Haloarchaeal diversity in 23, 121 and 419 MYA salts.

DNA was extracted from surface-sterilized salt of different geological ages (23, 121, 419 million years of age, MYA) to investigate haloarchaeal diversity. Only Haloarcula and Halorubrum DNA was found in 23 MYA salt. Older crystals contained unclassified groups and Halobacterium. The older crystals yielded a unique 55-bp insert within the 16S rRNA V2 region. The secondary structure of the V2 region completely differed from that in haloarchaea of modern environments. The DNA demonstrates that unknown haloarchaea and the Halobacterium were key components in ancient hypersaline environments. Halorubrum and Haloarcula appear to be a dominant group in relatively modern hypersaline habitats.

Limits imposed by ionizing radiation on the long-term survival of trapped bacterial spores: beta radiation.

PURPOSE: A model is presented for determining the survival time T(F) of a fraction F of a population of bacterial spores trapped within a fluid inclusion and subject to genetic damage from beta radiation. METHODS: The limiting factor to survival is the production of double-strand breaks (DSB) in the DNA resulting from single-track cleaving and from the cumulative effects of single-strand breaks (SSB) induced by the presence of ionizing radiation in the environment. The model considers the probability that radicals and ions formed by the passage of high-energy particles will interact with a DNA molecule and induce damage. RESULTS: The survival time T(F) for a fraction F of a trapped population is a weak function of both F and the length L in base pairs of the genome. For irradiation due to a beta source trapped with the spores within the inclusion, the survival time is also inversely proportional to the concentration of the radionuclide, the dominant factor in limiting survival time. CONCLUSIONS: The predictions of the model are consistent with measured DSB formation rates, the observed survival of trapped spores over time periods as long as 250 Ma, and track structure models which address low physical dose rates.

The question of uniqueness of ancient bacteria.

Microorganisms are associated with a variety of ancient geological materials. However, conclusive proof that these organisms are as old as the geological material and not more recent introductions has generally been lacking. Over the years, numerous reports of the isolation of ancient bacteria from geological materials have appeared. Most of these have suffered from the fact that the protocol for the surface sterilization of the sample was either poorly defined, inadequate or rarely included data to validate the overall effectiveness of the sterilization protocol. With proper sterility validation and isolation protocol, a legitimate claim for the isolation of an ancient microbe can be made. Biochemical, physiological, or morphological data indicate that these ancient microbes are not significantly different from modern isolates. As the role (decomposition) of modern and ancient microbes has not changed over time, it is probably unreasonable to expect these organisms to be vastly different. A discussion on the reasons for the homogeneity of ancient and modern microbes is presented.

Isolation of a 250 million-year-old halotolerant bacterium from a primary salt crystal.

Bacteria have been found associated with a variety of ancient samples, however few studies are generally accepted due to questions about sample quality and contamination. When Cano and Borucki isolated a strain of Bacillus sphaericus from an extinct bee trapped in 25-30 million-year-old amber, careful sample selection and stringent sterilization techniques were the keys to acceptance. Here we report the isolation and growth of a previously unrecognized spore-forming bacterium (Bacillus species, designated 2-9-3) from a brine inclusion within a 250 million-year-old salt crystal from the Permian Salado Formation. Complete gene sequences of the 16S ribosomal DNA show that the organism is part of the lineage of Bacillus marismortui and Virgibacillus pantothenticus. Delicate crystal structures and sedimentary features indicate the salt has not recrystallized since formation. Samples were rejected if brine inclusions showed physical signs of possible contamination. Surfaces of salt crystal samples were sterilized with strong alkali and acid before extracting brines from inclusions. Sterilization procedures reduce the probability of contamination to less than 1 in 10(9).

Haloterrigena thermotolerans sp. nov., a halophilic archaeon from Puerto Rico.

An extremely halophilic Archaeon belonging to the order Halobacteriales was isolated from the solar salterns of Cabo Rojo, Puerto Rico. The organism, designated strain PR5T, is rod-shaped, non-motile and requires at least 12% (w/v) NaCl to grow. The strain is highly thermotolerant: its temperature optimum is 50 degrees C and growth is possible up to 60 degrees C. Polar lipid analysis revealed the presence of the bis-sulfated glycolipid S2-DGD-1 as sole glycolipid and the absence of the glycerol diether analogue of phosphatidylglycerosulfate. Both C20,C20 and C20,C25 core lipids are present. The G+C content of the DNA is 63.3 mol%. According to 16S rDNA sequence data, strain PR5T is closely related to the representatives of the genera Haloterrigena and Natrinema, but on the basis of its phenotypic properties, 16S rDNA sequence and DNA-DNA hybridization studies, strain PR5T cannot be assigned to any of the recognized species within these genera. On the basis of its polar lipid composition, the isolate has been assigned to the genus Haloterrigena. The creation of a new species, Haloterrigena thermotolerans, is therefore proposed to accommodate this isolate. The type strain is strain PR5T (= DSM 11552T = ATCC 700275T).

Halogeometricum borinquense gen. nov., sp. nov., a novel halophilic archaeon from Puerto Rico.

A novel extremely halophilic archaeon was isolated from the solar salterns of Cabo Rojo, Puerto Rico. The organism is very pleomorphic, motile and requires at least 8% (w/v) NaCl to grow. Polar lipid composition revealed the presence of a novel non-sulfate-containing glycolipid and the absence of the glycerol diether analogue of phosphatidylglycerosulfate. The G + C content of the DNA is 59 mol%. On the basis of 16S rRNA sequence data, the new isolate cannot be classified in one of the recognized genera, but occupies a position that is distantly related to the genus Haloferax. All these features justify the creation of a new genus and a new species for the family Halobacteriaceae, order Halobacteriales. The name Halogeometricum borinquense gen. nov., sp. nov. is proposed. The type strain is ATCC 700274T.

Distribution and diversity of halophilic bacteria in a subsurface salt formation.

The Waste Isolation Pilot Plant (WIPP) is a salt mine constructed 650 meters below the ground surface by the United States Department of Energy. The facility will be used for permanent disposal of transuranic wastes. This underground repository has been constructed in the geologically stable Permian age Salado salt formation. Of the wastes to be placed into the facility, 85% will be biodegradable cellulose. A 3-year survey of the bacterial populations existing within the facility was conducted. Bacterial populations were found to be heterogeneously distributed throughout the mine. Populations in some mine areas reached as high as 1.0 x 10(4) colony-forming units per gram of NaCl. The heterogeneous distribution of bacteria within the mine did not follow any recognizable pattern related to either age of the workings or to human activity. A biochemical comparison between ten known species of halophilic bacteria, and strains isolated from both the mine and nearby surface hypersaline lakes, showed the presence of extreme halophiles with wide biochemical diversity, some of which could prove to represent previously undescribed groups. The halophilic bacteria isolated from the mine were found to degrade cellulose and a wide variety of other carbon compounds. When exposed to two types of common laboratory paper, the cellulose-degrading halophiles attached to the substrate within 30 minutes of inoculation. Cultures enriched directly from a brine seep in the mine easily destroyed both papers and produced detectable amounts of oxalacetic and pyruvic acids. The combination of heterogeneity in the distribution of organisms, the presence of a physiologically diverse community, and the relatively slow metabolism of cellulose may explain several long-standing debates about the existence of microorganisms in ancient underground salt formations.

Description of two new species of Halomonas: Halomonas israelensis sp.nov. and Halomonas canadensis sp.nov.

Six well-known strains of halotolerant bacteria, including two strains previously identified only as NRCC 41227 and Ba1, have been compared using 125 phenotypic characters and DNA-DNA hybridization. Although these strains represent some of the most heavily studied salt-tolerant bacteria, they have never been taxonomically compared. The data presented show that these bacteria form a relatively homogeneous group related at the genus level. The taxonomic comparison showed that these six organisms represented four distinct species all related above the 65% Jaccard coefficient level. In addition to two previously identified bacterial species, Halomonas elongata (ATCC 33173T) and Halomonas halodurans (ATCC 29686T), the strains included in this study represent two previously unnamed Halomonas species. These two new taxa have been assigned the names Halomonas israelensis (ATCC 43985T) and Halomonas canadensis (NRCC 41227T = ATCC 43984). DNA-DNA hybridization show that these two species are related to the type species H. elongata at 54.9 and 48.9%, respectively.

Changes in the hydrophobic-hydrophilic cell surface character of Halomonas elongata in response to NaCl.

Phase-partitioning studies of the euryhaline bacterium Halomonas elongata demonstrated that the hydrophobic-hydrophilic nature of the cell surface changed as the bacterium grew in different NaCl concentrations. Mid-log-phase cells grown in a high (3.4 M) NaCl concentration were more hydrophilic than were cells grown in a low (0.05 M) NaCl concentration. Mid-log-phase cells from defined medium containing 3.4 M NaCl normally produced a hydrophobicity reading of only 14 (hexadecane hydrophobicity = 100), while corresponding cells from defined medium containing 0.05M NaCl gave a hydrophobicity reading of 90. Compared with cells grown in low salt concentrations, cells grown in high salt concentrations were more hydrophilic at all stages of growth. Rapid suspension of log-phase cells grown in 1.37 M NaCl into a 0.05 or 3.4 M NaCl solution produced no detectable rapid changes in surface hydrophobicity. These data suggest that as H. elongata adapts to different NaCl concentrations, it alters the affinity of its outermost cell surface to water.

Mechanisms of halotolerance in microorganisms.

Microorganisms have the ability to adapt to a wide range of NaCl concentrations. In general the NaCl tolerance shown by microbes far exceeds the salt tolerance of any other organism, procryote or eukaryote. There are at least three mechanisms available for adaptation to different salt concentrations. The first would be a passive one in which the cytoplasmic ion content would always equal that in the medium. A second mechanism which is used by many organisms involves concentrating compatible solutes to create an osmotic balance between the cytoplasm and the external environment. The third mechanism involves changing the cell physiology to control the movement of water allowing the cell to exist with an ionically dilute cytoplasm. This article will review the major developments and discuss the implications of increasing knowledge about salt tolerance in microorganisms.

Cell wall and phospholipid composition and their contribution to the salt tolerance of Halomonas elongata.

The salt-tolerant bacterium Halomonas elongata makes a variety of physiological adaptations in response to increases in the salt concentration of its growth medium. The cell walls become more compact and internally coherent. The overall lipid pattern shows an increased amount of negatively charged lipids. In addition, the peptidoglycan composition of H. elongata, although not changing in response to increased NaCl, contains the hydrophobic amino acid leucine which is unique among bacterial species. The results suggest that H. elongata is able to live in a wide variety of salt concentrations because it alters its cell physiology in ways which increase both structural integrity and the amount of less-mobile, "structured" cell water, making the cells less susceptible to NaCl-induced dehydration.

Effects of NaCl on the uptake of alpha-[14C]aminoisobutyric acid by the halotolerant bacterium Halomonas elongata.

The alpha-aminoisobutyric acid (AIB) transport system of the halotolerant bacterium, Halomonas elongata, was examined. Cells were grown in L-alanine defined medium with 0.05, 0.375, 1.37, 2.5, or 3.4 M NaCl. Each group of cells was resuspended in buffered salts with different NaCl concentrations (0.05, 0.375, 1.37, 2.5, and 3.4 M) and the uptake of alpha-[14C]AIB was measured. Optimum AIB uptake occurred in the 0.375 M NaCl solution for the lower salt grown cells and the 1.37 M NaCl solution for the higher salt grown cells. When cells were grown in the higher salt media and suspended in hypoosmotic solutions, appreciable AIB uptake occurred; but for cells grown in lower salt media and suspended in hyperosmotic solutions, the uptake was dramatically reduced. This effect was mainly attributed to cell plasmolysis which in turn resulted in some cell death. The AIB uptake was Na+ specific and this analogue was not metabolized after being transported into the cells. An amino acid competition study gave a pattern similar to that of a marine bacterium.