the mineral soil horizons of the burn was not appreciably different from that of the unburnt sites.Higher laboratory rates of respiration and cellulose decomposition were observed for soil samples from the undisturbed forest. However, the rate of decomposition of cellulose in the field was much higher in the burnt sites, probably as a result of the higher soil temperatures in the burn area. Low soil temperature was concluded to be the main factor limiting microbial activities in the study area, and the removal of the insulating plant canopy and increased heat absorption by the ash in the burn area were found to increase decomposition rates, at least at this stage in the succession following the disturbance of fire.


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