- freely available
Biology 2013, 2(2), 629-650; doi:10.3390/biology2020629
Abstract: Lake Vostok is the largest of the nearly 400 subglacial Antarctic lakes and has been continuously buried by glacial ice for 15 million years. Extreme cold, heat (from possible hydrothermal activity), pressure (from the overriding glacier) and dissolved oxygen (delivered by melting meteoric ice), in addition to limited nutrients and complete darkness, combine to produce one of the most extreme environments on Earth. Metagenomic/metatranscriptomic analyses of ice that accreted over a shallow embayment and over the southern main lake basin indicate the presence of thousands of species of organisms (94% Bacteria, 6% Eukarya, and two Archaea). The predominant bacterial sequences were closest to those from species of Firmicutes, Proteobacteria and Actinobacteria, while the predominant eukaryotic sequences were most similar to those from species of ascomycetous and basidiomycetous Fungi. Based on the sequence data, the lake appears to contain a mixture of autotrophs and heterotrophs capable of performing nitrogen fixation, nitrogen cycling, carbon fixation and nutrient recycling. Sequences closest to those of psychrophiles and thermophiles indicate a cold lake with possible hydrothermal activity. Sequences most similar to those from marine and aquatic species suggest the presence of marine and freshwater regions.
Nearly 400 subglacial lakes have been discovered in Antarctica, the largest of which is Lake Vostok [1,2,3,4,5]. While Lake Vostok covers an area (15,690 km2) that is about 80% of the size of the Laurentian Great Lake Ontario, it holds a larger volume of water (5,400 km3), due to its depth (maximum depth = 510 m). It lies beneath 3,700 to 4,200 m of ice, and has been continuously ice-covered for the past 15 million years, with the only known influx of water originating from melting of the overriding glacier. Lake Vostok consists of a northern and the southern basin (Figure 1). Little is known about the northern basin, but more is known about the southern basin because of studies based on an ice core that was drilled over the southeastern corner of the lake. While glacial ice melts over portions of the lake, water from the lake freezes (i.e., accretes) to the bottom of the glacier in other parts of the lake creating an accretion ice layer that is over 200 m thick in some locales [2,6,7,8]. Because the glacier moves across the lake at a rate of approximately 3 m per year, the accretion ice holds a temporal record that spans approximately 5,000 to 20,000 years , as well as a spatial record of the surface waters of the lake. The accretion ice from the core represents several parts of the southern portion of the lake, including a region near a shallow embayment on the southwestern corner of the lake and the southern portions of the southern main basin.
Accretion ice from the ice core has been analyzed to determine the concentrations of specific ions (e.g., Na+, K+, Ca2+, Cl−, SO42−) [9,10,11,12] and biomass [13,14,15,16,17,18,19] originating from several locations in the lake. The ice that formed in the vicinity of the shallow embayment (3,538–3,608 m, termed type 1 accretion ice) contains fine particulate matter , as well as relatively high concentrations of ions , organisms and nucleic acids [9,16,17]. Conversely, accretion ice that formed over the southern basin (3,609–3,769 m, termed type 2 ice) contains low concentrations of particulates, ions, organisms and nucleic acids. Dozens of bacterial cells, fungal cells and sequences have been reported from several accretion ice core sections [12,13,14,15,16,17,18,19] with the highest numbers concentrated in the core sections that represent regions of the lake near the shallow embayment. They include many types of organisms that are common to other aquatic environments, as well as many that remain unidentified. Sequences from thermophilic bacteria have been reported, indicative of possible hydrothermal activity in the lake [20,21,22]. Autotrophic and heterotrophic species have also been reported from the accretion ice [16,17]. These reports indicate that Lake Vostok might be more biologically complex than previously concluded.
Another feature of Lake Vostok is that it lies entirely below current mean sea level. Its surface is more than 200 m below sea level, and the deepest point is almost 800 m below sea level. A recent study  concluded that Lake Vostok lies within a graben (similar to those in the Great Rift Valley in Africa) that formed more than 60 million years ago. A second study, based on radar data , reported that 35 million years ago when Antarctica was free of ice, the Southern Ocean was in the immediate vicinity of Lake Vostok. However, by 34 million years ago, ice had covered the lake and lowered sea level, which might have isolated it from a direct connection to the ocean. The fact that parts of Lake Vostok contain moderate levels of salt, and that sequences from marine organisms have been detected in the accretion ice indicate that this lake might have a complex history. In this study, we utilize metagenomic/metatranscriptomic sequence data (; Supplementary Tables S1–S10) to reconstruct the possible ecology of Lake Vostok.
|Taxon||Unique gene sequences||Unique rRNA gene sequences a||Ecology and physiology b||Species characteristics b|
|≥200 nt <200 nt|
|Acidobacteria||2||1||0||acidophilic, soil, adaptable||chemoorganotrophic heterotrophs|
|Actinobacteria||228||151||24||thermophilic, halotolerant, psychrotolerant, alkalaitolerant, psychrophilic, Antarctic, deep sea sediments, lake sediments, some grow on limestone||nitrogen fixation, nitrite oxidation, ammonia oxidation, organic decomposition, heterotrophs|
|Bacterioidetes/Chlorobi||88||61||8||aquatic, sediments, thermophilic, psychrophilic, alkalaiphilic, anaerobic||carbon fixation (use sulfide ions, hydrogen or ferrous ions), reductive TCA cycle|
|Chloroflexi||1||0||0||aerobic, thermophilic||carbon fixation using the 3-hydroxylpropionic bicycle|
|Cyanobacteria||228||144||60||common in Antarctic lakes, at least one is thermophilic (Thermosynecoccus sp.)||carbon fixation using the reductive pentose phosphate cycle, some are from anoxygenic ancestors|
|Deferribacteres||1||1||0||animal intestines, anaerobic||chemoorganotrophic heterotrophic|
|Deinococcus/ Thermus||5||1||1||thermophilic, radiophilic, aerobic some associate with cyanobacteria||chemoorganotrophic heterotrophic|
|Fibrobacteres||1||0||1||anaerobic, inhabit animal intestines||chemoorganotrophic heterotrophic|
|Firmicutes||602||401||40||Spore formers, common in extreme environments, thermophiles, mesophilic, psychrophilic, psychrotolerant, halophilic, hot springs, deep sea thermophilic, anaerobic, aerobic||heterotrophic|
|Fusobacteria||10||8||0||parasitic on animals, anaerobic||chemoorganotrophic heterotrophic|
|Planctomycetes||6||2||2||Fresh, brackish and saline lakes/ponds, anaerobic||chemoautolithotrophic anammox, nitrite reduction using ammonium as electron donor|
|Alphaproteobacteria||91||45||7||Psychrophilic, mesophilic, thermophilic, Antarctic lakes, animal symbionts, aerobic, soil/sediments, aquatic, alkalaitolerant, require calcium, marine, halotolerant||nitrite reduction, nitrifying bacteria, denitrification (nitrate to nitrogen gas), methylotrophic, use inorganic sulfur, oxidize sulfate and thiosulfate, carbon fixation using the reductive pentose phosphate cycle, carbon fixation using the reductive TCA cycle|
|Betaproteobacteria||105||31||7||thermophilic, mesophilic, psychrophilic, aquatic, aerobic, highly adaptable||nitrogen fixation, nitrate reduction, ammonia oxidation, carbon fixation using the reductive pentose phosphate cycle, manganese oxidation, iron oxidation, inorganic sulfur oxidation, arsenic oxidation|
|Deltaproteobacteria||10||5||0||aquatic, soil, mesophilic, anaerobic, aerobic, freshwater debris, predator of Gram-negative bacteria, halotolerant, marine||carbon fixation using the reductive TCA cycle, iron reduction, sulfur reduction, ethanol fermentation|
|Epsilonproteobacteria||6||3||2||Some animal associated, mesophilic, thermophilic, aerobic, anaerobic||carbon fixation using the reductive TCA cycle|
|Gammaproteobacteria||254||176||28||thermophilic, mesophilic, psychrophilic, psychrotolerant, aerobic, anaerobic, peizophilic, deep sea, halophilic, polar ice, soil, sediments, permafrost, 33 distinct sequences from species of Psychrobacter, 10 distinct sequences from species of Halomonas (halophilic), some produce intracellular gas vesicles, some are animal associated||nitrogen fixation, nitrate reduction, nitrite respiration, denitrification, sulfur oxidation, chemolithoautotrophs, iron oxidation, mineralization of aromatics, carbon fixation using the reductive pentose phosphate cycle|
|Tenericutes||4||4||0||saprobes and arthropod pathogens/symbionts, anaerobic||heterotrophic|
|Verrucomicrobia||3||1||0||freshwater, soil, symbionts of protists and nematodes, aerobic||heterotrophic|
|Uncultured Bacteria||1839||1492||278||Sequences similar to those from uncultured and unidentified species, many from other environmental metagenomic studies||Unknown|
|ARCHAEA||2||0||0||deep hydrate-bearing sediment, peizotolerant, psychrotolerant||Methanotrophic, carbon fixation using the reductive acetyl-CoA pathway|
|Amoebozoa||1||1||0||Nolandella sp.; aquatic; feed on bacteria, diatoms, nematodes, fungi, protozoans and organic matter||Heterotrophic|
|Chlorophyta||10||5||4||Antarctic and polar green algal species||carbon fixation using the reductive pentose phosphate cycle|
|Rhodophyta||1||0||0||Antarctic red alga||carbon fixation using the reductive pentose phosphate cycle|
|Streptophyta||63||23||5||Pollen from lake sediments or from glacial deposition?||(carbon fixation using the reductive pentose phosphate cycle)—non-viable?|
|Chromalveolata||12||6||2||diatoms, heterokonts, predatory protists, dinoflagellates, ciliates, Antarctic, aquatic||carbon fixation using the reductive pentose phosphate cycle, heterotrophic|
|Arthropoda||16||8||0||Arctic, Antarctic, aquatic. (e.g., Daphnia sp., Ellipura, Branchiopoda, Entomobryiadae).||heterotrophic|
|Bilateria||1||0||1||Deep sediment environmental sample||unknown|
|Chordata||3||1||0||Aves, from meteoric ice or contaminant?||heterotrophic|
|Cnideria||1||0||0||Small sea anemone, lives in soft sediment with water salinities of 9 to 52 ppt at temperatures from −1 to 28 °C.||heterotrophic|
|Mollusca||1||0||1||Nutricola sp., cold water marine bivalve that burrows into sediments.||heterotrophic|
|Rotifera||1||1||0||Survives under extreme conditions; feed on detritus, bacteria, algae and protists.||heterotrophic|
|Tardigrada||1||0||1||Hardy animal, eats rotifers and algae, can survive from approximately −270 to 150 °C||heterotrophic|
|Ascomycota||48||34||4||Antarctic, polar, aquatic, soil||heterotrophic|
|Basidiomycota||29||24||0||Antarctic, polar, psychrophilic, psychrotolerant||heterotrophic|
|Mucorales||1||0||1||Aquatic, parasitic on arthropods||heterotrophic|
|Rhizaria||1||0||0||Freshwater, Paulinella sp.||heterotrophic|
a Sequences ≥200 nt were submitted to NCBI GenBank and were assigned accession numbers, while those shorter than 200 nt could not be submitted to NCBI GenBank, and therefore do not have accession numbers. Totals based on BLAST searches using pyrosequencing reads; b Ecological, physiological and other characters were based on information from the sequenced organisms identified in the BLAST searches. Sources of information were NCBI descriptions, publications cited in the NCBI descriptions and web sources (see Supplementary Tables S1–S6).
2. Results and Discussion
2.1. Summary of Results
Two samples, each consisting of meltwater from two accretion ice core sections, were analyzed for this research. One (termed “V5”) contained meltwater from two ice core sections (3,563 m and 3,585 m; Figure 1) that accreted in the vicinity of the shallow embayment on the southwestern corner of Lake Vostok. The other (termed “V6”) contained meltwater from two ice core sections (3,606 m and 3,621 m) that accreted on the western side of the southern basin. Sequences have been deposited in the NCBI (National Center for Biotechnology) GenBank database (accession numbers are provided in the Experimental Section; BLAST results are presented in Supplementary Tables S1–S10 .). For the V5 sample, 36,754,464 bp of sequence data was obtained that included 94,728 high quality 454 sequence reads, with mean lengths of 388 bp. For the V6 sample, 1,170,900 bp of sequence data was obtained that included 5,204 high quality reads, with mean lengths of 225 bp. The lower quantity of sequence data for V6 is consistent with our previous results from the same core sections indicating much lower concentrations of cells and viable cells in the V6 ice core sections compared to the V5 ice core sections [16,17]. However, the lower number of sequences and the shorter average read lengths also might indicate that the nucleic acids in this sample were degraded to a greater extent than those in the V5 sample. Overall, approximately 15% of the sequences were unique, while the remaining 85% were additional copies from the unique set of sequences. A total of 3,718 unique sequences were retrieved from V5 (3,146 were rRNA gene sequences), of which 1,863 could be classified to species (Table 1; Supplementary Tables S1–S6 ), and 184 unique gene sequences were retrieved from V6 (111 were rRNA gene sequences), of which 133 could be classified to species (Table 2; Supplementary Tables S7–S10). Approximately 94% of the unique sequences in V5 and 85% in V6 were from Bacteria. Sequences closest to those from species of autotrophs and heterotrophs were present. Only two unique Archaea sequences were found (both in V5), and they were most similar to species of methanotrophs from deep-ocean sediments. The remaining sequences were closest to those from species of Eukarya (6% in V5 and 15% in V6), including more than 200 unique sequences from multicellular organisms, most of which were Fungi (primarily ascomycetes and basidiomycetes). In general, the species indicated by the sequence comparisons were organisms specific to lakes, brackish water, oceans/seas, soil, lake sediments, deep-sea sediments, deep-sea thermal vents, animals and plants.
|Unique rRNA gene sequences a||Ecology and physiology b||Species characteristics b|
|≥200 nt <200 nt|
|Actinobacteria||14||1||4||fish pathogen, psychrophilic, ocean/lake sediments||chemoorganotrophic heterotrophic|
|Bacterioidetes/Chlorobi||1||0||0||psychrophilic, alkalaiphilic, aerobic||heterotrophic|
|Deinococcus/Thermus||1||0||0||thermophilic, radiophilic, some associate with cyanobacteria||chemoorganotrophic heterotrophic|
|Firmicutes||16||5||0||alkalaiphilic, thermophilic, mesophilic, psychrophilic, soil/sediments, anaerobic, some parasitic/symbiotic on animals||heterotrophic, nitrate reduction|
|Fusobacteria||1||0||0||mesophilic, parasitic on animals, anaerobic||heterotrophic|
|Alphaproteobacteria||8||5||0||mesophilic, psychrophilic, aerobic, acid tolerance, aquatic, sediments, animal symbionts||nitrogen fixation, heterotrophic, carbon fixation using the reductive pentose phosphate cycle|
|Betaproteobacteria||22||6||3||annelid symbiont, annelid associated, Arctic soils, aquatic, Antarctic marine, intracellular gas vacuoles, high amounts of 16:1 ω7c fatty acids, psychrophilic, mesophilic, thermophilic, aerobic, highly adaptable, hot springs, (e.g., Thiobacillus sp., related to Hydrogenophilus thermoluteus, previously reported by Bulat et al. 2004 [20,21] Lake Vostok accretion ice at 3,607 m depth)||nitrogen fixation, chemoorganotrophic heterotrophic, aromatic hydrocarbon degradation, nitrous oxide reduction, arsenic oxidation, arsenic reduction, inorganic sulfur oxidation, chemolithoautotroph,, hydrogen oxidation, carbon fixation using the reductive pentose phosphate cycle|
|Gammaproteobacteria||39||14||3||fish intestinal symbionts (2 species), nematode associated, animal associated, plant associated, aquatic, soil/sediment, thermophilic, mesophilic, psychrophilic, anaerobic, aerobic, halotolerant||nitrogen fixation, nitrate reduction, nitrite respiration, heterotrophic, carbon fixation using the reductive pentose phosphate cycle|
|Uncultured Bacteria||50||36||10||sequences similar to those from uncultured and unidentified species, many from other environmental metagenomic studies||unknown|
|Streptophyta||2||1||1||pollen from lake sediments or from glacial deposition?||(carbon fixation using the reductive pentose phosphate cycle)—non-viable?|
|Arthropoda||5||0||0||aquatic, Acari, parasitic||heterotrophic|
|Ascomycota||13||7||3||aquatic, one grows on marble and limestone, one isolated from mid-ocean hydrothermal vents, some from sediments, one can use methanol as a carbon source, Antarctic species||heterotrophic|
|Basidiomycota||4||0||4||Antarctic, marine, aquatic||heterotrophic|
a Sequences ≥200 nt were submitted to NCBI GenBank and were assigned accession numbers, while those shorter than 200 nt could not be submitted to NCBI GenBank, and therefore do not have accession numbers; b Ecological, physiological and other characters were based on information from the sequenced organisms identified in the BLAST searches. Sources of information were NCBI descriptions, publications cited in the NCBI descriptions and web sources (see Supplementary Tables S7–S10).
A large number of the sequences were most similar to those from psychrophilic and psychrotolerant species (Table 1, Table 2; Supplementary Tables S1–S10). Within the Gammaproteobacteria, there were 33 unique sequences closest to various Psychrobacter species (most with rRNA SSU gene identities of greater than 97%), all described as psychrophiles. Also present were sequences closest to psychrophilic or psychrotolerant species of Actinobacteria, Alphaproteobacteria, Archaea, Archaeplastida, Bacteroidetes, Betaproteobacteria, Firmicutes, Chromalveolata, and Opisthokonta (both Animalia and Fungi). Conversely, there were many sequences that were closest to those from several thermophilic species (many with rRNA SSU gene identities greater than 97%). While most were found in V5 ice (46 with rRNA sequence identities greater than 97% to known taxa), a few were found in V6 ice (2 with rRNA sequence identities greater than 97% to known taxa). A number of sequences most similar to those of sulfur oxidizing bacteria were found in V5 (Table 1, Table 2). Previously, several gene sequences from a thermophilic bacterium, Hydrogenophilus thermoluteolus were reported from the Lake Vostok accretion ice [20,21].
Several sequences from marine species, as well as from halophilic and halotolerant species, were present in the metagenome/metatranscriptome data set (Table 1, Table 2). Sequences closest to Jeotgalicoccus halotolerans, Nesterenkonia halotolerans, and other halophilic bacteria were found in V5 accretion ice, several of which have rRNA SSU gene identities greater than 98%. Some of these species were alkalaitolerant. A number of sequences in V5 and V6 were most similar to sequences from marine species, including marine bacteria (many with rRNA identities above 97%), a sea squirt-associated bacterium (99% rRNA SSU gene identity to Pseudomonas xanthomarina), an oyster pathogen (100% identity to a hypothetical protein from Perkinseus maratimus), a sea anemone (78% identity to a hypothetical protein from Nematostella vectensis, a small sea anemone, related to Hydra spp.) and a marine mollusk (100% rRNA SSU identity to Nutricola tantilla). The presence of marine, halophilic and halotolerant species is suggestive of marine layers, or other regions with high ion concentrations, within the lake or lake sediments. Saltwater layers and submarine brine lakes have been reported at the bottom of the Mediterranean Sea and Gulf of Mexico [25,26]. The number of V5 sample sequences with ≥97% identities to psychrophiles and thermophiles were roughly equal (46 and 49, respectively).The combination of possible halophiles, psychrophiles and thermophiles (at the ≥97% identity levels; Table 1, Table 2; Figure 2), in addition to higher concentrations of ions and particulate matter in the V5 sample, all are suggestive of a diversity of conditions in the southwestern region of the lake. In the V6 samples, there were more sequences (sequence identities ≥97%) closest to psychrophiles (7) than thermophiles (2). This is consistent with the presence of hydrothermal activity in the vicinity of the shallow embayment, and colder conditions in the main basin.
2.3. Metabolic Classification
We considered only sequences whose species and functional characteristics had been clearly identified. Genes for glycolysis, the TCA (tricarboxylic acid) cycle and genes for the synthesis of most amino acids were present (Supplementary Figures S1–S5). Incomplete pathways were found for the synthesis of arginine, histidine and proline. Alternate enzymes might be used for these processes, as determination of some sequences could not be made unambiguously. Some of the genes for each of these pathways were present, and therefore it is assumed that some of the unidentified sequences may encode for the missing enzymes in the pathways.
Sequences closest to those from bacteria capable of nitrogen fixation, nitrosification, nitrification, nitrate reduction, denitrification, anammox, assimilation and decomposition were present (Figure 3). Several types of nitrogen fixing bacteria were indicated by the sequences, including species of Azospirillum, Azotobacter, Bacillus, Burkholderia, Cyanobacteria, Frankia, Klebsiella, Rhizobium, Rhodobacter, Rhodopseudomonas and Sinorhizobium. Sequences of nitrifying bacteria included species of Methylococcus, Nitrobacter, Nitrococcus, Notrosococcus and Nitrosomonas. Species important in other parts of the nitrogen cycle were within the genera Alkaligenes, Bacillus, Clostridium, Micrococcus, Paracoccus, Proteus, Pseudomonas, Streptomyces and Thiobacter. Several sequences from planctomycetes were closest to sequences from species capable of anammox metabolic processes in marine environments.
Sequences of genes and organisms involved in many phases of carbon fixation cycles and pathways were found (Figure 3). Three forms of carbon fixation were indicated. The sequences indicated that most of the organisms utilize either the reductive TCA (rTCA) cycle (α-, δ- and ε-proteobacteria, and Chlorobi) (Table 1, Table 2) or the reductive pentose phosphate (rPP; Calvin-Benson) cycle (Archaeplastida, Chromalveolates, Cyanobacteria, and α-, β-, and γ-Proteobacteria) . Based on the frequency of gene sequences, the most common mode of CO2-fixation was the rTCA cycle (Table 1, Table 2), while the rPP cycle was the second most common. The two Archaea in V5 may fix carbon via the reductive acetyl-CoA (rACA) pathway . However, mRNA gene sequences for enzymes in this pathway were not found in searches of the metagenome/metatranscriptome data set.
A large number and diversity of sequences from phototrophs were present in the accretion ice, including 228 cyanobacterial, 11 algal, 12 chromalveolate, and other unique sequences. Sequences for many of the genes involved in the light reactions of photosynthesis in cyanobacteria were found in the accretion ice. These included light-independent photochlorophyllide reductase and oxidase, phycocyanobilin oxidoreductase, a phycoerythrin subunit and several genes involved in carotenoid biosynthesis. However, gene function was not measured in this study, and it is possible that some of the gene sequences were from pseudogenes, that they are inactive genes, or they originated from organisms once entrapped in the meteoric ice.
While only about 6% of the unique sequences were closest to eukaryotes (221 from V5, 87 of which have sequence identities of ≥97% with sequences on NCBI; and 29 from V6, 24 of which have identities ≥97%), diverse taxonomic groups were represented. Most of the sequences were most similar to those from Fungi (91 sequences in V5 and 22 in V6), including one rRNA SSU sequence that was 99% similar to a marine fungus sequence that previously had been recovered from a deep-sea thermal vent . Several sequences from species of Animalia were found, including 21 sequences closest to those from arthropods (16 in V5 and 5 in V6), many of which are predatory or parasitic, including sequences closest to species of Daphnia (planctonic crustaceans; 98% identity), Ellipura (≥95% identity with species of springtails, some of which are aquatic or marine), Branchiopoda (fairy shrimp, primarily freshwater; 93% identity) and Entomobryidae (slender spingtails, some of which are aquatic; 89–98% identity). Additionally, V5 contained sequences closest to an unidentified bilaterian, a rotifer (closest to Adineta sp., which is a hardy, cosmopolitan, freshwater species; 98% identity), a tardigrade (closest to Milnesium sp., which is a hardy, predatory, cosmopolitan, freshwater species; 93% identity), a mollusk (Nutricola tantilla, a small [maximum diameter of 9 mm] marine bivalve that lives in sediments to about 120 m water depth; 100% identity) and a cniderian (related to Nematostella sp., a small sea anemone; 78% identity). Several Archaeplastida sequences were found in V5 and V6 (most with sequence identities of ≥99%).
Sequences closest to an uncultured lobster gut bacterium (98% identity), Verminephorbacter sp. (an annelid nephridia symbiont; 92% identity), Renibacter salmonarium (a salmonid fish pathogen; 98% identity), a rainbow trout intestinal bacterium T1 (93% identity) and Photorhabdus asymbiotica (a nematode symbiont; 98% identity) all were found in the V6 accretion ice sample. Additionally, sequences closest to Carnobacterium mobile (associated with fish; 100% identity), Macrococcus sp. (a bivalve-associated bacterium; 97% identity), Pseudomonas xanthomarina (associated with sea squirts; 99% identity) and Mycobacterium marinum (associated with fish; 99% identity) were found in the V5 accretion ice sample. All of the species are dependent on intimate associations (symbiotic or parasitic) with their eukaryotic hosts, which are crustaceans, annelids, tunicates, nematodes or fish. Species of all of these animal groups have been found in the vicinity of deep-sea thermal vents and elsewhere in marine and aquatic environments [29,30,31,32,33,34,35,36,37]. Additional indications of animals in the lake came from sequences of several species in the Enterobacteriaceae, which were present in both the V5 and V6 samples. These included sequences closest to several strains/species of E. coli, Erwinia, Klebsiella, Salmonella, and Shigella (most with sequence identities ≥97%), all of which are found in the digestive systems of fish and other aquatic and marine animals. In addition, sequences closest to those from species of Fusobacteria (some with ≥97% identities) that are parasitic on animals, Alphaproteobacteria (some with ≥97% identities) that are animal symbionts, and Tenericutes that are arthropod symbionts and pathogens (up to 91% sequence identity) were found in the V5 sample.
In V5, there were 16 sequences closest to those from single-celled eukaryotic species. These included sequences closest to species of Excavata (≥98% identity), Rhizaria (closest to Paulinella sp., a freshwater phototroph; 94% identity), Amoebozoa (Naeglaria gruberei, 98% identity; Nolandella sp., marine, 88% identity) and Chromalveolata (10 unique sequences, including two Ciliophora, 99% identity each; three bacillariophytes, Stephanodiscus sp.—99%, Stephanodiscus sp.—100%, Hatzschia sp.—95% identity; three heterokonts, Aphanomyces euteiches—98% identity, Botrydiopsis constricta—99% identity, Halosiphon tomentosus—97% identity); a cryptophyte, Cryptomonas paramecium—100% identity; and a member of Perkinsea, obligate parasite of mollusks—100% identity. While some of these eukaryotes are free-living, many are symbionts, parasites or commensals on multicellular organisms, including animals and plants. Several multicellular organisms were indicated by the sequence data, but the sequences closest to symbionts and parasites suggest that a more diverse set of multicellular eukaryotes might exist in the lake.
2.5. Possible Marine Environment in Lake Vostok
Organisms in Lake Vostok have had millions of years to adapt and evolve. The lake has been continuously ice-covered for approximately 15 million years [1,4,10,23,24,38]. During parts of the Miocene (15 to 25 million years ago, mya), it was intermittently ice-free, and previous to that, a cooling period from 25–34 mya led to the lake to be ice-covered much of the time . However, prior to 35 mya (during the Eocene), most of Antarctica (including the Lake Vostok region) was free of ice, sea levels were higher and extensive complex ecosystems were present on the continent, complete with lakes and streams, as well as diverse sets of microbes, plants (including extensive forests), fungi and animals. During these times, Lake Vostok probably contained a species-rich biota. Currently, Lake Vostok is below sea level. Currently, it is separated from regions that once were occupied by ocean water by low ridges that are approximately 20–50 m above current mean sea level [23,24,38]. However, 35 million years ago, sea levels were between 50–100 m higher. Therefore, this low area may have been a straight that connected Lake Vostok with the ocean, thus making it a large marine bay (Figure 4). Our metagenomic/metatranscriptomic data set included sequences that are most similar to sequences from marine organisms, including many Bacteria, halophiles, a marine mollusk, a sea anemone, a marine thermal vent fungus and two Archaea that previously were described from deep-ocean sediments. As temperatures in Antarctica began to cool and sea levels dropped about 34 million years ago, Lake Vostok become ice covered and isolated from the ocean . Aerobic organisms that survive in cold and partially shaded aquatic environments could have survived in the epilimnion. Anaerobes would have been limited to the benthic and sediment regions. Hydrothermal regions may have been present much of the time, because rifting of the region began more than 60 million years ago . As freshwater from the melting glacier flowed into the lake, ion gradients were likely to develop. These gradients are common in other ice-covered Antarctic lakes [39,40,41,42], and the differences in ion concentrations in the embayment compared to the main basin are consistent with this hypothesis. Hydrothermal activity in the vicinity of the embayment might cause mixing of any stratified layers in the lake in that region, leading to the higher ion and mineral inclusion concentrations in the accretion ice from that region.
Once current continuous ice-cover began approximately 15 million years ago, additional selection would have occurred as light intensities decreased, and oxygen concentrations and water pressures increased. Although extinctions would probably have been extensive, it is unlikely that all life would disappear from the lake and its sediments. Based on the number of unique species matches in BLAST searches of our accretion ice metagenomic/metatranscriptomic data set, we estimate the total number of species to be at least 1,996 in Lake Vostok, of which over 90% (approximately 1,800) are Bacteria. This converts to approximately 4 species mL−1, assuming that the concentration of nucleic acids in the accretion ice is representative of the concentration of nucleic acids and organisms in the lake water, and that the samples are representative of the lake in general. However, as ice forms, it can force out many components, including some molecules, minerals and cells. Therefore, the concentrations of organisms and nucleic acids are probably higher in the lake water than in the accretion ice. The calculated concentration is below the number of species found in ocean water, sediments and most freshwater lakes [43,44,45,46]. Because the accretion ice represents primarily water at the surface of the lake, species density and richness in the lake could be much higher in some locales. In any case, a relatively high number of sequences matching sequences from a diverse set of species were found in Lake Vostok accretion ice. The 15–35 million years of coverage by ice appears to have been ample time for many organisms to adapt to the extreme conditions that developed in the lake, which has likely led to numerous speciation events.
3. Experimental Section
3.1. Acquisition and Processing of Ice Core Sections
All ice core sections were selected from the USGS NICL (United States Geological Survey, National Ice Core Laboratory, Denver, CO, USA). They were selected based on desired depths and for the absence of cracks (to avoid possible external contamination). They were shipped frozen to our laboratory. Sections were surface sterilized according to a tested method that assures destruction and removal of all surface contaminating cells and nucleic acids, while preserving cells and nucleic acids frozen in the ice [16,17,47,48]. Briefly, quartered ice core sections, 6–16 cm in length (total volume approximately 125 mL), were warmed at 4 °C for 30 min (to avoid thermal shock and cracking) before surface decontamination. The work surfaces in a room (under positive pressure) separate from the main laboratory were treated with 0.5% sodium hypochlorite, 70% ethanol and UV irradiation for one hour prior to surface sterilizing and melting the ice core sections. Inside a sterile laminar flow hood, the ice core sections were surface decontaminated by total immersion in a 5.25% sodium hypochlorite solution (pre-chilled to 4 °C for at least 2 h) for 10 s followed by three rinses with 800 mL of sterile water (4 °C, 18.2 MΩ, <1 ppb [parts per billion] total organic carbon, TOC, and autoclaved). Then, the core section was transferred into a sterile funnel and melted at room temperature by collection of 25–50 mL aliquots. This protocol significantly reduces the risk of contamination of the ice core meltwater samples [47,48]. The meltwater was then frozen at −20 °C. Sample V5 included meltwater from Vostok 5G core sections at depths of 3,563 and 3,585 m, corresponding to type 1 ice that accreted in the vicinity of the embayment. Sample V6 included core sections 3,606 and 3,621 m, corresponding to type 2 ice that accreted over a portion of the southern main basin of Lake Vostok (Figure 1). A total of 250 mL of meltwater was used for each sample (approximately 125 mL from each ice core section). The meltwater samples were filtered sequentially through 1.2, 0.45 and 0.22 μm Durapore filters (Millipore, Billerica, MA, USA). The filters were stored at −80 °C for future reference. Then, the filtered meltwater was subjected to ultracentrifugation at 100,000 xg for 16 h to pellet cells and nucleic acids. Two control samples (purified water, 18.2 MΩ, <1 ppb TOC; and the same water, autoclaved and subjected to concentration by ultracentrifugation) also were processed using the same protocols. The V5, V6, and control samples were ultracentrifuged on different days to lessen potential cross-contamination. Pellets were rehydrated in 50 µL 0.1× TE (1 mM Tris [pH 7.5], 0.1 mM EDTA).
3.2. DNA and RNA Extraction
Nucleic acid extraction was performed using MinElute Virus Spin Kits (QIAGEN, Valencia, CA) and eluted in 150 µL AVE buffer (water with 0.04% sodium azide). This kit isolates both RNA and DNA. The eluted nucleic acids were further concentrated by precipitating overnight at −20 °C with 0.5 M NaCl in 80% ethanol. They were then pelleted by centrifugation at 16,000 × g for 15 min, washed with cold 80% ethanol and centrifuged at 16,000 × g for 5 min. They were dried under vacuum, and then they were resuspended in 15 µL 0.1× TE.
3.3. cDNA Synthesis and Amplification of cDNA and DNA
Complementary DNAs (cDNAs) were synthesized from the extracted RNAs. The procedure was performed using a SuperScript Choice cDNA kit (Invitrogen, Grand Island, NY, USA), according to the manufacturer’s instructions, using 10 µL of the extracted RNA and 80 pmol of random hexamer primers. The cDNA was then mixed with 10 µL of extracted DNA (less than 1 ng/µL) from the same meltwater sample, and EcoRI (Not I) adapters (AATTCGCGGCCGCGTCGAC, dsDNA) were added using T4 DNA ligase. The final concentration of components in each reaction for addition of EcoRI adapters was: 66 mM Tris-HCl (pH 7.6), 10 mM MgCl2, 1 mM ATP, 14 mM DTT, 100 pmols EcoRI (Not I) adapters and 0.5 units of T4 DNA ligase, in 50 µL total volume. The reaction was incubated at 15 °C for 20 h. Then, the reaction was heated to 70 °C for 10 min to inactive the ligase. [Note: The cDNAs and DNAs were mixed in order to maximize the biomass of nucleic acids, necessary for successful pyrosequencing. Thus, the cDNA comprised the metatranscriptomic fraction (of which most was from rRNA) and the DNA comprised the metagenomic fraction of each sample].
The products were size fractionated by column chromatography. Each 2 mL column contained 1 mL of Sephacryl® S-500 HR resin. TEN buffer (10 mM Tris-HCl [pH 7.5], 0.1 mM EDTA, 25 mM NaCl; autoclaved) was utilized to wash the columns and elute the samples through the columns. Fractions of approximately 40 µL were collected by chromatography. After measurement of the volume of each fraction, fractions 6–18 were precipitated to concentrate the DNA. Concentration was accomplished by adding 0.5 volumes (of the fraction size) of 1 M NaCl, and two volumes of −20 °C absolute ethanol. After gentle mixing, each was left to precipitate at −20 °C overnight. The fractions were centrifuged in a microfuge for 20 min at room temperature and decanted. Then, the pellets were washed with 0.5 mL of −20 °C 80% ethanol and centrifuged for 5 min. Finally each of the DNA pellets was dried under vacuum and rehydrated in 20 µL of 0.1× TE buffer.
After resuspension, fractions 6–18 were subjected to PCR amplification using EcoRI (NotI) adapter primers (AATTCGCGGCCGCGCTCGAC). The samples were amplified using a GeneAmp PCR Reagent Kit (Applied Biosystems, Carlsbad, CA, USA). Each reaction mixture contained: 10 mM Tris-HCl [pH 8.3], 50 mM KCl, 1.5 mM MgCl2, 0.001% (w/v) gelatin), 5 pmol each dNTP (dATP, dCTP, dGTP, and dTTP), 1 U AmpliTaq DNA polymerase and 50 pmols EcoRI (NotI) adapter primers (AATTCGCGGCCGCGCTCGAC), each in 25 µL total volume. The thermal cycling program was: 94 °C for 4 min; then 40 cycles of 94 °C for 1 min, 55 °C for 2 min, 72 °C for 2 min; followed by an incubation for 10 min at 72 °C. A 1 µL aliquot of each was subjected to 1% agarose gel electrophoresis at 5 V/cm in TBE (89 mM tris, 89 mM borate, 2 mM EDTA [pH 8.0]), containing 0.5 µg/mL ethidium bromide, and visualized by UV irradiation. Fractions that excluded small (<200 bp) and large (>2.0 kb) fragments were used for further processing. Then, amplified products for each fraction of the desired size range (as above) were pooled (approximately 350 µL per sample), and were precipitated with NaCl and ethanol, washed, and dried (as above). Each was rehydrated in 35 µL of 0.1× TE.
3.4. Addition of 454 A and B Sequences by PCR Amplification
Each of the amplified samples was then reamplified using primers that contained EcoRI/NotI sequences on their 3' ends and 454-specific primers on their 5' ends (one primer with sequence A; underlined: CGTATCGCCTCCCTCGCGCCATCAGAATTCGCGGCCGCGTCGAC; and the other with sequence B; CTATGCGCCTTGCCAGCCCGCTCAGAATTCGCGGCCGCGTCGAC). The thermal cycling program was: 94 °C for 4 min; then 40 cycles of 94 °C for 1 min, 55 °C for 3 min, 72 °C for 3 min; followed by an incubation for 10 min at 72 °C. All PCR products were cleaned with a PCR purification kit (QIAGEN, Valencia, CA, USA). The amplicons were quantified on agarose gels (as above) to calculate concentrations (based on comparisons to plasmid pGEM4Z (Promega, Madison, WI, USA) standards on the same gel). After adjusting concentrations to approximately 1 µg/µL, 20 µg of each was sent to Roche 454 Life Sciences 454 Technologies (Roche, Branford, CT, USA) for 454 pyrosequencing using a 454 GS Junior System.
3.5. Sequence Analysis
The sequences were extracted from the data file and organized using Python (Python Software Foundation) on the Ohio Super Computer (OSC, Columbus, OH, USA). The sequences were deposited in the GenBank nucleotide database at the National Center for Biotechnology Information (NCBI; accession numbers: JQ997163–JQ997235; JQ997237–JQ997322; JQ997324–JQ997402; JQ997404–JQ997547; JQ997549–JQ998298; JQ998300–JQ998745; JQ998747–JQ999505; JQ999568–JQ999624; JQ999909–JQ999910; JQ997196–JQ997198; JQ997274; JQ997284; JQ997285; JQ997287; JQ997308; JQ997309; JQ997361; JQ997374; JQ997375; JQ997378; JQ997384; JQ997393; JQ997394; JQ997443; JQ997448; JQ997457; JQ997460; JQ997469; JQ997487–JQ997497; JQ997541; JQ997613; JQ997623; JQ997624; JQ997638; JQ997639; JQ997651; JQ997695; JQ997698; JQ997801; JQ997804; JQ997847; JQ998421; JQ998746; JQ999303; JQ999327; JQ999330; JQ999348; JQ999360; JQ999361; JJQ999365–JQ999369; JQ999371; JQ999492; JQ999493; JQ999635–JQ999829; JQ999837–JQ999897; JQ999899; JQ999901–JQ999905; JQ999507–JQ999509; JQ999512; JQ999515; JQ999518–JQ999521; JQ999523–JQ999526; JQ999529–JQ999530; JQ999533; JQ999538; JQ999540; JQ999545; JQ999549; JQ999552; JQ999554; JQ999556–JQ999564; JQ999567; JQ999629; JQ999631; JQ999830; JQ999831; JQ999833–JQ999835). They were assembled using MIRA 3.0.5 (Whole Genome Shotgun and EST Sequence Assembler ), using the following command line: job=denovo, genome, accurate,454. From the assembly, the average lengths for V5 and V6 were 539 and 318, respectively. The average quality scores were 39.7 and 40.2, respectively; maximum coverages were 3.3 and 6.2, respectively; and average coverages were 2.2 and 3.5, respectively. Initial taxonomic analyses were performed on MG-RAST  and Galaxy , Batch Mega-BLAST searches were performed to determine taxonomic and gene identities. The BLAST execution file was set up to retrieve the top 10 similar sequences, with e-value cutoffs of 10−10. They were subjected to batch BLASTN similarity searches on the OSC, and then sorted according to gene, taxon, and similarity e-values using FileMaker (FileMaker, Inc., Santa Clara, CA, USA). The top BLASTN hit was used to determine taxonomic classification (when genus and species names were provided), also considering the lengths and percent similarities of the matches. The sequences were divided into four category files: V5 rRNA genes, V6 rRNA genes, V5 mRNA genes and V6 mRNA genes (Full list of sequences and descriptions in reference , and presented in Supplementary Tables S1–S10. The rRNA gene results were used primarily to determine taxonomic classifications. Each species was then categorized according to temperature requirements, growth requirements, metabolic functions and ecological niche, based on NCBI descriptions, publications cited in the NCBI descriptions, and internet sources. Some mRNA sequences were used to determine or confirm species identifications, where possible.
3.6. Metabolic Analysis
Sequences were uploaded onto the KAAS-KEGG (KEGG Automatic Annotation Server; KEGG—Kyoto Encyclopedia of Genes and Genomes, Kyoto, Japan) pathway website and blasted against the default set of bacterial and eukaryotic genes . The sequences were compared to known sequences from 40 taxa (23 provided on the KAAS-KEGG site, and 17 additional taxa added manually) The additional taxa (with abbreviations used for searches) were: Cryptococcus neoformans JEC21; Thalassiosira pseudonana; Dictyostelium discoideum; Burkholderia mallei ATCC 23344; Campylobacter jejuni NCTC11168; Desulfovibrio vulgaris DP4; Caulobacter crescentus CB15; Micrococcus luteus; Acidobacterium capsulatum; Flavobacterium johnsoniae; Fibrobacter succinogenes; Fusobacterium nucleatum; Opitutus terrae; Gemmatimonas aurantiaca; Rhodopirellula baltica; Chlorobium limicola; Chloroflexus aurantiacus. Based on the results from the KAAS-KEGG analysis, metabolic pathways that were present in our dataset were identified. Tables of enzymes that matched our sequences from each pathway were retrieved. Subsets of these are presented in Supplementary Figures S1–S5.
Lake Vostok accretion ice contains nucleic acids from a diversity of species. While many were closest to those from psychrophilic species, a large number of sequences were closest to those from thermophilic species. Sequences from both anaerobes and aerobes were represented, as well as halophiles, aquatic and marine species. The list of taxa included approximately 94% Bacteria and 6% Eukarya, including over 100 species of multicellular Eukarya. While most were fungi (primarily ascomycetes and basidiomycetes), a number of animals also were indicated, including a rotifer, tardigrade, nematode, bivalves, sea anemone, crustaceans, and possibly fish (as suggested by the presence of sequences that were most similar to those from bacterial symbionts and pathogens of fish species). The species indicated by the sequences include those that participate in many parts of the nitrogen cycle, as well as those that fix, utilize and recycle carbon. Because of the higher concentrations of nucleic acids and viable organisms in accretion ice compared to the overriding meteoric ice [16,17], it is likely that the organisms and nucleic acids in the accretion ice originated in the lake water. The indications of large numbers of marine, halophilic and halotolerant organisms suggest that marine layers, or other saline regions, might exist in the lake. They may have originated millions of years ago at a time when the lake might have been physically connected with the surrounding ocean. Therefore, Lake Vostok might contain a complex interdependent set of organisms, zones and habitats that have developed over the tens of millions of years of its existence.
We thank NICL, NICL-SMO and the Ice Core Working group for allowing us access to the ice core sections used in this research. This research was partially funded by the National Science Foundation (ANT-0536870) and Bowling Green State University. We greatly appreciate the donation of sequencing services by Roche 454 Life Sciences for testing of their GS junior system. We thank Paul F. Morris for his valuable help with the data analyses.
- Kapista, A.; Ridley, J.F.; Robin, G.Q.; Siegert, M.J.; Zotikov, I. Large deep freshwater lake beneath the ice of central Antarctica. Nature 1996, 381, 684–686. [Google Scholar] [CrossRef]
- MacGregor, J.A.; Matsuoka, K.; Studinger, M. Radar detection of accreted ice over Lake Vostok, Antarctica. Earth Planet Sci. Lett. 2009, 282, 222–233. [Google Scholar] [CrossRef]
- Masalov, V.N.; Lukin, V.V.; Shermetiev, A.N.; Popov, S.V. Geophysical investigation of the subglacial Lake Vostok in Eastern Antarctica. Dokl. Earth Sci. 2001, 379A, 734–738. [Google Scholar]
- Studinger, M.; Karner, G.D.; Bell, R.E.; Levin, V.; Raymond, C.A.; Tikku, A. Geophysical models for the tectonic framework of the Lake Vostok region East Antarctica. Earth Planet Sci. Lett. 2003, 216, 663–677. [Google Scholar] [CrossRef]
- Wright, A.; Siegert, M.J. The identification and physiographical setting of Antarctic subglacial lakes: An update based on recent discoveries. Geophys. Monogr. Ser. 2011, 192, 9–26. [Google Scholar] [CrossRef]
- Jouzel, J.; Petit, J.R.; Souchez, R.; Barkov, N.I.; Lipenkov, V.Y.; Raynaud, D.; Stievenard, M.; Vassiliev, N.; Verbeke, V.; Vimeux, F. More than 200 meters of lake ice above subglacial Lake Vostok, Antarctica. Science 1999, 286, 2138–2141. [Google Scholar] [CrossRef]
- Bell, R.; Studinger, M.; Tikku, A.; Castello, J.D. Comparative biological analyses of accretion ice from subglacial Lake Vostok. In Life in Ancient Ice; Castello, J.D., Rogers, S.O., Eds.; Princeton University Press: Princeton, NJ, USA, 2005; pp. 251–267. [Google Scholar]
- Gramling, C. A tiny window opens into Lake Vostok, while a vast continent awaits. Science 2012, 335, 788–789. [Google Scholar] [CrossRef]
- Siegert, M.J.; Ellis-Evans, J.C.; Tranter, M.; Mayer, C.; Petit, J.; Salamatin, A.; Priscu, J.C. Physical, chemical and biological processes in Lake Vostok and other Antarctic subglacial lakes. Nature 2001, 414, 603–609. [Google Scholar]
- Siegert, M.J.; Tranter, M.; Ellis-Evans, J.C.; Priscu, J.C.; Lyons, W.B. The hydrochemistry of Lake Vostok and the potential for life in Antarctic subglacial lakes. Hydrol. Process. 2003, 17, 795–814. [Google Scholar] [CrossRef]
- Bulat, S.A.; Alekhina, I.A.; Lipenkov, V.Y.; Lukin, V.V.; Marie, D.; Petit, J.R. Cell concentrations of microorganisms in glacial and lake ice of the Vostok ice core, East Antarctica. Microbiology 2009, 78, 808–810. [Google Scholar] [CrossRef]
- Christner, B.C.; Royston-Bishop, G.; Foreman, C.M.; Arnold, B.R.; Tranter, M.; Welch, K.A.; Lyons, W.B.; Tsapin, A.I.; Studinger, M.; Priscu, J.C. Limnological conditions in subglacial Lake Vostok, Antarctica. Limnol. Oceanogr. 2006, 51, 2485–2501. [Google Scholar] [CrossRef]
- Abyzov, S.S.; Poglazova, M.N.; Mitskevich, J.N.; Ivanov, M.V. Common features of microorganisms in ancient layers of the Antarctic ice sheet. In Life in Ancient Ice; Castello, J.D., Rogers, S.O., Eds.; Princeton University Press: Princeton, NJ, USA, 2005; pp. 240–250. [Google Scholar]
- Christner, B.C.; Mosley-Thompson, E.; Thompson, L.G.; Reeve, J.N. Isolation of bacteria and 16S rDNAs from Lake Vostok accretion ice. Environ. Micrbiol. 2001, 3, 570–577. [Google Scholar] [CrossRef]
- Christner, B.C.; Mosley-Thompson, E.; Thompson, L.G.; Reeve, J.N. Classification of bacteria in polar and nonpolar global ice. In Life in Ancient Ice; Castello, J.D., Rogers, S.O., Eds.; Princeton University Press: Princeton, NJ, USA, 2005; pp. 227–239. [Google Scholar]
- D’Elia, T.; Veerapaneni, R.; Rogers, S.O. Isolation of microbes from Lake Vostok accretion ice. Appl. Environ. Microbiol. 2008, 74, 4962–4965. [Google Scholar] [CrossRef]
- D’Elia, T.; Veerapaneni, R.; Theraisnathan, V.; Rogers, S.O. Isolation of fungi from Lake Vostok accretion ice. Mycologia 2009, 101, 751–763. [Google Scholar] [CrossRef]
- Karl, D.M.; Bird, D.F.; Björkman, K.; Houlihan, T.; Shakelford, R.; Tupas, L. Microorganisms in the accreted ice of Lake Vostok, Antarctica. Science 1999, 286, 2144–2147. [Google Scholar] [CrossRef]
- Priscu, J.C.; Adams, E.E.; Lyons, W.B.; Voytek, M.A.; Mogk, D.W.; Brown, R.L.; McKay, C.P.; Takacs, C.D.; Welch, K.A.; Wolf, C.F. Geomicrobiology of subglacial ice above Lake Vostok, Antarctica. Science 1999, 286, 2141–2144. [Google Scholar] [CrossRef]
- Bulat, S.A.; Alekhina, I.A.; Blot, M.; Petit, J.R.; Waggenbach, D.; Lipenkov, V.Y.; Vasilyeva, L.P.; Wloch, D.M.; Raynaud, D. DNA signature of thermophilic bacteria from the aged accretion ice of Lake Vostok, Antarctica: Implications for searching for life in extreme icy environments. Int. J. Astobiol. 2004, 1, 1–12. [Google Scholar]
- Lavire, C.; Normand, P.; Alekhina, I.; Bulat, S.; Prieur, D.; Birrien, J.L.; Fournier, P.; Hänni, C.; Petit, J.R. Presence of Hydrogenophilus thermoluteolus DNA in accretion ice in the subglacial Lake Vostok, Antarctica, assessed using rrs, cbb and hox. Environ. Microbiol. 2006, 8, 2106–2114. [Google Scholar] [CrossRef]
- Shtarkman, Y.M.; Koçer, Z.A.; Edgar, R.; Veerapaneni, R.; D’Elia, T.; Morris, P.F.; Rogers, S.O. Subglacial Lake Vostok (Antarctica) accretion ice contains a diverse set of sequences from aquatic, marine and sediment-inhabiting Bacteria and Eukarya. PLoS One 2012. in revision. [Google Scholar]
- Ferracciolli, F.; Finn, C.A.; Jordan, T.A.; Bell, R.E.; Anderson, L.M.; Damaske, D. East Antarctic rifting triggers uplift of the Gamburtsev Mountains. Nature 2011, 479, 388–392. [Google Scholar] [CrossRef]
- Young, D.A.; Wright, A.P.; Roberts, J.L.; Warner, R.C.; Young, N.W.; Greenbaum, J.S.; Schroeder, D.M.; Holt, J.W.; Sugden, D.E.; Blankenship, D.D. A dynamic early East Antarctic Ice Sheet suggested by ice-covered fjord landscapes. Nature 2011, 474, 72–75. [Google Scholar]
- Ferrer, M.; Werner, J.; Chernikova, T.N.; Barjiela, R.; Fernández, L.; La Cono, V.; Waldmann, J.; Teeling, H.; Golyshina, O.V.; Glöckner, F.O. Unveiling microbial life in the new deep-sea hypersaline Lake Thetis. Part II: A metagenomic study. Environ. Microbiol. 2011, 14, 268–281. [Google Scholar]
- Toth, D.J.; Lerman, A. Stratified lake and ocean brines: Salt movement and time limits of existence. Limnol. Oceanog. 1975, 20, 715–728. [Google Scholar] [CrossRef]
- Bar-Even, A.; Noor, E.; Milo, R. A survey of carbon fixation pathways through a quantitative lens. J. Exp. Bot. 2012, 63, 2325–2342. [Google Scholar] [CrossRef]
- Burgaud, G.; Le Calvez, T.; Arzur, T.D.; Vandenkoornhuyse, P.; Barbier, G. Diversity of culturable marine filamentous fungi from deep-sea hydrothermal vents. Environ. Microbiol. 2009, 11, 1588–1600. [Google Scholar] [CrossRef]
- Bell, E. Life at Extremes: Environments, Organisms and Strategies for Survival; CABI: Cambridge, MA, USA, 2012; p. 576. [Google Scholar]
- Daniel, M.; Cohen, D.M.; Richard, H.; Rosenblatt, R.H.; Moser, H.G. Biology and description of a bythitid fish from deep-sea thermal vents in the tropical eastern Pacific. Deep Sea Res. 1990, 37, 267–283. [Google Scholar] [CrossRef]
- Gaill, F.; Mann, K.; Wiedemann, H.; Engel, J.; Timpl, R. Structural comparison of cuticle and interstitial collagens from annelids living in shallow sea-water and at deep-sea hydrothermal vents. J. Mol. Biol. 1995, 246, 284–294. [Google Scholar] [CrossRef]
- Shank, T.M.; Black, M.B.; Halanych, K.M.; Lutz, R.A.; Vrijenhoek, R.C. Miocene radiation of deep-sea hydeothermal vent shrimp (Caridea: Bresiliidae): Evidence from mitochondrial cytochrome oxidase subunit I. Mol. Phylogenet. Evol. 1999, 13, 244–254. [Google Scholar] [CrossRef]
- Tunnicliffe, V. The biology of hydrothermal vents: Ecology and evolution. Oceanogr. Mar. Biol. 1991, 29, 319–407. [Google Scholar]
- Tunnicliffe, V.; McArthur, A.G.; McHugh, D. A biogeographical perspective of the deep-sea hydrothermal vent fauna. Adv. Mar. Biol. 1998, 34, 353–442. [Google Scholar] [CrossRef]
- Vishnivetskaya, T.A.; Erokhina, L.G.; Spirina, E.V.; Shatilovich, A.V.; Vorobyova, E.A.; Tsapin, A.; Gilichinsky, D. Viable phototrophs: Cyanobacteria and green algae from the permafrost darkness. In Life in Ancient Ice; Castello, J.D., Rogers, S.O., Eds.; Princeton University Press: Princeton, NJ, USA, 2005; pp. 140–158. [Google Scholar]
- Vrijenhoek, R.C. Gene flow and genetic diversity in naturally fragmented metapopulations of deep-sea thermal vent animals. J. Hered. 1997, 88, 285–293. [Google Scholar] [CrossRef]
- Tarasov, V.G.; Gebruk, A.V.; Mironov, A.N.; Moskalev, L.I. Deep-sea and shallow-water hydrothermal vent communities: Two different phenomena? Chem. Geol. 2005, 224, 5–39. [Google Scholar] [CrossRef]
- Zachos, J.; Pagani, M.; Sloan, L.; Thomas, E.; Billups, K. Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present. Science 2001, 292, 686–693. [Google Scholar] [CrossRef]
- Brambilla, E.; Hippe, H.; Hagelstein, A.; Tindall, B.J.; Stackebrandt, E. 16S rDNA diversity of cultured and uncultured prokaryotes of a mat sample from Lake Fryxell, McMurdo Dry Valleys, Antarctica. Extremophiles 2001, 5, 23–33. [Google Scholar] [CrossRef]
- Clocksin, K.M.; Jung, D.O.; Madigan, M.T. Cold-Active Chemoorganotrophic Bacteria from Permanently Ice-Covered Lake Hoare, McMurdo Dry Valleys, Antarctica. Appl. Environ. Microb. 2007, 73, 3077–3083. [Google Scholar] [CrossRef]
- Laybourn-Parry, J.; Pearce, D.A. The biodiversity and ecology of Antarctic lakes: Models for evolution. Philos. Trans. Roy. Soc. B 2007, 362, 2273–2289. [Google Scholar] [CrossRef]
- Mosier, A.C.; Murray, A.E.; Fritsen, C.H. Microbiota within the perennial ice cover of Lake Vida, Antarctica. FEMS Microbiol. Ecol. 2007, 59, 274–288. [Google Scholar] [CrossRef]
- Kalyuzhnaya, M.G.; lsapidus, A.; Ivanova, N.; Copeland, A.C.; McHardy, A.C.; Szeto, E.; Salamov, A.; Grigoriev, I.V.; Suciu, D.; Levine, S.R. High-resolution metagenomics targets specific functional types in complex microbial communities. Nat. Biotechnol. 2008, 26, 1029–1034. [Google Scholar] [CrossRef]
- Kemp, P.F.; Aller, J.Y. Estimating prokaryotic diversity: When are 16S rDNA libraries large enough? Limnol. Oceanogr. 2004, 2, 114–125. [Google Scholar] [CrossRef]
- Newton, R.J.; Jones, S.E.; Eiler, A.; McMahon, K.D.; Bertlisson, S. A guide to the natural history of freshwater lake bacteria. Microbiol. Mol. Biol. 2011, 75, 14–49. [Google Scholar] [CrossRef]
- Ravenschlag, K.; Sahm, K.; Pernthaler, J.; Amann, R. High Bacterial Diversity in Permanently Cold Marine Sediments. Appl. Environ. Microb. 1999, 65, 3982–3989. [Google Scholar]
- Rogers, S.O.; Ma, L.J.; Zhao, Y.; Catranis, C.M.; Starmer, W.T.; Castello, J.D. Recommendations for elimination of contaminants and authentication of isolates in ancient ice cores. In Life in Ancient Ice; Castello, J.D., Rogers, S.O., Eds.; Princeton University Press: Princeton, NJ, USA, 2005; pp. 5–21. [Google Scholar]
- Rogers, S.O.; Theraisnathan, V.; Ma, L.J.; Zhao, Y.; Zhang, G.; Shin, S.-G.; Castello, J.; Starmer, W. Comparisons of protocols to decontaminate environmental ice samples for biological and molecular examinations. Appl. Environ. Microbiol. 2005, 70, 2540–2544. [Google Scholar]
- Chevreux, B.; Wetter, T.; Suhai, S. Genome sequence assembly using trace signals and additional sequence information, Computer Science and Biology. In Proceedings of the German Conference on Bioinformatics (GCB), Hannover, Germany, 4–6 October 1999; pp. 45–56.
- Meyer, F.; Paarmann, D.; D’Souza, M.; Olson, R.; Glass, E.M.; Kubal, M.; Paczian, T.; Rodriguez, A.; Stevens, R.; Wilke, A. The Metagenomics RAST server—A public resource for the automatic phylogenetic and functional analysis of metagenomes. BMC Bioinforma. 2008, 9, 386. [Google Scholar] [CrossRef]
- Goecks, J.; Nekrutenko, A.; Taylor, J. The Galaxy Team. Galaxy: A comprehensive approach for supporting accessible, reproducible, and transparent computational research in the life sciences. Genome Biol. 2010, 11, R86. [Google Scholar] [CrossRef]
- Moriya, Y.; Itoh, M.; Okuda, S.; Yoshizawa, A.C.; Kanehisa, K. KAAS: An automatic genome annotation and pathway reconstruction server. Nucleic Acids Res. 2007, 35, W182–W185. [Google Scholar]
© 2013 by the authors; licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution license (http://creativecommons.org/licenses/by/3.0/).