Hypolithic communities shape soils and organic matter reservoirs in the ice-free landscapes of East Antarctica.

The soils of East Antarctica have no rhizosphere with the bulk of organo-mineral interactions confined to the thin microbial and cryptogamic crusts that occur in open or cryptic niches and are collectively known as biological soil crust (BSC). Here we demonstrate that cryptic hypolithic varieties of BSC in the Larsemann Hills of East Antarctica contribute to the buildup of soil organic matter and produce several types of continuous organogenous horizons within the topsoil with documented clusters of at least 100 m. Such hypolithic horizons accumulate 0.

[Diversity and viability of prokaryotes in primitive soils of the larsemann oasis (East Antarctica)].

The diversity and viability of prokaryotic communities in the primitive organomineral soils of East Antarctica have been studied; it has been shown that the total number of bacteria is smaller than and the viability of bacteria is similar to that in soils of the temperate zone. The prokaryotic communities are characterized by the occurrence of a major part of cells in filterable forms, which is higher than the analogous parameter for the temperate soils. The method of fluorescence in situ hybridization (FISH) revealed that the distribution of the main taxons is similar to that in the temperate soils: the portion of the domain Archaea is smaller than that of the domain Bacteria; the total content of Gram-negative bacteria (the phyla Proteobacteria, Acidobacteria, and Planctomycetes) is higher than that of Gram-positive bacteria (Actinobacteria).

[Association of the strA-strB genes with plasmids and transposons in the present-day bacteria and in bacterial strains from permafrost].

Transposons closely related to the streptomycin resistance transposon of modem bacteria, Tn5393, were detected in the bacterial isolates from permafrost resistant to streptomycin. Many transposons studied were located on the medium-size plasmids with a narrow host range. None of the streptomycin-resistant strains isolated from permafrost contained small plasmids carrying the strA-strB genes and related to the broad host range plasmid RSF1010.

[Isolation of antibiotic resistance bacterial strains from East Siberia permafrost sediments].

A collection of bacterial antibiotic resistance strains isolated from arctic permafrost subsoil sediments of various age and genesis was created. The collection included approximately 100 strains of Gram-positive (Firmicutes, Arthrobacter) and Gram-negative bacteria (Bacteroidetes, gamma-Proteobacteria, and alpha-Proteobacteria) resistant to aminoglycoside antibiotics (gentamycin, kanamycin, and streptomycin), chloramphenicol and tetracycline. Antibiotic resistance spectra were shown to differ in Gram-positive and Gram-negative bacteria.

Microbial populations in Antarctic permafrost: biodiversity, state, age, and implication for astrobiology.

Antarctic permafrost soils have not received as much geocryological and biological study as has been devoted to the ice sheet, though the permafrost is more stable and older and inhabited by more microbes. This makes these soils potentially more informative and a more significant microbial repository than ice sheets. Due to the stability of the subsurface physicochemical regime, Antarctic permafrost is not an extreme environment but a balanced natural one.

[Endospore formation by Streptomyces avermitilis in submerged culture].

The capability of streptomycetes to form endospores during their life cycle was studied in submerged cultures of Streptomyces avermitilis. Submerged S. avermitilis spores were most intensely formed (1) during the culture development cycles on synthetic medium CP1 with glucose under phosphate limitation, and (2) in autolysing cell suspensions of high density obtained by tenfold concentration of a stationary-phase culture grown in a synthetic medium resuspended in phosphate buffer (pH 7.

The structure of resting bacterial populations in soil and subsoil permafrost.

The structure of individual cells in microbial populations in situ of the Arctic and Antarctic permafrost was studied by scanning and transmission electron microscopy methods and compared with that of cyst-like resting forms generated under special conditions by the non-spore-forming bacteria Arthrobacter and Micrococcus isolated from the permafrost. Electron microscopy examination of microorganisms in situ revealed several types of bacterial cells having no signs of damage, including "dwarf" curved forms similar to nanoforms. Intact bacterial cells in situ and frozen cultures of the permafrost isolates differed from vegetative cells by thickened cell walls, the altered structure of cytoplasm, and the compact nucleoid, and were similar in these features to cyst-like resting forms of non-spore-forming "permafrost" bacterial strains of Arthrobacter and Micrococcus spp.

[Resting forms of gram negative chemolithoautotrophic bacteria Thioalkalivibrio versutus and Thioalkalimicrobium aerophilum].

The haloalkaliphilic chemoautotrophic gram-negative bacteria Thioalkalivibrio versutus, strain AL2, and Thioalkalimicrobium aerophilum, strain AL3, were shown to possess the capacity to produce resting forms, namely cyst-like refractile cells (CRC), whose production was controlled by the level of the d1 extracellular factors, exhibiting the function of anabiosis autoinducers. The conditions were elucidated that promoted the formation of CRC in the developmental cycles of the cultures studied, in condensed cell suspensions undergoing autolysis, and under the action of exogenously introduced chemical analogues of anabiosis autoinducers (alkylhydroxybenzenes). The peculiarities of the fine structure of the resting cells obtained were studied.

[Mercury-resistant bacteria from permafrost sediments and prospects for their use in comparative studies of mercury resistance determinants].

Mercury-resistant bacteria were isolated from permafrost sediments of Kolyma lowland and Canada existing over five thousand to two million years. Their content was shown to vary within the range 0.001-2.

[Synthesis of anabiosis autoinducers in non-spore-forming bacteria as a mechanism regulating their activity in soil and subsoil sedimentary rocks].

Non-spore-forming bacteria of the genera Arthrobacter and Micrococcus, isolated from permafrost subsoil, were found to produce greater amounts of the d1 extracellular factor than closely related collection strains isolated from soil. The effect of this factor, responsible for cell transition to anabiosis, was not species-specific. Thus, the d1 crude preparation isolated from the culture liquid of the permafrost isolate Arthrobacter globiformis 245 produced an effect on the collection strain Arthrobacter globiformis B-1112 and also on Micrococcus luteus and Bacillus cereus.

[Formation of resting forms of Arthrobacter globiformis in autolysing cell suspensions].

Under conditions of spontaneous or induced autolysis of thick cell suspensions, Arthrobacter globiformis strains produced cells exhibiting features typical of resting microbial forms. The number of viable resting cells was greater under conditions of induced rather than spontaneous autolysis. The thermoresistance of the resting cells of A.

[Reproductive resting forms of Arthrobacter globiformis].

Submerged cultures of Arthrobacter globiformis grown in media unbalanced with respect to carbon and nitrogen sources were found to contain cells exhibiting features typical of resting forms: long-term viability, specific ultrastructure, dormant metabolism, and thermoresistance. Such cells were produced not only in the collection strain VKM B-1112, but also in the A. globiformis strains isolated from 2- to 3-million-year-old permafrost sediments.

Preservation of cell structures in permafrost: a model for exobiology.

The present report is the first contribution toward a comprehensive fine-structural study of microbial cells from permafrost. Prokaryotes with a variety of cell wall types demonstrate high stability of cell structure after long-term cryopreservation in frozen soils and sediments of the Arctic. The surface capsular layers that were a salient feature of the cells both in situ and on nutrient media may be an adaptation to low temperature.

[Extracellular alkaline ribonucleases produced by Bacilli strains from the permafrost of the Kolyma lowland].

Aerobic spore-forming bacteria were isolated from the permafrost of the Kolyma lowland. Two strains of bacilli are shown to produce a relatively large amount of extracellular low-molecular weight alkaline RNases. The N-terminal amino acid sequences of the RNases secreted by these strains are similar.

Cryoprotective properties of water in the Earth cryolithosphere and its role in exobiology.

In permanently frozen rocks, water occurs in all the three phases and plays a dual role from the biological point of view. About 93-98% of it is in the solid state. This, alongside with negative temperatures, contributes to cell cryoconservation.

[Comparative electron microscopic study of cultures of Nocardia asteroides and of the Nocardia-like variant, Actinomyces chrysomallus].

The ultrastructural organization of the red-orange cultures of Nocardia (Proactinomyces) asteroides was compared with that of a Nocardia-like variant of Actinomyces (Streptomyces) chrysomallus isolated upon the inoculation of the submerged parent culture. The comparison has demonstrated for the first time that the major difference consists in the structure of their cross partitions. In Nocardia, the septa is split at all stages of its formation; in the Nocardia-like variant, the partitions have the same structure as the cultures of the genus Actinomyces (Streptomyces).

Fine structure of vegetative mycelium and spores of Nocardia spp.

The fine structure of a fragmenting and sporulating mycelium of cultures of actinomycetes possessing biochemical properties characteristic of the genus Nocardia--a cell wall of type IV and lipid LCN a--was studied. It was found that fragmenting hyphae are similar in structure to the vegetative hyphae of known actinomycetes. Sporulation takes place through the simultaneous division of a sporulating hypha by numerous septa.

[New elementary structures of actinomycete spores of the genera Actinomadura and Streptomyces].

The structure of spore surfaces was studied by electron microscopy in five species of actinomycetes, and two new types of elementary surface structures were discovered. The surface of spores in Streptomyces regensis consists of long flexible, closely interwoven, band-like structures 25 A wide. Ring-like structures 140--150 A in diameter can be observed on spores of Actinomadura verrucosospora; their clusters resemble grapes and the spore silhouette looks like a cone.

[Electron microscopic structure of the mycelium of Actinomyces chrysomallus, the producer of the antibiotic chrysomallin, during the stab fermentation process].

Ultrastructural changes in the mycelium of Actinomyces (Streptomyces) chrysomallus 2703 producing the antibiotic chrysomallin in the process of submerged fermentation are described. When the antibiotic was produced at a high rate, most hyphae remained viable for a long period of time and had the ultrastructure typical of the young cells of actinomycetes. At the same time, a number of degenerative changes due to aging were observed; these resulted in autolysis.

[Electron microscopic study of spore formation in Actinomadura verrucosospora].

The formation of spores was studied with a morphologic type of the Actinomadura genus, Acd. verrucosospora (Nonomura a. Ohara, 1971.

[Fine structure of the vegetative and spore-forming hyphae of Micropolyspora fascifera].

Changes in the fine structure of the hyphae were studied in the course of spore formation by Micropolyspora fascifera. Sporulating hyphae differ from vegetative hyphae by a less dense cytoplasm, a large zone of the nucleoid with distinctly fibrillar structure, and a thin layerless cell wall. Spore formation is accompanied with autolysis of the vegetative hyphae, which consists in vacuolization of the hyphae and appearance of a large number of tubular membrane structures within them.