Cultureable bacterial diversity of previously unexplored Siachen glacier, Pakistan, was studied. Out of 50 isolates 33 (66%) were Gram negative and 17 (34%) Gram positive. About half of the isolates were pigment producers and were able to grow at 4–37°C. 16S rRNA gene sequences revealed Gram negative bacteria dominated by Proteobacteria (especially γ-proteobacteria and β-proteobacteria) and Flavobacteria. The genus Pseudomonas (51.51%, 17) was dominant among γ- proteobacteria. β-proteobacteria constituted 4 (12.12%) Alcaligenes and 4 (12.12%) Janthinobacterium strains. Among Gram positive bacteria, phylum Actinobacteria, Rhodococcus (23.52%, 4) and Arthrobacter (23.52%, 4) were the dominating genra. Other bacteria belonged to Phylum Firmicutes with representative genus Carnobacterium (11.76%, 2) and 4 isolates represented 4 genera Bacillus, Lysinibacillus, Staphylococcus and Planomicrobium. Most of the Gram negative bacteria were moderate halophiles, while most of the Gram positives were extreme halophiles and were able to grow up to 6.12 M of NaCl. More than 2/3 of the isolates showed antimicrobial activity against multidrug resistant S. aureus, E. coli, Klebsiella pneumonia, Enterococcus faecium, Candida albicans, Aspergillus flavus and Aspergillus fumigatus and ATCC strains. Gram positive bacteria (94.11%) were more resistant to heavy metals as compared to Gram negative (78.79%) and showed maximum tolerance against iron and least tolerance against mercury.
Citation: Rafiq M, Hayat M, Anesio AM, Jamil SUU, Hassan N, Shah AA, et al. (2017) Recovery of metallo-tolerant and antibiotic resistant psychrophilic bacteria from Siachen glacier, Pakistan. PLoS ONE 12(7): e0178180. https://doi.org/10.1371/journal.pone.0178180
Editor: William M. Shafer, Emory University School of Medicine, UNITED STATES
Received: January 21, 2017; Accepted: May 9, 2017; Published: July 26, 2017
Copyright: © 2017 Rafiq et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Data Availability: All relevant data are within the manuscript and the Sequences of all isolates described in this study were deposited in NCBI under the accession number KX128918 through KX128967.
Funding: The funds were provided for the research, but no funds for the publication charges. The research grant was from, Higher Education Commission, Pakistan, fellowship for Muhammad Rafiq. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Glaciers are a huge mass of moving ice that runs slowly over the land. Generally, glaciers are stable bodies of ice that consist mostly of re-crystallized snow that displays evidence of depressed slope or outward movement due to gravity. In a glacier bionetwork, microorganisms play significant role in cycling of carbon, subglacial weathering  and other nutrients. For example, snow algae act as primary producer that sustain heterotrophic population on glaciers, such as copepods, insects, fungi and bacteria . Organic carbon is trapped deep in the glacial ice, microbes metabolize it and form methane , a greenhouse gas. This conversion of carbon to methane could be of significance in climate change . Subglacial microbes perform mineral weathering  and make available minerals and other nutrients for fellow life forms. Moss can survive for centuries underneath glaciers, and recolonizes land as the ice retreats . There is a potent connection between geochemical signatures in subglacial materials and the metabolic processes occurring in that environment. Studies of glaciers and other habitats of permanent snow and ice have shown a diverse range of cold tolerant organisms [2, 7]. Previously glacial ice was considered biologically inactive or life-entrapping medium that collects and preserves microorganisms that are deposited through rain or snow . Scientists have discovered that glaciers can be a favorable environment to support active and diverse communities of micro- as well as macrobiota [9, 10]. The presence of bacteria in polar and non-polar glaciers have been reported by many researchers through both culture-dependent and culture-independent techniques [11–13]. Dormant and vegetative forms of bacteria exist under ice of glacier and are adapted to this unique ecosystem by one or more diverse mechanisms . Comparison of geographically distinct glaciers worldwide have shown a great variation in microbial biomass and community structure [15–17] which is mainly controlled by climatic and environmental factors, including geographic location [1, 18] wind direction, wind speed, light intensity, and availability of nutrients and liquid water . There is some limited evidence of biogeographic effects on the distribution of microorganisms in the geographically distinct glaciers [15–17, 20] and the factors driving the dynamics of microbial community in glacial systems are still not clear.
Many scientists have reported a number of bacterial species including Pedobacter himalayensis , Exiguobacterium indicum , Dyadobacter hamtensis , Leifsonia pindariensis, Bacillus cecembensis , Cryobacterium roopkundense , Cryobacterium pindariense  and Paenibacillus glacialis  from snow, water, soil and sediments of glaciers located in Himalaya. Baghel et al  reported the psychrotrophic proteolytic bacteria from Gangotri Glacier, Western Himalaya, India. Bacterial populations in Roopkund Glacier, Himalayan mountain ranges, were studied by Branda et al. . They found Actinobacteria as the predominant class, followed by β- proteobacteria. Actinobacteria are potent producers of antimicrobial compounds and thus can have dominant role in generating a stress on other microbial life. Bacterial diversity of soil samples from Drass, India a coldest place after Siberia, was explored and screened for various hydrolytic enzymes . Phylogenetic analysis revealed 40 different bacteria, grouped into three major phyla, Proteobacteria, Actinobacteria and Firmicutes differentiated into 17 different genera. These isolates were also investigated for production of hydrolases at 4–30°C. All the isolates secreted one or the other hydrolytic enzyme, i.e. esterase (90%), lipase (80%), protease (32.5%), amylase (20%) and cellulase (17.5%). These results indicate that culturable bacteria in soil of Drass could serve as an ideal candidate for enzyme bioprospecting.
Dumping of non-biodegradable waste in large quantities and the use of arms and ammunition have considerably affected the ecosystem of the region . The troops on the glacier dump the waste in the crevasses of the glacier. About 40% of the waste at the glacier is plastic and metals including cobalt, cadmium and chromium that affects water of the Shyok River (which enters Indus River near Skardu). The water of Indus is used for drinking and irrigation [31, 32]
The aim of the present study was to isolate bacteria from Siachen glacier, Pakistan, and to characterize the strains on basis of different physiological characteristics and determine antibiotic and metal resistance and their antimicrobial activity.
Materials and methods
The area from where the samples were collected was not inside the private land. The sampling sites were accessed with support of people of the local community, and the procedures did not involve any disturbance to endangered or protected species of animals or vegetation. Three types of samples (glacial ice, glacial melt water and glacial sediment) were collected from Siachen glacier, Pakistan (35°25′16″N 77°06′34″E/35.421226°N77.109540°E Google map coordinates of the glacier, not specifically of the sampling site) in sterile bottles and transported to the laboratory at the Department of Microbiology, Quaid-i-Azam University, Islamabad. The samples were processed for isolation of bacterial strains following standard microbiological protocols. The samples were stored at low temperature till further analysis. Temperature and pH of sample site were also recorded.
Reagents and chemicals
Media, sodium chloride, metal salts, H2SO4, HCl and NaCl were obtained from Sigma Chemicals Co. (St. Louis, MO, USA). Antibiotic discs were from (Oxoid, Limited, Basingstoke, Hampshire, England).
Total viable count
Total viable count of the samples was determined by calculating colony forming units (CFU) per ml or g for each sample. About 200 μl of melted ice, sediment or glacial water samples were spread on R2A medium. Water and ice samples were diluted to 1:10 by adding 1 ml sample in tubes containing 9 ml sterile saline, while sediment sample was diluted by adding 1 g in 10 ml normal saline. All the plates were incubated at two different temperatures 4°C and 15°C for about 60 days. Number of culturable bacteria was estimated by counting the average colony formation units (CFU/ml or g) on individually R2A agar plate. Characteristic bacterial colonies with visually different morphologies were chosen and subcultured to obtain pure colonies.
Isolation and identification of bacteria
The isolation and characterization of culturable bacterial isolates wwas performed according to Zang et al. . About 50 distinct colonies were identified according to phenotypic properties like (colony morphology, growth properties pigment production), physiological characteristics (pH, temperature range, sodium chloride tolerance) and 16S rRNA gene sequencing.
In the current study, a total of all the 50 isolates were checked for antibacterial and antifungal activity, metal tolerance and resistance to commonly used antibiotics. The isolates were consistently cultured on LB agar and R2A agar and stored as glycerol stocks at -70°C.
DNA extraction, sequencing and phylogenetic analysis
The bacterial DNA was extracted according to protocol previously described by Shivaji et al. . The 16S rRNA sequencing was done by Macrogen Inc. Seoul, Korea. The sequences obtained were further evaluated by comparing the nucleotide sequences available in NCBI database . The evolutionary history was inferred on method based on the Tamura-Nei model . The phylogenetic tree was constructed in MEGA software . at the bootstrap value 1000.
Deposition of accession numbers in NCBI
Sequences of all isolates described in this study were deposited in NCBI (National Center for Biotechnology Information) under the accession numbers from KX128918 to KX128967, as the following:
HS1 KX128918, HS2 KX128919, HS3 KX128920, HS4 KX128921, HS5 KX128922, HS6 KX128923, HS7 KX128924, HS8 KX128925, HS9 KX128926, HS10 KX128927, HS11 KX128928, HS13 KX128929, HS14 KX128930, HS16 KX128931, HS17 KX128932, HS18 KX128933, HS19 KX128934, HS21 KX128935, HS22 KX128936, HS23 KX128937, HS24 KX128938, HS25 KX128939, HS26 KX128940, HS27 KX128941, HS28 KX128942, HS29 KX128943, HS30 KX128944, LS1 KX128945, LS2 KX128946, LS3 KX128947, LS4 KX128948, LS5 KX128949, LS7 KX128950, LS8 KX128951, LS15 KX128952, LS16 KX128953, LS17 KX128954, LS18 KX128955, LS19 KX128956, LS20 KX128957, LS22 KX128958, LS23 KX128959, LS24 KX128960, LS25 KX128961, LS26 KX128962, LS27 KX128963, LS29 KX128964, LS30 KX128965, LS35 KX128966, LS36 KX128967.
Antimicrobial susceptibility was evaluated through disk diffusion method following the guidelines of the Clinical and Laboratory Standards Institute CLSI, 2013. A total of 9 antibiotics representing different classes; colistin sulphate (CT 10 μg); sulfamethoxazole/trimethoprim (SXT 23.75/1.25 μg), clindamycin (DA 2 μg), Ofloxacin (OFX 5 μg), imipenem (IMI 10 μg), cefotaxime (CTX 30 μg), nalidixic acid (NA 30 μg), Vancomycin (VA 30 μg) and Methicillin (ME 5 μg) were used for determination of antibiotic resistance.
Multiple Antibiotic Resistance index was calculated using formula: where “a” represents the number of antibiotics to which the isolates were resistant, while “b” represents the total number of antibiotics used.
Metal tolerance was checked by prepared stock solutions (4000 ppm) of each heavy metal. The minimum inhibitory concentration (MIC) of heavy metals was determined using LB medium (Sigma) containing Cd+2, Cr+3, Hg+2, Fe+3, Ar+3 and Ni+3 (5–1300 ppm). The metals were supplemented as CdCl2. 2H2O, CrCl3, HgCL2, FeCl2, ArCl3 and NiCl3. The isolates were considered resistant when the MIC values exceeded that of E. coli and S. aureus used as a control.
Screening for antimicrobial activity
The antimicrobial activity was determined by spot on lawn assay. Briefly, the cell suspensions of bacteria, Candida and fungal spores were prepared according to 0.5 McFarland standard and were spread on Muller-Hinton agar and ~ 5 μL of each isolate was spot inoculated and the plates were incubated at 15°C for 72 to 96 hours. A clear zone of inhibition around the indicator organism indicated the antagonistic effect.
In order to screen the isolates for antimicrobial activity, drug resistant bacterial, fungal and bacterial ATCC cultures were used as test organisms. Multidrug resistant isolates including S. aureus, E. coli, Klebsiella pneumoniae, Enterococcus faecium, Candida albicans, Aspergillus flavus and Aspergillus fumigatus, and ATCC strains of S. aureus (ATCC6538), E. coli (ATCC10536) and Pseudomonas aeruginosa (ATCC27853) were used as indicator microorganisms. The MDR (multi drug resistant) strains were obtained from Medical Microbiology Laboratory, Department of Microbiology, Quaid-i-Azam University, Islamabad.
Recovery of bacteria
Out of three samples, the richest source of bacteria in terms of CFU/g or mlwas glacial sediment, followed by melt water and ice, respectively. The number of viable cells was slightly higher at 15°C as compared to 4°C (Table 1). On the basis of colony morphology, a total of 50 bacterial strains were isolated from all samples of Siachen glacier. A total of 23 isolates were obtained at 4°C and 27 at 15°C. On the basis of different colony morphology, 24 isolates were recovered from glacial sediment, 14 from melt water and 12 from glacial ice (Table 1).
Microscopic, morphological and physiological identification
Identification and classification of bacterial isolates was done according to Zhang et al. . The isolates were placed in two distinct groups on the basis of microscopic analysis. Gram negative bacterial isolates [66% (33)] were more prevalent than Gram positive [34% (17)] bacteria. Almost half of the isolates were observed to produce pigments.
All the isolates could grow at temperature ranging from 4°C to 37°C, however, these isolates fail to grow at 45°C. Among Gram negative bacteria, 81.81% (27 isolates) did not show growth at 37°C, while 6.06% (2 isolates) failed to grow at 15°C and 6.06% (2 isolates) were unable to grow at 4°C. Among Gram positive bacteria 41.17% (7 isolates) were unable to grow at 37°C, 5.88% (1 isolate) and 11.76% (2 isolates) could not grow at 15 and 4°C, respectively.
All the strains showed a remarkable level of tolerance to increasing concentrations of NaCl [from 0.9 to 36% (0.14–6.12 M)]. The NaCl tolerance ranging from 0.15–1.33 M (0.9–8%) was observed in 14 (42.42%) Gram negative bacteria, 15 (45.45%) isolates showed growth at NaCl ranging from 1.33–3.4 M (8 to 20%), while 4 (12.12%) isolates showed tolerance to 3.4–6.12 M (20–36%) concentration of NaCl. Of Gram positive bacteria a single bacterial isolate (5.88%) showed growth at 0.9–2% (0.15–0.34 M NaCl, 3 (17.64%) isolates showed growth at salt concentration 1.8–3.4 M (8–20%) while, 13 (76.47%) isolates tolerated 22 to 36% (3.74–6.12 M) NaCl concentration (Table 2).
Most of the Gram negative isolates belonged to proteobacteria with predominance of γ- proteobacteria and β-proteobacteria. The genus Pseudomonas (17 isolates) dominated the γ- proteobacteria group, while the other genera belonging to this class were Psychrobacter (2 isolates) and Acinetobacter (1 isolate). The Class β-proteobacteria constitutes 4 isolates of Alcaligenes and 4 isolates of Janthinobacterium, however, a single isolate of genus Afipia belongs to class α-proteobacteria. Similarly, Flavobacteria belonging to phylum Bacteroides was represented by Flavobacterium (2 isolates), Chryseobacterium (1 isolate) and 1 novel isolate (Table 3). Gram positive isolates belonging to phylum and class Actinobacteria with dominating genera of Rhodococcus (4 isolates), Arthrobacter (4 isolates), Leucobacter (2 isolates) and Brevibacterium (1 isolate), while Firmicutes with representative genera Carnobacterium (2 isolates) and 4 isolates representing 4 genera including Bacillus, Lysinibacillus, Staphylococcus and Planomicrobium.
The evolutionary history was inferred by using the Maximum Likelihood method based on the Tamura-Nei model 42. The tree with the highest log likelihood (-4713.0244) is shown. The percentage of trees in which the associated taxa clustered together is shown next to the branches. Initial tree(s) for the heuristic search were obtained automatically by applying Neighbor-Join and BioNJ algorithms to a matrix of pairwise distances estimated using the Maximum Composite Likelihood (MCL) approach, and then selecting the topology with superior log likelihood value. The tree is drawn to scale, with branch lengths measured in the number of substitutions per site. The analysis involved 53 nucleotide sequences. Codon positions included were 1st + 2nd + 3rd + Noncoding. All positions containing gaps and missing data were eliminated. There were a total of 593 positions in the final dataset. Evolutionary analyses were conducted in MEGA6. The phylogenetic tree of both High and Low temperature isolates are given in Fig 1 & Fig 2.
A total of 9 antibiotics (5 broad spectrum antibiotics, 2 antibiotics against Gram positive and 2 against Gram negative bacteria) were used to evaluate the antibiotic resistance pattern of all the isolates. Interestingly, these isolates showed some varying resistance to all antibiotics used in the current study.
Among Gram negative study isolates, more resistance was found against imipenem (51.51%, 17 isolates) then cefotaxime (CTX) and clindamycin (DA) each 45.45%, (15 isolates) followed by resistance to Ofloxacin (OFX) 24.24%, 8 isolates. Only 21.21%, (7 isolates) showed resistance to colistin sulphate (CT), 15.15%, 5 isolates were resistant to Nalidixic acid, while 12.12%, 4 isolates were resistant to sulfamethoxazole/trimethoprim (SXT). The Gram positive isolates were highly resistant to majority of the antibiotics. Resistance to cefotaxime (CTX) was more prevalent in 76.47% (13 isolates) followed by resistance to imipenem and Vancomycin in 64.70%, 11 strains each. Resistance to CTX and Methicillin was observed in 58.82% (10 isolates). Only (11.76%, 2 isolates showed resistance to Ofloxacin while all the isolates were sensitive to combination of sulphamethaxazole/trimethoprim (Table 3)
Multiple antibiotic resistance (MAR) index
Multiple antibiotic resistance index was determined.Among Gram negative bacteria, 78.79% (26 isolates) showed multiple antibiotic resistance, 9.09% (3 isolates) showed resistance to 1 antibiotic and 12.12% (4 isolates) were sensitive to all antibiotics (Table 4). About 94.11% (16 isolates) Gram positive bacteria showed multiple antibiotic resistance, while 5.89% (1 isolate) showed resistance to a single antibiotic (Table 5).
Screening for antimicrobial activity
All the 50 isolates were screened for their antimicrobial activity. Among Gram negative bacteria, 13 (39.39%) isolates showed antimicrobial activity against 4 or more than 4 test strains, while 3 distinct isolates showed inhibitory effects against 1, 2 and 3 isolates. About 3 (17.64%) Gram positive bacteria showed antimicrobial activity against 1 test strain, 3 (17.64%) showed activity against 3 and 2 (11.76%) of the isolates showed antimicrobial activity against 4 or more than 4 test strains (Tables 4 & 5).
All isolates were screened for their tolerance against 6 different metal ions and minimum inhibitory concentration was determined. Among Gram negative bacteria the minimum inhibitory concentration of Cadmium were 651–850 ppm in (36.36%, 12 isolates), (39.39%, 13 isolates) and (54.54%, 18 isolates) showed tolerance to 651–850 ppm of chromium and nickel respectively, 27.27%, 9 isolates tolerate arsenic level ranging from 851–1050, and (27.27%, 9 isolates tolerate iron level greater than 1050 ppm, however the MIC level in case of Mercury was ≤ 50 in 18 (54.54%) isolates. Of Gram positive bacteria 8, 47.05% isolates showed tolerance to cadmium and 6 (35.29%) showed tolerance to nickel, in the range of 651–850 ppm. Minimum inhibitory concentration of chromium was 451–651 ppm in 5 isolates while 5 (29.41%) isolates showed tolerance to 851–1050 ppm of cadmium. A minimum inhibitory concentration of arsenic and iron ranging from (851–1050 ppm) was noted in 6 (35.29%) and 7 (41.17%) isolates respectively. The MIC of mercury was ≤ 50 in 11 (64.70%) while the highest tolerable level was observed ˂ 120 ppm in mercury. Comparative analysis of both Gram positive and Gram negative bacterial strains is given in Table 6.
To our understanding, this is the first report regarding the diversity of antibiotic producing, metallo- tolerant and antibiotic resistant bacteria isolated from Siachen glacier. In the current research work, A total 50 islates from 3 different samples of glacial ice, melt water and sediment were recovered. Sediment had the highest number because it is known to contain numerous nutrients and have slightly higher temperature  as compared to ice and glacial melt water. It is also obsereved that Gram negative bacteria were more dominant and abundant as compared to Gram positive bacteria, which is in a close association with previous studies [38, 39, 40] that also reported high prevalence of Gram negative bacteria with predominance of γ-proteobacteria, α-proteobacteria and β-proteobacteria. The dominance of bacterial diversity in a particular glacier or cold environments might be due to the seasonal variation in glaciers which can counter-select the bacteria with greater adaptability. Boetius et al.  identified bacterial isolates with greater abundance of Gram positive bacteria which is contradictory to our finding. The predominance of Gram negative bacteria in the current study could be related to the psychrophilic nature of Gram negative bacteria, as psychrophiles have been reported to grow faster and out-compete psychrotrophic bacteria .
There was a significant difference in terms of growth range among Gram negative and Gram positive bacteria. Most of the Gram negative bacteria (78.78%) were able to grow at 15°C, while most of the Gram positive (58.82%) isolates were able to grow at 37°C. According to definition of Turley , the Gram negative bacteria can be placed among psychrophilic, and the Gram positive isolates in psychrotrophic bacteria. Previously, Carpenter et al.  identified bacteria from South Pole snow, all of which were true psychrophiles while Morita  isolated and characterised bacteria from Ellesmere Island ice as psychrotrophs. Around the year the temperature of Siachen valley remains far below 0°C (down to -41°C) to 11°C . It is unclear how these bacteria survive under such a diverse conditions. However, the survival of psychrotrophic bacteria in extremely stressful conditions is due to formation of spores in Gram positive bacteria as described earlier [47–49]. These findings strongly support our study as most of the Gram positive bacteria in our study were psychrotrophic and spore formers. Spore formation might help overcome the stress conditions to low temperature, desiccation and damage of bacteria by UV [50–51]. The possible mechanism of survival in Gram negative bacteria could be associated with upregulation of desaturase genes and increase of membrane lipids like Poly-unsaturated fatty acids (PUFAs) in association with decrease in temperature [52, 53].
Our isolates also showed tolerance to different concentrations of NaCl ranging from 0.14–6.12 M (0.9 to 36%). In active ecological environments in glacial habitats, water nuclei forms inside glacier mass, the solutes around that environment diffuse to this active ecological environment and make it hypertonic . The exposure of bacteria to such conditions leads to salt tolerance. In our isolates the increased tolerance could be due to this phenomenon. It is for the first time to report salt tolerance of glacial bacteria above 5.1 molar concentration, although detailed investigation and research is required to investigate the phenomenon of such a high tolerance in depth.
The current research also showed increased antibiotic resistance in our isolates. Previous investigations from pristine cold environments like ancient Siberian permafrost, alpine glacier cryoconite and non-anthropogenic alpine soil [29, 55, 56] opposed our results as bacteria from such environments have been reported to have greater sensitivity to antibiotics. However, wide distribution and multiple antibiotic resistance genes have been previously documented in different glaciers except antarctic glaciers and has been well described by transmission of migratory birds and air borne bacteria .
Our isolates also showed increased tolerance to various metals. Previous reports [58, 59] also supported our findings, however, these earlier studies do not include all the metals used in our studies. This is the first study of Siachen glacier, Pakistan, also include to the intrinsic property of low temperature bacteria to demonstrate metal and antibiotic resistance with antimicrobial activity.
Siachen glacier is known as the world’s highest non-polar glacier and considered as the highest and world’s biggest garbage dump, 40% of which are plastics and metals, worn out gun barrels, splinters from gun shelling, empty fuel barrels and burnt shelters, which permanently pollute glacial ice and water and leach toxins like cobalt, cadmium, chromium and other metals due to unavailability of natural biodegrading agents . The heavy metal tolerance could possibly be due to these pollutants, and could possibly lead to antibiotic resistance too, as metal and antibiotic resistance is often present as co-resistance . On the other hand Siachen glacier is the world’s highest warzones. The antibiotic resistance in such area could also be due to army patrolling that might harbour pathogenic or opportunistic bacteria that can transmit resistance genes to environmental bacteria. The third possible reason for antibiotic resistance is the production of antimicrobial compounds that leads to natural resistance in such bacteria.
About 40% of the isolates produced antimicrobial compounds against American Type Culture Collection (ATCC) and clinical isolates of bacteria, yeasts and molds. Our results are strongly supported by works of previous scientists [31, 62] who identified potent bacterial isolates from diverse cold habitats, a large number of which produced antimicrobial compounds. However, our results are in contrast to the research carried out by many scientists [63–66] on Antarctic, arctic, Argentine soil and marine organisms. The low temperature habitats are less explored as compared to mesophiles and data regarding antimicrobial compounds is very rare. Therefore, it is necessary to study these isolates along with neighbour glaciers, ice caps and glacial lakes to reveal the microbial compounds.
We conclude that the bacteria belonging to diverse groups were present with Pseudomonas as the most dominant genus, with Gram positive more abundant than the Gram negative bacteria. Low temperature adapted bacteria isolated from Siachen glacier, showed varying degree of resistance to metals and commonly used antibiotics and also they showed pronounced ability to inhibit the other ATCC as well as pathogenic bacteria. They were also moderate to extreme halophilic in nature.
- 1. Takeuchi N, Koshima S. A snow algal community on a Patagonian glacier, Tyndall glacier in the southern Patagonia Icefield. Arct Antarct Alpine Res. 2004; 36: 91–98.
- 2. Kohshima S. A novel cold-tolerant insect found in a Himalayan glacier. Nature. 1984; 310: 225–227.
- 3. Boyd ES, Skidmore M, Mitchell AC, Bakermans C, Peters JW. Methanogenesis in subglacial sediments.Environ Microbiol Rep. 2010; 2: 685–692. pmid:23766256
- 4. Wadham JL, Arndt S, Tulaczyk S, Stibal M, Tranter M, Telling J, et al. Potential methane reservoirs beneath Antarctica. Nature. 2012; 488: 633–637. pmid:22932387
- 5. Montross SN, Skidmore M, Tranter M, Kivim AL, Parkes RJ. A microbial driver of chemical weathering in glaciated systems. Geology. 2013; 41: 215–218.
- 6. La-Farge C, Williams KH, England JH. Regeneration of Little Ice Age bryophytes emerging from a polar glacier with implications of totipotency in extreme environments. Proc Nat Acad Sci; 2013.
- 7. Takeuchi N, Uetake J, Fujita K, Aizen V, Nikitin S. A snow algal community on Akkem Glacier in the Russian Altai Mountains. Ann Glaciol. 2006; 43: 378–384.
- 8. Butinar L, Spencer-Martins I, Gunde-Cimerman N. Yeasts in high Arctic glaciers: the discovery of a new habitat for eukaryotic microorganisms. Ant van Leeuwen. 2007; 91(3): 277–289.
- 9. Hodson A, Anesio A M, Tranter M, Fountain A, Osburn M, Priscu J, Laybourn-Parry J, Sattler B. Glacial ecosystems. Ecological Monographs 78, No. 1. 2008: 41–67.
- 10. Anesio AM, Laybourn-Parry J. Glaciers and ice sheets as a biome. Trends Ecol Evol. 2012; 27: 219–225. pmid:22000675
- 11. Mikucki JA, Priscu JC. Bacterial diversity associated with Blood Falls, a subglacial outflow from the Taylor Glacier, Antarctica. Appl Environ Microbiol. 2007; 73: 4029–4039. pmid:17468282
- 12. Kim HJ, Park S, Lee JM, Park S, Jung W, Kang JS, et al. Moritella dasanensis sp. nov., a psychrophilic bacterium isolated from the Arctic ocean. Inter J System Evol Microbiol. 2008; 58: 817–820.
- 13. Baghel VS, Tripathi RD, Ramteke PW, Gopal K, Dwivedi S, Jain RK, Rai UN, Singh SN. Psychrotrophic proteolytic bacteria from cold environment of Gangotri glacier, Western Himalaya, India. Enz Microb Technol. 2005; 36(5): 654–659.
- 14. Miteva VI. Bacteria in snow and glacier ice. In: Marginson R, Schinner F, Marx JC, Gerday C (eds). Psychrophilies: from biodiversity to biotechnology: Springer; New York. 2008; 31–50.
- 15. Liu Y, Yao T, Jiao N, Kang S, Xu B, Zeng Y, Huang S, Liu X. Bacteria diversity in the snow over Tibetan plateau glaciers. Extremophiles. 2009; 13: 411–423. pmid:19159068
- 16. Zhang S, Hou S, Ma X, Qin D, Chen T. Culturable bacteria in Himalayan glacial ice in response to atmospheric circulation. Biogeosci. 2007; 4: 1–9.
- 17. Zhang X, Ma X, Wang N, Yao T. New subgroups of Bacteroidetes and diverse microorganisms in Tibetan plateau glacial ice provide a biological record of environmental conditions. FEMS Microbiol Ecol. 2009; 67: 21–29. pmid:19049497
- 18. Mueller DR, Pollard WH. Gradient analysis of cryoconite ecosystems from two polar glaciers. Pol Biol. 2004; 27: 66–74.
- 19. Bhatia M, Sharp M, Foght J. Distinct bacterial communities exist beneath a high Arctic polythermal glacier. Appl Environ Microbiol. 2006; 72: 5838–5845. pmid:16957202
- 20. Takeuchi N, Uetake J, Fujita K, Aizen V, Nikitin N. A snow algal community on Akkem Glacier in the Russian Altai Mountains. Ann Glaciol. 2006; 43: 378–384.
- 21. Shivaji S, Chaturvedi P, Reddy GS, Suresh K. Pedobacter himalayensis sp. nov., from the Hamta glacier located in the Himalayan mountain ranges of India. Int J Syst Evol Microbiol. 2005; 55:1083–1088. pmid:15879237
- 22. Chaturvedi P, Shivaji S. Exiguobacterium indicum sp. nov., a psychrophilic bacterium from the Hamta glacier of the Himalayan mountain ranges of India. Int J Syst Evol Microbiol. 2006; 56:2765–2770. pmid:17158975
- 23. Chaturvedi P, Reddy GSN, Shivaji S. Dyadobacter hamtensis sp. nov., from Hamta glacier, located in the Himalayas, India. Int J Syst Evol Microbiol. 2005; 55: 2113–2117. pmid:16166718
- 24. Reddy GSN, Prabagaran SR, Shivaji S. Leifsonia pindariensis sp. nov., isolated from the Pindari glacier of the Indian Himalayas, and emended description of the genus Leifsonia. Int J Syst Evol Microbiol. 2008a; 58: 2229–2234.
- 25. Reddy GSN, Pradhan S, Manorama R, Shivaji S. Cryobacterium roopkundense sp. nov., a psychrophilic bacterium from a Himalayan glacier. Int J Syst Evol Microbiol. 2009; 60:866–887.
- 26. Reddy GSN, Pradhan S, Manorama R, Shivaji S. Cryobacterium Pindariense sp. nov., a psychrophilic bacterium from a Himalayan glacier. Int J Syst Evol Microbiol. 2010; 60: 866–870. pmid:19661491
- 27. Kishore KH, Begum Z, Pathan AA, Shivaji S. Paenibacillus glacialos sp. nov., isolated from kafni glacier of Himalayas, India. Int J Syst Evol Microbiol. 2010; 60(Pt 8):1909–1913. pmid:19783613
- 28. Branda E, Turchetti B, Diolaiuti G, Pecci M, Smiraglia C, Buzzini P. Yeast and yeast-like diversity in the southernmost glacier of Europe (Calderone Glacier, Apennines, Italy). FEMS Microbiol Ecol. 2010;72(3): 354–369. pmid:20402775
- 29. Gupta P, Sangwan N, Lal R, Vakhlu J. Bacterial diversity of Drass, cold desert in Western Himalaya, and its comparison with Antarctic and Arctic. Arch Microbiol. 2015;197(6): 851–860. pmid:26055487
- 30. ActionAid (2010). Natural Resource Management In South Asia. Pearson Education. pp 58. ISBN 978–8131729434.
- 31. Kemkar NA. Environmental peacemaking: Ending conflict between India and Pakistan on the Siachen Glacier through the creation of a transboundary peace park. Stanford Environ Law J. 2006; 25 (1): 67–121.
- 32. Fedarko K, Jackson, N, editors. The Coldest War. Outside (Mariah Media Network). ASIN B001OTEIG8. 2003. ISSN 0278–1433.
- 33. Zhang DC, Brouchkov A, Griva G, Schinner F, Margesin R. Isolation and characterization of bacteria from ancient Siberian permafrost sediment. Biology online Journal 2013; 2:64–85.
- 34. Shivaji S, Reddy GSN, Aduri RP, Kutty R, Ravenschlag K. Bacterial diversity of a soil sample from Schirmacher Oasis, Antarctica. Cell Mol Biol. 2004; 50:525–536. pmid:15559969
- 35. Thompson JD, Higgins DG, Gibson TJ. CLUSTAL W: Improving the sensitivity of progressive multiple sequence alignment through sequence weighting, position-specific gap penalties and weight matrix choice. Nuc Acids Res. 1994; 22: 4673–4680.
- 36. Tamura K, Nei M. Estimation of the number of nucleotide substitutions in the control region of mitochondrial DNA in humans and chimpanzees. Mol Biol Evol. 1993; 10:512–526. pmid:8336541
- 37. Parnell J, McMahon S. Physical and chemical controls on habitats for life in the deep subsurface beneath continents and ice. Phil Trans R Soc. 2016; 374: 20140293. http://dx.doi.org/10.1098/rsta.2014.0293
- 38. Tamura K, Stecher G, Peterson D, Filipski A, Kumar S. MEGA6: Molecular Evolutionary Genetics Analysis version 6.0. Mol Biol Evol. 2013; 30:2725–2729. pmid:24132122
- 39. Männistö MK, Häggblom MM. Characterization of psychrotolerant heterotrophic bacteria from Finnish Lapland. Syst Appl Microbiol. 2006; 29(3): 229–243. pmid:16564959
- 40. Musilova M, Tranter M, Bennett SA, Wadham J, Anesio AM. Stable microbial community composition on the Greenland Ice Sheet. Front Microbiol. 2015;6.
- 41. Boetius A, Anesio AM, Deming JW, Mikucki JA, Rapp JZ. Microbial ecology of the cryosphere: sea ice and glacial habitats.Nat Rev Microbiol; 2015.
- 42. Collins RE, Rocap G, Deming JW. Persistence of bacterial and archaeal communities in sea ice through an Arctic winter. Environ Microbiol. 2010; 12:1828–1841. pmid:20192970
- 43. Turley C. Bacteria in the cold deep-sea benthic boundary layer and sediment-water interface of the NE Atlantic. FEMS Microbiol Ecol. 2000; 33:89–99. pmid:10967208
- 44. Carpenter EJ, Lin S, Capone DG. Bacterial activity in South Pole snow. Appl Environ Microbiol. 2000; 66:4514–4517. pmid:11010907
- 45. Morita Y. psychrophilic bacteria. Bacteriol Rev. 1975; 39:144–167. pmid:1095004
- 46. Dancer SJ, Shears P, Platt DJ. Isolation and characterization of coliforms from glacial ice and water in Canada’s high Arctic. J Appl Microbiol. 1997; 82:597–609. pmid:9172401
- 47. https://www.meteoblue.com/en/weather/forecast/modelclimate/siachen-glacier pakistan 1164949
- 48. Sheridan PP, Miteva VI, Brenchley JE, Phylogenetic analysis of anaerobic psychrophilic enrichment cultures obtained from a Greenland glacier ice core. Appl Environ Microbiol. 2003; 69:2153–2160. pmid:12676695
- 49. Miteva VI, Brenchley JE. Detection and isolation of ultrasmall microorganisms from a 120,000-year-old Greenland glacier ice core. Appl Environ Microbiol. 2005; 71:7806–7818. pmid:16332755
- 50. Yung PT, Shafaat HS, Connon SA, Ponce A. Quantification of viable endospores from a Greenland ice core. FEMS Microbiol Ecol. 2007; 59:300–306. pmid:17313579
- 51. Nicholson WL, Munakata N, Horneck G, Melosh HJ, Setlow P. Resistance of Bacillus endospores to extreme terrestrial and extraterrestrial environments. Microbiol Mol Biol Rev. 2000; 64:548–572. pmid:10974126
- 52. Onyenwoke RU, Brill JA, Farahi K, Wiegel J. Sporulation genes in members of the low GþC Gram-type-positive phylogenetic branch (Firmicutes). Arch Microbiol, 2004; 182:182–192. pmid:15340788
- 53. Okuyama H, Orikasa Y, Nishida T, Watanabe K, Morita N. Bacterial genes responsible for the biosynthesis of eicosapentaenoic and docosahexaenoic acids and their heterologous expression. Appl Environ Microbiol. 2007; 73:665–670. pmid:17122401
- 54. Clarke A, Morris GJ, Fonseca F, Murray BJ, Acton E, Price HC. A low temperature limit for life on Earth. PLoS ONE 2013; 8(6): e66207. pmid:23840425
- 55. Bergé JP, Gilles B. Fatty acids from lipids of marine organisms: molecular biodiversity, roles as biomarkers, biologically active compounds, and economical aspects. Mar Biotechnol 2005; 49–125.
- 56. Zhang D, Schumann P, Liu HC, Xin YH, Zhou YG, Schinner F, et al. Arthrobacter alpinus sp. nov., a psychrophilic bacterium isolated from alpine soil. Int J Syst Evol Microbiol. 2010; 60:2149–2153. pmid:19880631
- 57. Zhang D, Busse HJ, Liu HC, Zhou YG, Schinner F, Margesin R. Sphingomonas glacialis sp. nov., a psychrophilic bacterium isolated from alpine glacier cryoconite. Int J Syst Evol Microbiol. 2011; 61:587–591. pmid:20382784
- 58. Segawa T, Takeuchi N, Rivera A, Yamada A, Yoshimura Y, Barcaza G, et al. Distribution of antibiotic resistance genes in glacier environments. Environ Microbiol Rep. 2013; 5:127–134. pmid:23757141
- 59. Mangano S, Luigi M, Caruso C, Giudice AL. Metal and antibiotic resistance in psychrotrophic bacteria associated with the Antarctic sponge Hemigellius pilosus (Kirkpatrick, 1907). Pol Biol. 2014; 37:227–235.
- 60. Tomova I. Characterization of heavy metals resistant heterotrophic bacteria from soils in the Windmill Islands region, Wilkes Land, East Antarctica. Polish Pol Res. 2014; 35(4):593–607.
- 61. Seiler C, Berendonk TU. Heavy metal driven co-selection of antibiotic resistance in soil and water bodies impacted by agriculture and aquaculture. Role and prevalence of antibiosis and the related resistance genes in the environment. 2007:101.
- 62. Hemala L, Zhang D, Margesin R. Cold-active antibacterial and antifungal activities and antibiotic resistance of bacteria isolated from an alpine hydrocarbon-contaminated industrial site. Res Microbiol. 2014; 165:447–456. pmid:24880083
- 63. Dimitrova S, Pavlova K, Lukanov L, Korotkova E, Petrova E, Zagorchev P, Kuncheva M. Production of metabolites with antioxidant and emulsifying properties by Antarctic strain Sporobolomyces salmonicolor AL1. Appl Biochem Biotechnol. 2013;169(1):301–311. pmid:23179285
- 64. Biondi N, Tredici MR, Taton A, Wilmotte A, Hodgson DA, Losi D, et al. Cyanobacteria from benthic mats of Antarctic lakes as a source of new bioactivities. J Appl Microbiol. 2008; 105:105–115. pmid:18217933
- 65. Sanchez LA, Gomez FF, Delgado OD. Cold-adapted microorganisms as a source of new antimicrobials. Extremophiles. 2009; 13: 111–120. pmid:19015813
- 66. O'Brien A, Sharp R, Russell NJ, Roller S. Antarctic bacteria inhibit growth of food-borne microorganisms at low temperatures. FEMS Microbiol Ecol. 2004; 11:157e67.