Perennial Antarctic lake ice: an oasis for life in a polar desert.

The permanent ice covers of Antarctic lakes in the McMurdo Dry Valleys develop liquid water inclusions in response to solar heating of internal aeolian-derived sediments. The ice sediment particles serve as nutrient (inorganic and organic)-enriched microzones for the establishment of a physiologically and ecologically complex microbial consortium capable of contemporaneous photosynthesis, nitrogen fixation, and decomposition. The consortium is capable of physically and chemically establishing and modifying a relatively nutrient- and organic matter-enriched microbial "oasis" embedded in the lake ice cover.

Dilution-to-extinction culturing of psychrotolerant planktonic bacteria from permanently ice-covered lakes in the McMurdo Dry Valleys, Antarctica.

Lakes in the McMurdo Dry Valleys of Antarctica are characterized by a permanent ice cover and little or no anthropogenic influence. Although bacterial cultures have been obtained from these habitats, recent culture-independent studies indicate that the most abundant microbes in these systems are not yet cultivated. By using dilution-to-extinction cultivation methods with sterilized and nutrient-amended lake water as media, we isolated 148 chemotrophic psychrotolerant bacterial cultures from fresh surface water of Lake Fryxell and the east lobe of Lake Bonney and the hypersaline, suboxic bottom water from the west lobes of Lake Bonney. Screening of the 16S ribosomal ribonucleic acid (rRNA) genes of the cultures by restriction fragment length polymorphism (RFLP) yielded 57 putatively pure psychrotolerant, slow growing cultures grouped into 18 clusters. The sequencing of 16S rRNA genes of randomly selected representatives of each RFLP cluster revealed that the corresponding isolates belong to the Alphaproteobacteria (six RFLP patterns), Betaproteobacteria (six RFLP patterns), Bacteroidetes (four RFLP patterns), and Actinobacteria (two RFLP patterns). Phylogenetic analysis of the sequences showed that the vast majority of the isolates were not closely related to previously described species. Thirteen of 18 RFLP patterns shared a 16S ribosomal deoxyribonucleic acid sequence similarity of 97% or less with the closest described species, and four isolates had a sequence similarity of 93% or less with the nearest described species. Phylogenetic analysis showed that these sequences were representatives of deeply branching organisms in the respective phylum. A comparison of the isolates with 16S rRNA clone libraries prepared from the same environments showed substantial overlap, indicating that dilution-to-extinction culturing in natural lake water media can help isolate some of the most abundant organisms in these perennially ice-covered lakes.

Effects of imposed salinity gradients on dissimilatory arsenate reduction, sulfate reduction, and other microbial processes in sediments from two California soda lakes.

Salinity effects on microbial community structure and on potential rates of arsenate reduction, arsenite oxidation, sulfate reduction, denitrification, and methanogenesis were examined in sediment slurries from two California soda lakes. We conducted experiments with Mono Lake and Searles Lake sediments over a wide range of salt concentrations (25 to 346 g liter(-1)). With the exception of sulfate reduction, rates of all processes demonstrated an inverse relationship to total salinity. However, each of these processes persisted at low but detectable rates at salt saturation. Denaturing gradient gel electrophoresis analysis of partial 16S rRNA genes amplified from As(V) reduction slurries revealed that distinct microbial populations grew at low (25 to 50 g liter(-1)), intermediate (100 to 200 g liter(-1)), and high (>300 g liter(-1)) salinity. At intermediate and high salinities, a close relative of a cultivated As-respiring halophile was present. These results suggest that organisms adapted to more dilute conditions can remain viable at high salinity and rapidly repopulate the lake during periods of rising lake level. In contrast to As reduction, sulfate reduction in Mono Lake slurries was undetectable at salt saturation. Furthermore, sulfate reduction was excluded from Searles Lake sediments at any salinity despite the presence of abundant sulfate. Sulfate reduction occurred in Searles Lake sediment slurries only following inoculation with Mono Lake sediment, indicating the absence of sulfate-reducing flora. Experiments with borate-amended Mono Lake slurries suggest that the notably high (0.46 molal) concentration of borate in the Searles Lake brine was responsible for the exclusion of sulfate reducers from that ecosystem.

Dissimilatory arsenate and sulfate reduction in sediments of two hypersaline, arsenic-rich soda lakes: Mono and Searles Lakes, California.

A radioisotope method was devised to study bacterial respiratory reduction of arsenate in sediments. The following two arsenic-rich soda lakes in California were chosen for comparison on the basis of their different salinities: Mono Lake (approximately 90 g/liter) and Searles Lake (approximately 340 g/liter). Profiles of arsenate reduction and sulfate reduction were constructed for both lakes. Reduction of [73As]arsenate occurred at all depth intervals in the cores from Mono Lake (rate constant [k] = 0.103 to 0.04 h(-1)) and Searles Lake (k = 0.012 to 0.002 h(-1)), and the highest activities occurred in the top sections of each core. In contrast, [35S]sulfate reduction was measurable in Mono Lake (k = 7.6 x10(4) to 3.2 x 10(-6) h(-1)) but not in Searles Lake. Sediment DNA was extracted, PCR amplified, and separated by denaturing gradient gel electrophoresis (DGGE) to obtain phylogenetic markers (i.e., 16S rRNA genes) and a partial functional gene for dissimilatory arsenate reduction (arrA). The amplified arrA gene product showed a similar trend in both lakes; the signal was strongest in surface sediments and decreased to undetectable levels deeper in the sediments. More arrA gene signal was observed in Mono Lake and was detectable at a greater depth, despite the higher arsenate reduction activity observed in Searles Lake. A partial sequence (about 900 bp) was obtained for a clone (SLAS-3) that matched the dominant DGGE band found in deeper parts of the Searles Lake sample (below 3 cm), and this clone was found to be closely related to SLAS-1, a novel extremophilic arsenate respirer previously cultivated from Searles Lake.

Identification of bacterial cells by chromosomal painting.

Chromosomal painting is a technique for the microscopic localization of genetic material. It has been applied at the subcellular level to identify regions of eukaryotic chromosomes. Here we describe the development of bacterial chromosomal painting (BCP), a related technology for the identification of bacterial cells. Purified genomic DNAs from six bacterial strains were labeled by nick translation with the fluorochrome Fluor-X, Cy3, or Cy5. The average size of the labeled fragments was ca. 50 to 200 bp. The probes were hybridized to formaldehyde-fixed microbial cells attached to slides and visualized by fluorescence microscopy. In reciprocal comparisons, distantly related members of the class Proteobacteria (Escherichia coli and Oceanospirillum linum), different species of the genus Bacillus (B. subtilis and B. megaterium), and different serotypes of the subspecies Salmonella choleraesuis subsp. choleraesuis (serotype typhimurium LT2 and serotype typhi Ty2) could easily be distinguished. A combination of two probes, each labeled with a different fluorochrome, was used successfully to simultaneously identify two cell types in a mixture. Lysozyme treatment was required for the identification of Bacillus spp., and RNase digestion and pepsin digestion were found to enhance signal strength and specificity for all cell types tested. Chromosome in situ suppression, a technique that removes cross-hybridizing fragments from the probe, was necessary for the differentiation of the Salmonella serotypes but was not required to distinguish the more distantly related taxa. BCP may have applications in diverse branches of microbiology where the objective is the identification of bacterial cells.

Bacterial chromosomal painting for in situ monitoring of cultured marine bacteria.

We previously described a new method, bacterial chromosomal painting (BCP), for the in situ identification of bacterial cells. Here, we describe the application of this technique to study the ecology and physiology of cultured marine pelagic bacteria from the western Sargasso Sea (WSS). A total of 86 bacteria were isolated from seawater collected from near the surface, at a depth of 250 m and from nutrient-amended seawater incubations. The 10 bacterial isolates that were best represented in environmental genomic DNA from the WSS were selected using reverse genome probing. BCP hybridization cell counts were used to determine the depth-specific distribution of one of the alpha proteobacterial isolates, B5-6, in the WSS during two thermal stratification regimes: stratified and partially mixed. The maximum cell count measured for B5-6 at the summer deep chlorophyll maximum was approximately 4% of the total cell count. This study is the first application of BCP to natural environments.

pH and the cAMP-dependent protein kinase mediate growth phase induction of the cytochrome c oxidase subunit VI gene, COX6, in Saccharomyces cerevisiae.

Respiratory adaptation in Saccharomyces cerevisiae is a complex genetic program that ensures ATP synthesis in a glucose-depleted environment. ATP is generated during respiration by the mitochondrial electron transport chain which is induced by respiratory adaptation. We have studied the terminal enzyme in mitochondrial electron transport, cytochrome c oxidase, from S. cerevisiae. Because subunits in this multisubunit enzyme are coordinately regulated, we have focused upon the well characterized subunit VI gene, COX6. In yeast, COX6 transcription is regulated by several factors thought to mediate respiratory adaptation including growth phase induction, oxygen dependence, and glucose repression. In the present study, we found that in addition to these known regulators, COX6 expression also depends upon pH and the cAMP-dependent protein kinase which may comprise additional factors signaling respiratory adaptation.

Identification of a low specificity, oxygen, heme, and growth phase regulated DNA binding activity in Saccharomyces cerevisiae.

Cytochrome c oxidase from Saccharomyces cerevisiae is subject to intricate control at the level of transcription of the various genes encoding its subunits. Expression of the subunit VI encoding gene, COX6, is glucose repressed, growth phase induced, and dependent on oxygen and heme availability. An upstream activation region for COX6, UAS6, was found to contain a glucose responsive region, a heme dependent region (HDS1), and a binding site for the transcription factor, BAF1. BAF1 was the only factor observed to form a protein complex with UAS6 in vitro. However, we found that binding of BAF1 was unaffected by oxygen or heme regulation. In the present communication, we have identified a DNA binding activity that was growth phase induced and dependent on oxygen and heme availability. This highly regulated activity was detected by its discrete binding to the heme responsive site, HDS1, in UAS6. Nonetheless, it appears to have weak DNA binding specificity.

Oxygen regulation of the cytochrome c oxidase subunit VI gene, COX6, in Saccharomyces cerevisiae.

Cytochrome c oxidase (CcO) in Saccharomyces cerevisiae is subject to intricate physiological control. Growth phase, carbon source, and oxygen level are three well recognized modulators of CcO expression. We focused on the subunit VI encoding gene, COX6, and detected unexpectedly complex oxygen regulation. We found that COX6 transcription possessed a critical threshold oxygen regulation between 0 and 2%. COX6 transcription was superinduced by elevated oxygen level up to 45%; however, superinduction was lost at 60% oxygen and above. The COX6 upstream activation region, UAS6, contains both glucose and heme responsive regions, and COX6 oxygen regulation was transduced through UAS6 by heme, as has been described for other oxygen regulated genes in yeast. We found that binding of the UAS6-domain 1 protein, BAF1, was unaltered by oxygen regulation. Nor were the alternative BAF1 complexes observed by growth in different glucose conditions formed by growth at different oxygen levels.

The marine bacterium Pseudoalteromonas haloplanktis has a complex genome structure composed of two separate genetic units.

The genome size of Pseudoalteromonas haloplanktis, a ubiquitous and easily cultured marine bacterium, was measured as a step toward estimating the genome complexity of marine bacterioplankton. To determine total genome size, we digested P. haloplanktis DNA with the restriction endonucleases Notl and Sfil, separated the fragments using pulsed-field gel electrophoresis (PFGE), and summed the sizes of the fragments. The P. haloplanktis genome was 3512 +/- 112 kb by Notl digestion and 3468 +/- 54.1 kb by Sfil digestion. P. haloplanktis is also shown to have a complex genome structure, composed of two large replicons of approximately 2700 and 800 kb. Three pieces of evidence support this conclusion: (1) Two separate bands are always seen in PFGE of undigested P. haloplanktis DNA; (2) restriction digests of the larger band are missing a band of approximately 650 kb compared with restriction digests of total genomic DNA; and (3) a 16S rDNA probe hybridized to the larger replicon but not to the smaller. To our knowledge, P. haloplanktis is the first marine bacterium shown to have a complex genome structure.

Screening of a fosmid library of marine environmental genomic DNA fragments reveals four clones related to members of the order Planctomycetales.

A fosmid library with inserts containing approximately 40 kb of marine bacterial DNA (J. L. Stein, T. L. Marsh, K. Y. Wu, H. Shizuya, and E. F. DeLong, J. Bacteriol. 178:591-599, 1996) yielded four clones with 16S rRNA genes from the order Planctomycetales. Three of the clones belong to the Pirellula group and one clone belongs to the Planctomyces group, based on phylogenetic and signature nucleotide analyses of full-length 16S rRNA genes. Sequence analysis of the ends of the genes revealed a consistent mismatch in a widely used bacterium-specific 16S rRNA PCR amplification priming site (27F), which has also been reported in some thermophiles and spirochetes.

Bacteria and Archaea physically associated with Gulf of Mexico gas hydrates.

Although there is significant interest in the potential interactions of microbes with gas hydrate, no direct physical association between them has been demonstrated. We examined several intact samples of naturally occurring gas hydrate from the Gulf of Mexico for evidence of microbes. All samples were collected from anaerobic hemipelagic mud within the gas hydrate stability zone, at water depths in the ca. 540- to 2,000-m range. The delta(13)C of hydrate-bound methane varied from -45.1 per thousand Peedee belemnite (PDB) to -74.7 per thousand PDB, reflecting different gas origins. Stable isotope composition data indicated microbial consumption of methane or propane in some of the samples. Evidence of the presence of microbes was initially determined by 4,6-diamidino 2-phenylindole dihydrochloride (DAPI) total direct counts of hydrate-associated sediments (mean = 1.5 x 10(9) cells g(-1)) and gas hydrate (mean = 1.0 x 10(6) cells ml(-1)). Small-subunit rRNA phylogenetic characterization was performed to assess the composition of the microbial community in one gas hydrate sample (AT425) that had no detectable associated sediment and showed evidence of microbial methane consumption. Bacteria were moderately diverse within AT425 and were dominated by gene sequences related to several groups of Proteobacteria, as well as Actinobacteria and low-G + C Firmicutes. In contrast, there was low diversity of Archaea, nearly all of which were related to methanogenic Archaea, with the majority specifically related to Methanosaeta spp. The results of this study suggest that there is a direct association between microbes and gas hydrate, a finding that may have significance for hydrocarbon flux into the Gulf of Mexico and for life in extreme environments.