Assessment of the competitiveness of fast-growing rhizobia infectingAcacia senegal using antibiotic resistance and melanin production as identification markers

The competitiveness of fourRhizobium sp. strains infectingAcacia senegal and originating in the Sudan was assessed in a growth chamber experiment using Sudanese soil, WhenAcacia senegal was inoculated with pure cultures of the strains, there were statistically significant differences among the strains with respect to the numbers of nodules formed, the amount of dry matter produced and acetylene reduction activity. However, the best strain when applied as a pure culture, was only the second best as a competitor. Two strains with inferior symbiotic capabilities were also bad competitors but nevertheless reduced the yields of the plants when they were applied as inocula mixed with the better strains. The bacterial markers used to assess nodule occupancy were resistance to streptomycin or spectinomycin. Two of the strains formed the dark-brown pigment melanin. Melanin production was a stable characeristic, well suited to serve as an intrinsic identification marker when assessing the competitiveness of melanin-producing versus non-producing strains in controlled conditions.     

Alteration of lipopolysaccharide and protein profiles in SDS-PAGE of rhizobia by osmotic and heat stress

The effects of osmotic and heat stress on lipopolysaccharides and proteins of rhizobia isolated from the root nodules of leguminous trees grown in semi-arid soils of the Sudan, and of agricultural legumes grown in salt-affected soils of Egypt, were determined by SDS-PAGE. The rhizobia were of three types: (1) sensitive strains, unable to grow in 3% (w/v) NaCl in yeast mannitol medium; (2) tolerant strains which could grow in 3% (w/v) NaCl; and (3) halophytic strains which grew with 3 to 10% (w/v) NaCl. The sensitive strains changed their gel pattern or the amount of lipopolysaccharide they synthesized when grown in 1% (w/v) NaCl. The tolerant and halophytic strains often modified their lipopolysaccharides in 3% NaCl, which was evident by a shift in the banding patterns towards longer chain length. Similar effects were observed in cells incubated with sucrose and, to a lesser extent, in cells incubated at growth temperatures near the recorded maximum temperature for growth. The stress-induced changes in lipopolysaccharides were not associated with specific banding patterns of the lipopolysaccharides. During incubation in medium containing elevated concentrations of NaCl or sucrose, the protein patterns of the rhizobia were also changed. A protein with relative mobility of 65 kDa appeared during temperature stress. The maximum growth temperature of the Sudanese rhizobia were up to 44.2°C.H.H. Zahran and M. Karsisto were and L.A. Räsänen and K. Lindström are with the Department of Applied Chemistry and Microbiology, University of Helsinki, POB 27, SF-00014 University of Helsinki, Finland. H.H. Zahran is now with the Department of Botany, Faculty of Science, Beni-Suef, Egypt. M. Karsisto is now with the Finnish Forest Research Institute, PL 18, SF-01301 Vantaa, Finland.     

Relationship between decomposition of cellulose strips and chemical properties of humus layer in natural boreal forests

The relationships between the decomposition of cellulose strips buried completely within the humus layer (Of + Oh) for two 1-year periods and humus layer properties were studied at forested sites with minimal anthropogenic influence. The 18 study sites are clustered in four catchments located between 61° and 69° N in Finland. The stands were composed of varying proportions of Scots pine, Norway spruce and deciduous species. Of the 23 humus layer properties studied, significant correlations were found between decomposition and soil pH, effective cation exchange capacity, base saturation, C/N ratio, the concentrations of P, Mn, Pb, Zn and Cu. The relationships, however, were inconsistent except for heavy metal concentrations which were positive in all cases. Decomposition was more strongly and consistently correlated to tree stand characteristics (mean height and stem volume) than to the humus layer properties. Both the decomposition of cellulose strips and the concentrations of heavy metals were intercorrelated with climate and the stand characteristics. Partial correlation analysis revealed that the relationships between decomposition and humus layer heavy metal concentrations were more strongly affected by the tree stand characteristics than by climate. After the statistical elimination of the effects of stand characteristics, no significant positive correlations between decomposition and humus layer heavy metal concentrations remained and, in some cases for total and extractable Zn, the correlations became significant and negative. Results from litterfall chemistry (nutrients and heavy metals) also underlined that any specific effects of humus layer heavy metal concentrations on decomposition may be masked if the effects of stand characteristics are not accounted for. We conclude that the relationships between decomposition and soil chemical properties can not be elucidated without considering stand structure and composition of the forest stand.     

Post-drainage changes in vegetation composition and carbon balance in Lakkasuo mire,Central Finland

The post-drainage changes in vegetation composition and carbon balance were studied on four site types (from minero- to ombrotrophic conditions) in Lakkasuo mire, central Finland, by directly comparing undrained and drained parts (30 years ago) of the mire. Drainage had drastically changed the species composition of the sites, especially at the minerotrophic sites, where almost all Sphagna had been replaced by forest mosses. On the ombrotrophic sites much of the mire vegetation still remained 30 years after drainage. Drainage had decreased the C stores in ground vegetation on the minerotrophic sites but increased them on the ombrotrophic sites. The changes were, however, very small compared to the changes in the tree stand, where the C stores had increased at all sites (increasing with nutrient level). The change in peat C balance over the 30-year post-drainage period was negative on the most nutrient-rich site, and positive on the others, increasing with lower nutrient levels. The decrease in the peat C balance on the most nutrient-rich site was compensated by the greater increase in the tree stand C stores and the changes in the total C balance (peat+tree stand+ground vegetation) remained positive on all sites. This revised version was published online in June 2006 with corrections to the Cover Date.