Diverse cellulolytic bacteria isolated from the high humus, alkaline-saline chinampa soils

Aiming at learning the functional bacterial community in the high humus content, saline-alkaline soils of chinampas, the cellulolytic bacteria were quantified and 100 bacterial isolates were isolated and characterized in the present study. Analysis of 16S-23S IGS (intergenic spacer) RFLP (restriction fragment length polymorphism) grouped the isolates into 48 IGS types and phylogenetic analysis of 16S rRNA genes identified them into 42 phylospecies within 29 genera and higher taxa belonging to the phyla Actinobacteria, Firmicutes and Proteobacteria, dominated by the genera Arthrobacter, Streptomyces, Bacillus, Pseudomonas, Pseudoxanthomonas and Stenotrophomonas. Among these bacteria, 63 isolates represent 26 novel putative species or higher taxa, while 37 were members of 17 defined species according to the phylogenetic relationships of 16S rRNA gene. Except for the novel species, the cellulolytic activity was not reported previously in 9 of the 17 species. They degraded cellulose in medium at pH?4.5–10.0 or supplied with NaCl up to 9 %. In addition, 84.8 and 71.7 % of them degraded xylan and Avicel, respectively. These results greatly improved the knowledge about the diversity of cellulolytic bacteria and demonstrated that the chinampa soils contain diverse and novel cellulolytic bacteria functioning at a wide range of pH and salinity levels, which might be a valuable biotechnological resource for biotransformation of cellulose.     

Characterization and comparison of potential denitrifiers in microbial mats from King George Island,Maritime Antarctica

Cyanobacterial microbial mats are highly structured communities commonly found in Antarctic inland waters including melt streams. These benthic microbial associations comprise a large number of microorganisms with different metabolic capacities, impacting nutrient dynamics where established. The denitrification process is a feasible nitrogen loss pathway and a biological source of nitrous oxide, a potent greenhouse gas that also promotes ozone depletion. Potential denitrifiers from five microbial mats were characterized using a PCR-DGGE (denaturing gradient gel electrophoresis) approach. Molecular markers encoding for key enzymes in the denitrification process (nirK, nirS and nosZ) were used. Fingerprints were obtained for the five sampled mats and compared for two successive years. Distance analysis showed that despite the sampled year, the denitrifying genetic potential was similar between most of the sites when represented in Euclidean space. The number of dominant denitrifiers detected for each sample ranged between 6 and 18 for nirK, 4–10 for nirS and 6–17 for nosZ. The seventy-two sequenced phylotypes showed 80–98 % identity to previously reported environmental sequences from water column, sediments and soil samples. These results suggest that Antarctic microbial mats have a large denitrification potential, previously uncharacterized and composed by both site-specific and common phylotypes belonging mainly to Alpha-, Beta- and Gammaproteobacteria.     

Ecological indicators of habitat and biodiversity in a Neotropical landscape: multitaxonomic perspective

Ecological indicators of habitat and biodiversity in a Neotropical landscape: multitaxonomic perspective. The use of indicator species to characterize specific ecological areas is of high importance in conservation/restoration biology. The objective of this study was to identify indicator species of diverse taxa that characterize different landscape units, and to better understand how management alters species composition. We identified two ecomosaics, tropical rain forest and the agricultural matrix, each one comprised of four landscape units. The taxonomic groups studied included birds (highly mobile), butterflies (moderately mobile), terrestrial gastropods (less mobile) and trees (sessile). Sampling efficiency for both ecomosaics was > or = 86%. We found 50 mollusks, 74 butterflies, 218 birds and 172 tree species, for a total of 514 species. Using ordination and cluster analysis, we distinguished three habitat types in the landscape: tropical rainforest, secondary vegetation and pastures with scattered trees and live fences. The InVal (> or = 50%) method identified 107 indicator species, including 45 tree species, 38 birds, 14 butterflies and 10 gastropods. Of these, 35 trees, 10 birds, four butterflies and eight gastropods were forest indicators. Additionally, 10, 28, 10 and two species, respectively per group, were characteristic of the agricultural matrix. Our results revealed a pattern of diversity decrease of indicator species along the rainforest-secondary forest-pasture gradient. In the forest, the gastropods Carychium exiguum, Coelocentrum turris, Glyphyalinia aff. indentata y Helicina oweniana were significantly correlated (p < 0.05) with 90% of the other groups of flora and fauna indicator species. These findings suggest that gastropods may be good indicators of forest habitat quality and biodiversity. The secondary vegetation is an intermediate disturbance phase that fosters high diversity in the agricultural matrix. We exemplify a multitaxa approach, including mesofauna, for ecological monitoring of agricultural landscapes.     

Mineralization of 14C-labelled maize in alkaline saline soils

The turnover of organic material determines the availability of plant nutrients in unfertilized soils, and this applies particularly to the alkaline saline soil of the former Lake Texcoco in Mexico. Uniformly labelled [¹⁴C] maize and its neutral detergent fibre (NDF) fraction, mainly containing cellulose and hemi-cellulose, were added to these soils to investigate dynamics of C and N and the importance of the NDF fraction. Soil with electrolytic conductivity (EC) of 1.2, 3.2, 24.6 and 32.7 dS m^–1 was incubated aerobically, while CO₂ and ¹⁴CO₂ production, and inorganic N dynamics (NH₄ ⁺, NO₂ ^–, NO₃ ^–) were monitored. The amount of ¹⁴C-labelled maize mineralized after 97 days was >500 mg C kg^–1 dry soil (D.S.) of the 1000 mg C kg^–1 D.S. added in soils with EC 24.6 dS m^–1, but only 257 mg C kg^–1 D.S. in soil with EC 32.7 dS m^–1. The decomposition of the NDF fraction showed a lag, greatest in the soil with the largest EC and the amount of ¹⁴C-labelled NDF fraction mineralized after 97 days was > 300 mg C kg^–1 D.S. in soils with EC 3.2 dS m^–1, but in the soil with EC 32.7 dS m^–1 it was only 118 mg C kg^–1D.S. Application of ¹⁴C-labelled maize and the NDF fraction induced a priming effect, most accentuated at the onset of the incubation. The ratio between the amount of CO₂ produced due to the priming effect and the ¹⁴CO₂ produced was 16-times larger when 250 mg maize-C kg^–1 D.S. was added and only 3-times when 2000 mg maize-C kg^–1 D.S. was added. Oxidation of NO₂ ^– occurred in soil with EC 32.7 dS m^–1 as witnessed by decreases in concentration of NO₂ ^– and increases in concentration of NO₃ ^–. It was found that EC affected the decomposition of maize, the NDF fraction and the priming effect. Decomposition of cellulose and oxidation of NO₂ ^– occurred in soil with EC 32.7 dS m^–1 although cellulolytic micro-organisms and autotrophic NO₂ ^– oxidizers could previously not be isolated from this soil.     

Bacterial Communities in Soil Under Moss and Lichen-Moss Crusts

Biological soil crusts are symbiotic microbial communities formed by green algae, mosses, fungi, lichens, cyanobacteria and bacteria in different proportions. Crusts contribute to soil fertility and favour water retention and infiltration. However, little is known about the bacterial community structure in soil under the crusts. Soil was sampled under a moss crust (considered the MOSS group), lichen plus moss (considered the LICHEN group) and bare soil (considered the BARE group) and the microbial communities determined using nearly full 16S rRNA gene libraries. Bacteria belonging to seven different phyla were found and the Acidobacteria and Alphaproteobacteria were the dominant in each group. The crusts affected negatively the abundance of the Burkholderiales. The phylogenetic diversity and bacterial community membership were different in the LICHEN group compared to the BARE and MOSS groups, but not species richness and community structure. The beta diversity analysis also revealed a different bacterial community structure beneath the LICHEN and MOSS crusts, suggesting species-specific influence. This is a first insight into the effect of a biological soil crust on the bacterial community structure in an organic matter rich soil of a high altitude mountain forest.