To elucidate how geothermal irregularities affect the sustainability of high-temperature microbiomes we studied the synecological dynamics of a geothermal microbial mat community (GMMC) vis-à-vis fluctuations in its environment. Spatiotemporally-discrete editions of a photosynthetic GMMC colonizing the travertine mound of a circum-neutral hot spring cluster served as the model-system. In 2010 a strong geyser atop the mound discharged mineral-rich hot water, which nourished a GMMC continuum from the proximal channels (PC) upto the slope environment (SE) along the mound’s western face. In 2011 that geyser extinguished and consequently the erstwhile mats disappeared. Nevertheless, two relatively-weaker vents erupted in the southern slope and their mineral-poor outflow supported a small GMMC patch in the SE. Comparative metagenomics showed that this mat was a relic of the 2010 community, conserved via population dispersal from erstwhile PC as well as SE niches. Subsequently in 2012, as hydrothermal activity augmented in the southern slope, ecological niches widened and the physiologically-heterogeneous components of the 2011 “seed-community” split into PC and SE meta-communities, thereby reclaiming either end of the thermal gradient. Resilience of incumbent populations and the community’s receptiveness towards immigrants, were the key qualities that ensured the GMMC’s sustenance amidst habitat degradation and dispersal to discrete environments.
Despite the wide acceptance of geothermal environments as abodes of ancient lifeforms and facilitators of primordial metabolisms1,2,3,4 it is still unclear how ecological constraints affect the stability and sustainability of high temperature microbiomes. We do not have a precise understanding of how the structures and functions of geothermal microbial communities respond to fluctuating physicochemical conditions of their hydrothermal habitats. Synecological investigation of geothermal communities over time and space becomes more important in view of the ephemeral nature of the geochemistry of hydrothermal systems, which puts a subtle question mark on the feasibility of the hydrothermal origin of life. This was first highlighted when return expeditions to the famous Rose Garden vent field in the East Pacific rise (the first deep-sea hydrothermal vent to be discovered) revealed its total deactivation and consequent annihilation of the associated biodiversity within a decade5,6. Interestingly, during the same expedition, a young vent field in the Rose Garden neighborhood, christened as the Rosebud, was found to support another nascent geothermal community7. Yet, the issue of sustainability of microbial communities thriving on a nutrient source as uncertain as geothermal discharge was never quite adequately addressed with specific geomicrobiological investigations.
In this study we used high-throughput metagenomic techniques to trace the structures and metabolic potentials of a spatiotemporally-erratic geothermal microbial mat community (GMMC) over three consecutive years and correlated the community dynamics data with the physicochemical fluctuations in the environment. In the process we identified those community attributes and niche constraints and opportunities, which collectively helped the GMMC sustain in the face of habitat instabilities. Many aspects of the community dynamics of the present GMMC could find parallels in other microbial communities enduring environmental whimsicalities elsewhere, thereby explaining how microbial populations within community frameworks cope with uncertain habitat conditions in general.
Results and Discussion
Site description and sample identity
The Dhauliganga valley in the Garhwal Himalayas (in the state of Uttarakhand, India) encompasses several circum-neutral hydrothermal vents, which discharge up to 95 °C hot waters having low chlorine and silica content8. The hot spring cluster of our interest, christened as the “Pilgrim Terrace” (PT) after the holy shrines of the nearby areas, is located at Tapovan (30.492542 N / 79.631002 E), 15 km south-east of the Joshimath town on the Malari-Joshimath Road. This site was explored in the November months of 2010, 2011 and 2012 and data gathered thereof constituted the basis of this report. Topographically, PT is a massive mound of hydrothermally deposited travertine interspersed with iron, nickel, aluminium, silver and sulfur. Spatiotemporally unstable vents seated within this mound discharge hot waters with fluctuating vigor and mineral content.
In 2010, vigorous hydrothermal discharge and fumarolic activity occurred from a large geyser situated on the flat top of the PT (Fig. 1A1). Thermal water (95 °C, pH 7.5) ejecting out of this vent (at a flow rate of ~20 l s−1) was rich in thiosulfate, sulfate and ferrous iron (Table 1, Fig. 2A). Active deposition of vertically-laminated red and creamy white sediments (Figure S1A) could be observed around the geyser mouth. Downslope, the laminated pattern gave way to fragile bulbous reddish yellow spherulites that entrapped fumarolic and/or microbially-produced gases (Figure S1B). Hyaline green microbial mats (GMs) grew all along the proximal as well as distal outflow channels (OFC) on the west-facing slope of the PT (area demarcated by green arrows in Fig. 1A1). GMs were sampled from the proximal channels (PC) as 2010_GM_PC and also from the OFC in the slope environment (SE) as 2010_GM_SE (Fig. 1A2).
During our survey in 2011 we found that there was zero discharge from the PT-top geyser as its crater was completely clogged by sinter deposition. Consequently, there was no visible sign of the erstwhile GMMC along the west-facing slope of the PT (Fig. 1B1). Large chunks of the west-slope travertine had already been quarried, exposing hard old sinters from the deeper layers. The active sedimentary fabrics observed in the 2010 PCs were found vividly preserved in the texture of the old sinter layers exposed by fresh vertical cuts (Figure S1C). Elsewhere, on the eroded slopes of the remnant sinter, algae and mosses had started colonizing. Notwithstanding this scenario on the west-face, two relatively-weaker mid-terrace hot water vents were found to have formed anew on the south-facing slope of the PT where there was neither any hydrothermal feature nor any microbial mat in the previous year. Both had flow rates of ~4 l s−1, temperatures ~85 °C and pH 7.0. Their combined mineral-poor outflow (Table 1, Fig. 2A) drained down the southern slope and supported a small patch of deep green mat (sampled as 2011_GM_SE) on the thin layer of freshly-precipitated travertine (Fig. 1B2). Noticeably, this was the only visible counterpart of the sprawling 2010 GMMC in the entire PT microbiome of 2011.
Until 2012, there was no revival of the PT-top geyser (Fig. 1C1) and the western slope had started hosting angiospermous herbs (Figure S1D). However, hydrothermal manifestations in the southern slope had gained momentum as the two vents of 2011 origin had become more vigorous (flow rates ~6 l s1, 85–90 °C, pH 7.0–7.25) and just beneath the dead cavern of the 2010 geyser a small mud pool (~85 °C; pH 8.0) and a very strong but small vent (flow rate ~8 l s−1, ~95 °C, pH 7.5) formed anew. Discharge from this new vent joined the combined OFC of the 2011 vents below; and together the three created an outflow more vigorous and mineral-rich than last year. A small patch of deep green mat (sampled as 2012_GM_PC) grew on the PC close to the vents of 2011-origin (Fig. 1C2), while a couple of discrete GM stretches (sample 2012_GM_SE) also grew along the OFC in the SE.
Rationale of the study and work-plan
For all practical purposes, our central objective was to know whether the small GM_SE patch of 2011 was a remnant of the expansive 2010 GMMC and then whether the two niche-partitioned mats (GM_PC and GM_SE) of 2012 were derivatives of that 2011 GM_SE propagule. If these conjectures were found to be incorrect then it was imperative to confirm whether the 2011 and/or 2012 mats were distinct pioneer communities trying to colonize the PT afresh. It is further noteworthy that even if there was a spatiotemporal dispersal of the original west-slope community to the southern slope, its structure and function(s) were most likely to undergo alterations owing to the differences in the physicochemical conditions of the two sites. As such, the two types of changes needed to be identified and their potential correlations investigated.
Now, over the three assessment years five mat samples were retrieved from two distinct ecological niches, viz. the PC and SE OFCs. Incidentally, the SE niche was consistently occupied by mats throughout the study period but the PC niche was vacant in-between. Accordingly, the three GM_SE editions were chosen as the central models of this investigation and studied by both (i) shotgun metagenome analysis and (ii) amplified 16 S rDNA V3 sequence analysis. The two GM_PCs, on the other hand, were investigated mainly for comparative purposes and V3 sequence-based taxonomic diversity analysis was sufficient for the same.
Bacterial predominance in the GM_SE
>1 Gb metagenomic sequence was generated for each GM_SE sample and used to draw synecological inferences (Table S1). As such, percentage distribution of metagenomic reads over various groups of a particular taxonomic category was considered as a direct measure of the relative abundance of those groups. Initially, reads were classified up to the domain level (Fig. 3A) by searching against the non-redundant (nr) protein database using the Organism Abundance tool of MG-RAST. Similarly, 16S rRNA gene (rDNA) reads within the datasets were classified by searching against the RDP database using the same tool (Fig. 3B). Read distribution patterns obtained from either analysis was broadly in agreement with each other. Unassigned and unclassified sequences constituted ~15% of every metagenome, while reads assigned to eukaryotes made up only 0.2–0.8% and those attributable to viruses were <0.05%. Archaeal contribution in the GM_SE metagenomes of 2010, 2011 and 2012 was 0.01%, 1% and 0.5% respectively.
Whatever little archaeal reads were there in the 2010 dataset were all attributable to Euryarchaeota. In contrast, out of the 1% archaeal share in the 2011_GM_SE metagenome, 0.37% came from Thaumarchaeota, 0.32% from Euryarchaeota and 0.29% from Crenarchaeota. In 2012_GM_SE Euryarchaeota was the predominant phylum accounting for 0.23% of the total 0.5% archaeal share in the community. Out of the remaining 0.27%, Thaumarchaeota alone contributed 0.2%, while Crenarchaeota put in 0.07%. In both the 2011 and 2012 GM_SEs the thaumarchaeon Nitrosopumilus was the dominant genus accounting for 18–20% of all archaeal reads. Two other thaumarchaea Cenarchaeum and Nitrososphaera, alongside the Euryarchaeota member Methanosarcina, were the other dominant constituents of the 2011 and 2012 archaeal populations, collectively accounting for another 18% and 20% of all archaeal reads in the respective datasets. The exceptional hike in the proportion of Crenarchaeota in 2011_GM_SE was mainly due to increased representation of Pyrobaculum, which contributed ~50% of the all Crenarchaeota reads in this sample.
98–99% of the taxonomically classifiable reads of all three GM_SE editions were from Bacteria. Hence it was deemed appropriate to focus only on bacterial community dynamics for the rest of the study.
Bacterial community dynamics in the GM_SE
A broad consensus was witnessed between the pictures of phylum-level read abundance emerging from comparison against the RDP (Fig. 3C) and the nr protein (Fig. 3D; Table S2) databases. As illustrated by these figures, the three GM_SE editions varied considerably in the relative abundance of the various bacterial phyla. The 2011 edition showed maximum heterogeneity, while 2010_GM_SE was the least diversified. Proteobacteria dominated all the three GM_SEs, but the extent of their predominance was exceptionally high in 2010_GM_SE where 95% of all reads were ascribed to this phylum. The only other phylum having >1% representation in 2010 was Actinobacteria. Again, within Proteobacteria, Alphaproteobacteria was always the most abundant class except in 2010_GM_SE where Betaproteobacteria predominated (Fig. 3E). There was a sharp decline in the abundance of Proteobacteria in 2011_GM_SE where ~41% of total classifiable reads were affiliated to the phylum. This was accompanied by remarkable upturns in the representation of Chloroflexi, Bacteroidetes, Cyanobacteria, Firmicutes, Nitrospirae, Verrucomicrobia, Chlorobi, Deinococcus-Thermus, Acidobacteria and Planctomycetes. Several marginal phyla, which did not have >1% representation in any of the three GM_SE metagenomes, also increased their abundance by ≥10 times (Fig. 2B; Table S2). Interestingly again, Proteobacteria rebounded in 2012, complemented by concomitant fall in the abundance of many of those phyla which had surged in 2011. Notably, Actinobacteria was the only phylum whose oscillation was in sync with this trend of Proteobacteria. On the other hand, most of the phyla that had increased their representation in 2011_GM_SE could not hold on to their gains in 2012. Chloroflexi and Deinococcus-Thermus were the biggest casualties of proteobacterial resurgence in 2012, suffering maximum losses and retreating almost back to their 2010 levels. Cyanobacteria, Chlorobi, Nitrospirae, Gemmatimonadetes, Planctomycetes, Spirochaetes and Acidobacteria also experienced considerable downturn between 2011 and 2012, but were still above their 2010 levels. Firmicutes suffered minimum cutback from their 2011 level, whereas only Bacteroidetes and Verrucomicrobia managed to further increase their representations in 2012.
Different mathematical indices were calculated (Table S3 A through S3 C) to quantify the phylum-level ecological diversity (which involves ‘what types’ as well as ‘how many’) of the GM_SEs. Corroborating the relative abundance trends of Fig. 3, Simpson dominance index D was exceptionally high for 2010_GM_SE (0.95), moderate for 2012_GM_SE (0.44) and lowest for 2011_GM_SE (0.22) (Fig. 4A). Expectedly, fluctuations of Shannon diversity index H (Fig. 4B) and Shannon equitability index EH (Fig. 4C) were inverse to the trend observed for D.
Concurrence between genus- and phylum-level trends
It was remarkable to observe that >50% of all taxonomically classifiable reads of any given GM_SE metagenome were assigned to the 50 most-abundant putative genera identified in that metagenome (Fig. 5). In 2010_GM_SE, top-50 genera accounted for ~80% of all classifiable reads, thereby justifying its high dominance index D. In 2011 and 2012 GM_SE respectively top-50 genera accounted for 56% and 58% of all classifiable reads. Interestingly again, year-on-year constancies and fluctuations exhibited by the top-50 genera mirrored the trends observed for the relative abundance of GM_SE phyla in Fig. 3D. As a mark of stability, 13 names (written in green font in Fig. 5) were common to all the three top-50 generic lists (referred to hereafter as the ‘leaderboard’). The leaderboard of 2010_GM_SE (Fig. 5A) encompassed representatives from only two phyla, while that of 2011_GM_SE (Fig. 5B) was taxonomically most inclusive (encompassing genera from eight phyla), followed by that of 2012_GM_SE that included genera from five different phyla (Fig. 5C). These data also corroborated the synecological indices of the three GM_SE editions.
In 2010_GM_SE, all but only one genus in the top-50 were from Proteobacteria. Apart from the 13 genera common to all three leaderboards and the single genus Azoarcus that was common to the 2010 and 2011 GM_SEs, the rest of the 36 members of the 2010_GM_SE leaderboard dropped from the corresponding list of 2011. Interestingly, 10 out of these 36 (names in blue font in Fig. 5) reappeared in the 2012_GM_SE leaderboard. Moreover, none of those 36 leaderboard members of 2010_GM_SE which dropped from the list in 2011 (including those 26 which failed to make a comeback in 2012) were actually dispelled from the community. The fact that they continued to occupy significant positions in the 2011 and 2012 GM_SEs was evident from their high read counts in these two metagenomes (see the numbers given in parenthesis in Fig. 5A).
2011_GM_SE had only 23 Proteobacteria among its top-50 genera. Concomitant to this proteobacterial retreat there were 36 new entries in the 2011 leaderboard, out of which, 21 remained predominant in 2012_GM_SE (names in red font in Fig. 5). Again, among the 36 new leaders of 2011 only eight were completely absent in the 2010_GM_SE metagenome (see names in Fig. 5B whose first number in parenthesis is zero). Again, all these eight newcomers maintained significant presence in 2012_GM_SE, with four of them even managing to retain their place in that leaderboard.
Proteobacterial resurgence was again conspicuous in 2012_GM_SE as 35 genera affiliated to the phylum hit the leaderboard. Concomitantly, all genera from Deinococcus-Thermus (three), Chloroflexi (two), Planctomycetes (one) and Firmicutes (one), which had made it to the top-50 in 2011_GM_SE, were relegated from the chart. Number of genera from Cyanobacteria and Bacteroidetes in the top-50 list also decreased in 2012_GM_SE. Additionally, there were six new leaderboard entrants in 2012_GM_SE, all of which except Opitutus were already there in the community since 2010 but gained preeminence only in 2012.
These numbers highlighted the resilience of the dominant components of the GM_SE, even as the community remained consistently receptive towards newcomers, which in their turn got stably incorporated into the guild. The last inference was evidenced by the fact that despite several transpositions in and out of the top-50 list over the three assessment years, not a single instance was apparent where an erstwhile leaderboard member went totally undetected in a subsequent GM_SE edition (follow the numbers in parentheses of Fig. 5).
Correlating populational and environmental fluctuations
It is presumable that in between 2010 and 2011 disappearance of the PT-top geyser and desiccation of the substratum ushered wide-ranging ecological limitations for the GMMC and eventually rendered irreparable damage to its habitat. In this scenario, even if a substantive fraction of the 2010 community managed to render dispersal to the southern slope, this calamity must have already impacted the community’s structure and function(s) significantly. In course of time, the distinct physicochemical conditions of the newfound habitat ought to have impacted the community further. However, it must be acknowledged that we lacked data on the environmental constraints, or for that matter, community alterations within the degenerating mats, around the time points when the west slope environment was actually drying up. As such, direct impact assessment of habitat degradation was not possible and environment-community correlations could only be based on comparative geochemistry and metagenomics of the spatiotemporally discrete hot water outflows and mat samples respectively. On top of that, comparative physicochemical information (see Table 1 or Fig. 2A) used in the correlation studies were averages of data collected at three discrete time points of only one particular day. Hence there was no data in hand to prove that the apparent year-on-year geochemical variations between the niches did not also occur on a more regular, say monthly or seasonal, basis.
The above caveat notwithstanding, it is noteworthy that nine out of the ten tested physicochemical parameters of the SE outflow showed identical patterns of oscillation over the three assessment years. Sulfate concentration was the only exception to the U-shaped curves observed for the nine other factors. Correspondingly, all the GM_SE phyla except Proteobacteria (particularly Gammaprotoebacteria) and Actinobacteria exhibited bell-shaped trends of population fluctuation over the three assessment years (see Fig. 2B & 3E). Temperature, pH, total dissolved solid (TDS) and concentrations of thiosulfate, sulfide, Fe2+ and Fe3+ iron, acetate and formate, all were at their relative highs in 2010. Next year all these values dipped sharply, only to increase again in 2012. While in 2012 most of these parameters were still below their 2010 levels, ferric iron recovered to its 2010 high while acetate went past that level. As such, the physicochemical milieu of 2011_GM_SE was quite different from that of 2010_GM_SE, while environmental parameters for 2012_GM_SE tended partly back towards the 2010 values. Here it may be recalled that a wide divergence between 2010_GM_SE and 2011_GM_SE and an intermediary status of 2012_GM_SE, was already evident from community structure comparisons. These prima facie impressions were quantitatively established when the environmental conditions experienced by the three GM_SE editions were statistically correlated with their community compositions. Bray-Curtis similarities and Euclidean distances between GM_SE sample pairs (Table S4) evidenced the wide divergence between 2010 and 2011 GM_SEs and the intermediary status of 2012_GM_SE, while Canonical Correspondence (CCA) (Fig. 6) and Principal Coordinate (PCoA) (Figure S2) analyses with phylum/class-level data graphically illustrated the same. CCA further revealed that the trifurcated relationship of the three GM_SEs stemmed mainly from the concentration of Betaproteobacteria in 2010_GM_SE and Deinococcus-Thermus and Chloroflexi in 2011_GM_SE, while there was no such skewed population in 2012_GM_SE. Besides such large-scale population growths, a few instances of modest but significant population expansion were also apparent, e.g. (i) Actinobacteria and Zetaproteobacteria in 2010_GM_SE, (ii) Acidobacteria, Deltaproteobacteria, Cyanobacteria and Planctomycetes in 2011_GM_SE and (iii) Verrucomicrobia and Bacteroidetes in 2012_GM_SE. Separation of the three GM_SE editions in CCA was further explained by the fact that some environmental factors were exceptionally high or low for certain particular samples. Such examples included (i) higher sulfide and Fe2+ in the 2010 outflow, (ii) lower pH and temperature alongside higher sulfate in 2011 and (iii) higher acetate in 2012.
As observable in Fig. 6, several cases of population fluctuation in the GM_SE were correlated to the oscillations of one or more environmental factors. In the following section we discuss only those cases which were further corroborated by strong Pearson correlation values, i.e. r numerically >0.8 alongside P < 0.05. Fluctuations in the abundance of Deltaproteobacteria, Acidobacteria and Gammaproteobacteria vis-à-vis sulfur species concentrations and pH were some of the most conspicuous correlations observed in these analyses. Decrease in the pH of the SE outflow in 2011 coincided with ~50% increase in sulfate concentration. These were accompanied by matching decreases in the flow rate and, sulfide and thiosulfate content of the fluid (Table 1). On the contrary, the 2012 pH upturn towards neutrality concurred with ~22% slump in sulfate content alongside relative hikes in flow rate, sulfide and thiosulfate content. However, none of these reversals were high enough to take the concerned parameters back to their 2010 levels. Within this gamut of fluctuations, increase in sulfate concentration of the 2011 SE outflow could have particularly ushered the five and a half fold increase in the relative abundance of Deltaproteobacteria in 2011_GM_SE (Fig. 3E), which in its turn was mainly attributable to rise in read counts of sulfate-reducing Desulfuromonadales and Desulfovibrionales members such as Geobacter, Pelobacter, Desulfovibrio, etc. The fact that deltaproteobacterial abundance in 2012_GM_SE, despite being halved from its 2011 level, still remained more than twice the level of 2010_GM_SE could be attributed to the moderately high sulfate concentration of 2012. It was further noteworthy that upturns in the abundance of sulfate-reducing bacteria coincided with the steep population growth of Cyanobacteria. This observation was in agreement with earlier reports of syntrophism between the two groups within microbial mats, where cyanobacterial excretory products (such as glycolate) are used by sulfate-reducing bacteria as electron sources9. The Acidobacteria population oscillated (Fig. 2B) in sync with Deltaproteobacteria (Fig. 3E), even as the former’s fluctuations were sharper. While both the groups showed strong positive and negative correlations with sulfate concentration and pH respectively, the small dip in the pH of the OFC could have driven the influx and/or proliferation of Acidobacteria in 2011_GM_SE. Acidobacteria can slow down metabolism and live long under low-nutrient conditions and substratum desiccation10. This together with their diverse mechanisms of respiration may have helped them overcome similar adversities between 2010 and 2011. The gammaproteobacterial population oscillated in a pattern opposite to that of Deltaproteobacteria and Acidobacteria, thereby showing strong positive and negative correlations with thiosulfate and sulfate respectively. These data were consistent with the fact that decrease in the overall population of Gammaproteobacteria in 2011_GM_SE involved sharp decrease in lithotrophic sulfur-oxidizing bacteria (SOB) like Thioalkalivibrio, Acidithiobacillus, Allochromatium and Halothiobacillus. Actinobacteria was the only phylum other than Proteobacteria that showed U-shaped oscillation over the years. Its abundance correlated positively with Fe2+, which was remarkable since iron oxidation is reportedly not widespread in Actinobacteria and that too mostly confined to Acidimicrobidae11, a subclass absent from the Actinobacteridae-dominated PT GM_SE.
Other significant canonical correspondences and linear correlations observed in the GM_SE community dynamics included (i) Cyanobacteria versus pH, TDS and formate (r = −0.998 for all three); (ii) Firmicutes versus sulfide and ferrous (r = −0.999 and r = −0.998 respectively); (iii) Nitrospirae versus pH, TDS and formate (r = −1.000 for all); and (iv) Planctomycetes versus pH, TDS and formate (r = −1.000 for all); (v) Deinococcus-Thermus versus temperature and ferric iron (r = −0.997 for both); and (vi) Chlorobi versus sulfide (r = −1.000). Negative correlations between Deinococcus-Thermus and temperature and Chlorobi and sulfide, appeared strange. However, subsequent 16S rDNA sequence-based diversity estimation of the GM_SEs versus the GM_PCs (Fig. 7) showed that the growth of Deinococcus-Thermus in 2011_GM_SE could be due to their dispersal from the 2010_GM_PC. Again relative abundance of Chlorobi or green sulfur bacteria (GSB) was lowest in 2010_GM_SE (Fig. 2B) when sulfide concentration in the OFC was at its highest (Fig. 2A). Unusually again, the GSB population increased to its highest level in 2011_GM_SE when sulfide was at its lowest. This could be explained by fact that Chromatiaceae and Ectothiorhodospirilaceae, or the purple sulfur bacteria (PSB), accounted for >10 times, 1.25 times and 1.4 times more reads than Chlorobi in the metagenomes of 2010, 2011 and 2012 GM_SE respectively. Now, despite their common requirement for sulfide, the PSB are nutritionally more versatile than the GSB by virtue of their ability to utilize organic compounds and also grow chemotrophically on thiosulfate in the dark by reducing oxygen12. So in 2010_GM_SE, the PSB might had outnumbered the fastidious GSB by making full use of thiosulfate (that was also abundant that year) and then by virtue of their numbers usurped the available sulfide also. However, with thiosulfate going down next year, the PSB potentially lost this advantage, thereby allowing the GSB to avail whatever sulfide was available in the 2011 discharge and grow from ~0.1% of all bacteria in 2010_GM_SE to ~0.5% in 2011_GM_SE.
Constancy and variability of metabolic types in the GM_SE metagenomes
Detection of photosynthetic genes in all GM_SE metagenomes concurred with their hyaline to deep green appearance. As such, the detectable repertoire of genes involved in electron transport and photophosphorylation and chlorosome and phycobilisome light-harvesting complexes was higher in 2011 and 2012 GM_SEs than in 2010_GM_SE. Notably again, photosynthetic genes detected in 2010_GM_SE were mostly proteobacterial in origin, while those of the next two editions were mainly from Cyanobacteria.
Invariable presence of multiple homologs of all the sox (sulfur oxidation) structural genes of chemo- as well as photo-lithotrophic bacteria in all the three GM_SE metagenomes indicated that reduced sulfur species, which were by and large abundant in this spring system, could be a key source of energy and/or electron for the community. Molecular hydrogen could also be an important source of energy and/or electron for the autotrophic as well as mixotrophic members of the GM_SE. This was suggested not only by the detection of energy-generating NAD+ -reducing [NiFe] hydrogenases in all three GM_SE metagenomes but also by the occurrence of the hydrogen-oxidizing “Knallgas” bacterium Ralstonia in all the three lists of top-50 genera (Fig. 5). Other such organisms as Rhodococcus, Azotobacter, Chloroflexus etc., which too can utilize H2 as a source of energy and/or electron via the oxyhydrogen “Knallgas” reaction 2H2 + O2 → 2H2O13,14 were also significantly represented in all these metagenomes. Consistent presence of facultatively hydrogen-oxidizing chemolithoautotrophic diazotrophs like Bradyrhizobium and phototrophs like Rhodobacter and Rhodopseudomonas14, in significant proportions further underscored the potential importance of hydrogen as an energy source of the community. Besides sulfur- or hydrogen-based lithotrophy, anaerobic carbon monoxide (CO) oxidation could also be another important source of energy and electron for the GM_SE. This was evidenced by the constant predominance of the anoxygenic phototroph Rhodospirillum [which can grow anaerobically in the dark on CO as the sole source of energy14] and the presence of several homologs of CO dehydrogenase (CODH) and CO-insensitive [NiFe] hydrogenases in all GM_SE metagenomes. Notably, other carboxydotrophs like Streptomyces15,16, Carboxydothermus and Oligotropha14 also accounted for significant fractions of metagenomic reads in all GM_SE editions.
Hydrothermal supply of iron (particularly Fe2+) could be another key determinant of the GM_SE community structure. While an apparent parallelism existed between Fe2+ concentration in OFCs (Table 1, Fig. 2A) and the iron richness of the GM_SE substrata (Figure S3), fluctuations of these two factors correlated well with the oscillation of iron-oxidizing bacteria (IOB) within the community (see lower panel of Figure S3). In 2010 the hydrothermal discharge and the deposited sinters were remarkably rich in Fe2+ and Fe3+ respectively (Table 1). Correspondingly, there were at least eight lithotrophic or organotrophic IOB (viz. Pseudomonas, Rhodobacter, Thiobacillus, Leptothrix, Sideroxydans, Rhodopseudomonas, Gallionella and Marinobacter)17 in the list of top-50 genera of 2010_GM_SE. Out of these eight genera three were also present in the corresponding list of 2011_GM_SE, while four made the cut in 2012_GM_SE (Fig. 5). IOB, as such, accounted for >10% of all bacterial metagenomic reads of 2010_GM_SE, while their read share was ~3% in the next two GM_SE editions. Drop in IOB abundance in the GM_SE clearly coincided with the sharp decline in Fe2+ availability in 2011, but, due to some unknown reason, their population did not recover appreciably in 2012 despite considerable increase in Fe2+ abundance in the discharge as well as the substratum.
Significant synchrony was also observed between the oscillation of the Shewanella population (Fig. 5) and that of iron, thiosulfate or TDS in the OFC (Fig. 2A), or for that matter, iron in the substratum (Figure S3). Under oxygen-stressed conditions Shewanella respire by reducing diverse oxidized metals and other substrates like fumarate, nitrate, trimethylamine N-oxide, dimethyl sulfoxide, sulfite, thiosulfate and elemental sulfur18. As such, this facultatively aerobic alphaproteobacterium, or its close phylogenomic relatives, could complement the biogeochemical roles of IOB and SOB and help complete the iron and sulfur cycles in the PT slope environment. They could also play central role in the biomineralization process in the slope microfacies by reducing dissolved metal ions from the hydrothermal fluid to their insoluble sulfide or oxide forms.
So far as carbon sources were concerned, all three GM_SE metagenomes encompassed large number of CO2 fixation-related genes such as those involved in carboxysome, CO2 uptake, Calvin-Benson cycle and photorespiration/oxidative C2 cycle. Potentials for autotrophic acetogenesis via the acetyl-CoA “Wood-Ljungdahl” pathway19 were noticeable in the GM_SE throughout the assessment period. However, standard acetogens like Clostridium, Moorella, Eubacterium and Thermoanaerobacter were present in significant proportions only in the 2011 and 2012 editions of the GM_SE, but not in 2010_GM_SE. As such, these four genera together accounted for 0.01%, 0.34% and 0.27% of all taxonomically classifiable reads of the 2010, 2011 and 2012 GM_SE metagenomes respectively. Nonetheless, genes for some of the key enzymes of the bacterial acetyl-CoA pathway, viz. (i) formate dehydrogenase, (ii) methenyltetrahydrofolate cyclohydrolase and methylenetetrahydrofolate dehydrogenase complex and (iii) methylenetetrahydrofolate reductase were present in all GM_SE metagenomes, including the 2010 edition. This observation illustrated that in 2010 cryptic potentials for acetogenesis could have well been dispersed up to the SE community, even as the main hub of acetogens lied somewhere up in the reductive gradient closer to the venting point. On the other hand, although both 2011 and 2012 GM_SE had equally increased abundance of acetogenic genera, genes for the three sub-units of key acetogenesis enzyme acetyl CoA synthase19, viz. (a) acetyl-CoA synthase corrinoid iron-sulfur protein; (b) CO dehydrogenase/acetyl-CoA synthase, CO dehydrogenase subunit; and (c) CO dehydrogenase/acetyl-CoA synthase, acetyl-CoA synthase subunit, appeared only in the 2012_GM_SE metagenome, plausibly due to sheer stochasticity. Anyway, these observations certainly implied that the altered SE conditions of 2011, which appreciably lingered until 2012, promoted the growth of acetogenic bacteria. Now this population growth could have been driven by elements that were already there in subdued abundance in 2010_GM_SE and/or those which migrated from more reduced and hotter niches of 2010.
Remarkably again, the apparent rise of acetogens in 2011 as well as their significant retention through 2012 coincided with identical population dynamics of methanogens and sulfate-reducing bacteria, which like the acetogens also employ the Acetyl-CoA pathway either in the direction of acetate/biomass synthesis or that of acetate degradation19. In this connection it is noteworthy that the summation of potential methanogens, acetogens and sulfidogens (sulfate-reducers) did not account for more than 5% of total metagenomic reads in any GM_SE sample, but their steep rise between 2010 and 2011 (followed by strong retention through 2012) was relatively significant. For example, the representation of methanogens went up from <0.01% of all classifiable reads in 2010_GM_SE to 0.21% in 2011_GM_SE and 0.14% in 2012_GM_SE, corresponding to which 6, 10 and 16 different methanogenesis-associated genes were identified in the respective metagenomes (Table S5). Similarly, proportion of potential sulfidogens (which included probable members from Deltaproteobacteria, Firmicutes and Nitrospirae) increased from 1.25% of all reads in 2010_GM_SE to almost 4.0% in 2011 and 3.3% in 2012. As envisaged for the acetogens, the observed upturn of methanogenic and sulfidogenic populations could have also been driven by elements already present in 2010_GM_SE (albeit, as minuscule minorities) and/or by immigrants from more reduced and hotter niches of 2010 (as apparent from subsequent analyses). However, simultaneous rise of these three biotypes in the same SE niche was bioenergetically intriguing since all the three metabolisms are hydrogen-requiring processes and the populations in question ought to compete with each other for hydrogen. Sulfate-reducing bacteria are known to utilize H2 at concentrations lower than that required by methanogens and their ability to outcompete the methanogens plausibly arise from the more-positive reduction potential of SO42− than that of CO220. From this point of view, the spike in methanogenic archaea in 2011_GM_SE was all the more intriguing because it happened when sulfate and sulfide contents of the SE outflow were at their three-year highest and lowest levels respectively. In other oxygen-stressed environments with sufficient quantities of SO4, H2S is reportedly the predominant reduced product and the major fate of biodegradable organic carbon is oxidation to CO2 (formed from the CH3 group of acetate)20. Conversely, CH4 replaces H2S as the main reduced product typically when SO4 is limiting (as organic carbon is disproportionated to CO2 and CH4 via H2- or formate-using aceticlastic reactions, which form CH4 from the CH3 of acetate)20. As such, the unusual expansion of the GM_SE methanogenic population amidst copious sulfate availability could have been rendered feasible by metabolisms based on methylated substrates like methylamines, which are monopolistic substrates rapidly fermentable (to CH4, CO2 and NH3) by methanogens. So far as the supply of trimethylamine is concerned, it can form from betaine glycine or other related osmoprotectants20, which in their turn are likely to be produced profusely by geothermal bacteria to balance the osmolarity of their cytoplasm with that of the thermal fluid21,22. Predominance of Methanosarcinaceae among the GM_SE methanogens in tandem with the steady detection of methylamine fermentation genes (monomethylamine permease and trimethylamine:corrinoid and methanol:corrinoid methyltransferases) insinuated the prevalence of methylotrophic methanogenesis in the community. Nevertheless, since the observed oscillation trend of acetate in the thermal discharge was opposite to that of acetogenic/methanogenic populations in the GM_SE it was quite likely that aceticlastic reactions were also rendered significantly. All these circumstantial evidences collectively hinted that H2 was a limiting factor for the community, which again could plausibly be compensated by the formate (an equally efficient reductant for methanogens) available in the system (Table 1). Anyway, even if the methanogens were out of the race for H2, the number of potential H2-utilizing processes and the count of corresponding bacteria were still significantly high in the GM_SE. As such, the community ought to have ensured sufficient and steady supply of H2, either from the native H2-generating bacteria and/or by inorganic reaction between Fe2+ and water.
So far as biotic H2 contribution is concerned, phototrophic Proteobacteria like Rhodobacter and Rhodospirillum, perpetually predominant in the GM_SE, could transform carbon substrates like lactate, acetate, butyrate, malate, etc. (using dinitrogen, glutamate or aspartate as nitrogen source) to CO2 and H2, which in their turn could also be reused for photoautotrophic growth23. Fermentation of organic matter could be another major energy-yielding as well as H2-forming process in the community. Constant occurrence of several genes for [NiFe] hydrogenases and formate hydrogenlyase indicated that mixed-acid fermentations could be in vogue in the GM_SE. Cyanobacteria like Cyanothece and Microcoleus and anoxygenic phototrophs like Rhodospirillum, Rhodobacter and Rhodopseudomonas (which ferment endogenous reserves in the dark to produce H2 as one of the fermentation products) could significantly contribute to H2 production via this route. Chemotrophic CO oxidation by anaerobic anoxygenic phototrophs like Rhodospirillum could be another viable source of molecular hydrogen in the GM_SE. Detection of CODH and CO-insensitive [NiFe] hydrogenase (which together catalyze the net reaction CO + H2O → CO2 + H2) in all three metagenomes spoke volubly in favor of this process. H2 could also be produced substantively as a byproduct of nitrogenase-mediated N2 fixation without involving a hydrogenase14. This was insinuated not only by the abundant dinitrogen-fixing rhizobia but also the various nitrogen-fixation genes detected in all three GM_SE metagenomes. Last but not the least; metagenomic data also suggested that alkaline phosphatase-mediated phosphite oxidation (H3PO3 + H2O → H3PO4 + H2) could also be a viable source of H2 in the GM_SE.
Besides a large number of heterotrophic bacteria capable of growing on complex sugars and amino acids, several methylotrophic and methanotrophic genera24 predominated the GM_SE consistently. Although the concentration of methylated compounds in the PT environment was not measured their importance as carbon source for the community was apparent from the occurrence of Methylibium, Methylobacillus, Methylobacterium, Methylotenera, Methylovorus and Methylococcus in the top-50 genera list of all three metagenomes (see Fig. 5 and Table S6). In addition, all the GM_SE metagenomes encompassed genes for at least one of the three subunits of methane monooxygenase, the key enzyme oxidizing the C-H bond of methane and other alkanes25.
Taxonomic diversity flux corroborated the fluctuations in ecological diversity
To get a precise picture of the taxonomic diversity (which only involves ‘what types’ and not ‘how many’) of the discrete GM_SE editions we estimated their species richness by analyzing amplified 16S rDNA fragments. V3 regions of all potential bacterial 16S rDNA present in a GM_SE metagenome was PCR-amplified using Bacteria–specific primers, but no amplicon could be obtained with Archaea–specific primers plausibly due to their extremely low abundance. The bacterial V3 amplicon pools were sequenced by Ion PGM up to such depths which ensured that plateaus of rarefaction curves were reached. Table S7 documents all data pertaining to the clustering of OTUs from the PGM reads.
The GM_SEs of 2010, 2011 and 2012 encompassed 1478, 1248 and 1220 OTUs respectively (Fig. 7). The species richness of 2010_GM_SE, though numerically highest among the three GM_SEs, was confined to only a few higher-level groups. In contrast, 2011_GM_SE was taxonomically most dispersed, followed by 2012_GM_SE. As such, the classifiable OTU diversity of 2010, 2011 and 2012 GM_SE was distributed over 9, 16 and 11 phyla respectively (Fig. 7, Table S8). Likewise, 12, 22 and 14 classes (Table S9) and 19, 52 and 27 genera (Table S10) were identifiable in 2010, 2011 and 2012 GM_SE in that order. These numbers were suggestive of an oscillation in the GM_SE taxonomic diversity in line with the trend observed for its ecological diversity. They further highlighted that higher OTU count did not necessarily mean greater taxonomic diversity if the spread of the OTUs over various higher-level taxa was included in the concept of diversity. However, since in the existing literature there is no mathematical scale to quantify the taxonomic spread of OTU sets we first had to formulate such an index and then use it to analyze potential swings in the GM_SE alpha diversity. It needs to be clarified at this juncture that this new Relative Taxonomic Diversity Index (Tr) only gives a comparative measure of the alpha diversities of closely related communities at a chosen hierarchic level (‘phylum’ in the present case) and is not an absolute measure of taxonomic diversity of a community. As such, it can only quantify the taxonomic diversity of a community relative to other spatially- or temporally-linked communities.
So far as calculating Tr was concerned, first, diversity pertaining to the ith phylum within a given GM_SE edition (pi) was estimated as a proportion of the cumulative diversity of that phylum encompassed by all three GM_SEs. Equation 1 gives the general expression for this ratio. Notably, the denominator (Ni) of the term pi represented the taxonomic scope of the ith phylum in the whole GM_SE system and was determined as follows: (i) First, the three multifasta files that respectively contained the consensus sequences of all the OTUs of the three GM_SE editions were merged into a single multifasta. (ii) Pair-wise alignment of all the sequences of this merged file was performed, followed by their tree-based clustering at 97% sequence similarity level. The new OTU superset thus formed gave the full scope of species diversity in the whole system. (iii) Finally, the consensus sequences in this OTU superset were classified via the RDP Classifier and those OTUs which were found to be affiliated to the ith phylum gave the taxonomic scope (Ni) of that phylum in the whole GM_SE system. After pi value was calculated for any phylum identified in a given OTU set it was multiplied by the square roots of their corresponding ni value to account for the actual species count for that phylum. The resulting products were then summed across phyla and the summation gave the final Tr value for the OTU set or GM_SE edition in question (equation 2).
All raw calculations involved in the current analysis are given in Table 2. As such, Tr value for 2011_GM_SE happened to be the highest, i.e. 54.3 out of a maximum possible 101.85, which was achievable only if a community edition by itself encompassed the whole diversity scope of the community system. 2012_GM_SE had the lowest Tr value (28.1), while 2010_GM_SE (39.51) enjoyed intermediate status. Thus, the year on year fluctuations in the Tr value of the GM_SE (Fig. 4D) almost mirrored the oscillations witnessed for the ecological diversity indices H and EH. The only distinction was that the Tr of 2012_GM_SE was less than that of 2010_GM_SE. Although the Tr values suggested an eventual loss of taxonomic diversity in the GM_SE, subsequent inclusion of the two GM_PC samples in a comprehensive OTU analysis of the entire PT GMMC revealed that a considerable portion of taxonomic diversity concentrated in 2011_GM_SE actually migrated to the PC niches in 2012 rather than being lost from the system.
Constancy, resilience and flux of bacterial groups in the entire GMMC
The above analyses comprehensively showed that a substantive fraction of GM_SE constituents were spatiotemporally constant while others were transitory in nature. However, the key questions that remained unresolved were the potential source(s) of so many newcomers into the GM_SE and the eventual fate of the incumbent populations that were apparently marginalized in course of community restructuring. Answers to these questions required a thorough idea about all plausible paths of dispersion and dispersal of populations as well as influx and efflux of bacteria within the entire GMMC continuum and not just the GM_SE alone. This could be achieved only via a holistic comparison of the taxonomic diversity of the all GM_SEs and GM_PCs encountered in the PT microbiome over the three assessment years. Thus, V3 regions of all bacterial 16S rDNAs present in the two GM_PC samples were PCR-amplified and sequenced by Ion PGM up to depths ensuring plateaus in the rarefaction curves. The resultant OTU sets were then compared with the existing GM_SE OTU sets to generate comprehensive pictures of phylum (Fig. 7) and genus (Fig. 8) level diversities of the three GMMCs as a whole. Figure 8 additionally retraced the putative paths via which genus-level entities could have transmitted from one PT niche to another. The quotient of all demographic interrelations between pertinent mat sample pairs was determined by identifying their shared and unique OTUs (Fig. 9A). This was done by first merging the consensus sequences of all the OTUs of the two samples in question and then doing tree-based clustering at 97% similarity level. The doubletons of the new consensus sequence superset represented the OTUs common to the two samples. Similarly, final quotient of year on year addition, deduction and transmission of OTUs at the level of the whole GMMC was also determined (Fig. 9B). First, following the above principles a consensus sequence superset was created for 2010 or 2012 by taking all OTUs from the GM_PC and GM_SE samples of that year. The resultant superset, representing the total diversity of the 2010 or 2012 GMMC, was then merged with the consensus sequence set of 2011_GM_SE and the clustering process repeated as above to get the common and unique OTUs between the GMMCs of 2010 and 2011, or 2011 and 2012 respectively.
Figure 8 revealed that a number of genera were dispersed throughout the GMMC continuum (see light green-highlighted names which are common to all PC or SE mat samples in question), while others were restricted to either PC or SE microenvironments (names highlighted in crimson, orange or light blue). While Fig. 8 identified only a few genera as common to all five mat samples, Fig. 9A indicated that the total count of such consistent broad niche-width OTUs could be quite high. Holistic comparison of the five OTU sets also offered a plausible reason for the sharp hike in the relative abundance of Deinococcus-Thermus, Chloroflexi, Verrucomicrobia, Acidobacteria or Firmicutes in the GM_SE edition of 2011 as against its 2010 counterpart. Since the 2010 PC niche was significantly rich in members of these phyla (see Fig. 7) it was natural to conjecture that between 2010 and 2011 spatiotemporal dispersal had occurred from the PC to the SE, thereby boosting the species richness and/or abundance of such bacteria in 2011_GM_SE. Fig 9A reinforced this notion by revealing that the total count of such niche-transcending OTUs (represented by the overlap between 2010_GM_PC and 2011_GM_SE) could be as high as 397, while the total number of native GM_SE OTUs conserved over 2010 to 2011 was 464. Concurrent to this, Fig. 8 identified seven such genera in 2011_GM_SE (names highlighted in deep blue) which were not present in the 2010_GM_SE but apparently migrated to the former from 2010_GM_PC. Subsequently, it was further interesting to detect all these seven genera in 2012_GM_PC while only two of them were archived in 2012_GM_SE. This gave the inkling that a sizeable fraction of the diversity accumulated in 2011_GM_SE from the previous year’s GM_PC actually migrated back to its original PC niche once that window of opportunity revived in 2012. The last notion was buttressed by the observation that in Fig. 9A, 562 out of the total 1248 OTUs of 2011_GM_SE overlapped with 2012_GM_PC, whereas only 438 OTUs of 2011_GM_SE overlapped with 2012_GM_SE. Corroboratively, the final quotient of diversity conservation in the PC niche over 2010–2012 was also as high as 515 (Fig. 9A).
Bacterial community structure of the mat-adjacent sediments was further studied to check whether the hypothesis of long-term survival and dispersal of the GMMC constituents was indeed true and the 2011 or 2012 mats were not constructed by similar founder bacteria from anywhere other than the GMMC. 2011_GM_SE-adjacent sediments were sampled thrice by scooping out 2.5 cm3 of freshly-precipitated mineral deposits in each round from three discrete points around and at least 10 cm beyond, the mat structure. The three sub-samples were mixed thoroughly and labeled as the 2011_sediment sample. In 2012, sediments around the GM_SE and GM_PC growths were sampled separately as above; subsequently the six sub-samples were mixed thoroughly and treated as the 2012_sediment sample. Total community DNA was extracted from these two composite sediment samples and V3 regions of all bacterial 16S rDNAs present therein PCR-amplified and sequenced by Ion PGM up to depths that yielded plateaus in rarefaction curves. Table S11 documents the numerical details pertaining to the clustering of OTUs from the PGM reads of the 2011 and 2012 sediment samples.
Taxonomic composition of the two sediment samples was quite similar to each other and at the same time clearly distinct from any of the five green mat samples. Bulk of their OTUs belonged to the phyla Actinobacteria and Firmicutes (Fig. 10), which, notably, had contributed very little to the alpha diversity of the GMMC samples (see Fig. 7). Most importantly, the 2011_sediment sample was found to include only one (viz. Limnobacter) out of the 20 genera hypothesized to have been handed over to 2011_GM_SE from 2010 GM_PC and/or GM_SE (compare the sedimentary genera listed in Table S12 with data shown in Fig. 8). Similarly, the 2012_sediment community included only four (viz. Limnobacter, Meiothermus, Brevundimonas and Chloroflexus) out of the 28 genera hypothesized to have been carried over to 2012 GM_PC and/or GM_SE from 2011_GM_SE (compare information given in Table S12 and Fig. 8). These observations, along with the fact that there was no microbial mat in the southern slope in 2010, reinforced the hypothesis that long-term survival and dispersal of 2010 GMMC constituents and not the founder effect of similar bacteria from other mat-adjacent niches, created the framework of the 2011 and 2012 mats.
Figure 9A showed 679 OTUs to be common between 2010 and 2012 GM_SEs, thereby insinuating extensive species conservation within the GM_SE itself. Intriguingly, this number was much higher than the number of OTUs common between 2010 and 2011 GM_SE (464), or 2011 and 2012 GM_SE (438). These numbers were indicative of a scenario where several species native to the SE niche were pushed below detectable levels in 2011_GM_SE as this minimally-dispersed community was overcrowded by the influx of immigrants from discrete ecological niches, potentially extending beyond the GMMC framework. Then in 2012, when a large number of species apparently vacated the GM_SE space and migrated back to the revived PC niche, some of the GM_SE components marginalized in 2011 restored their populations above detectable limits. Similar results were also observed for the two GM_PCs, where the number of 2010 OTUs recovered from the 2012 edition was higher than the number of 2010_GM_PC OTUs which could have been transmitted via 2011_GM_SE. As such, in Fig. 9A, 515 OTUs were common to the 2010 and 2012 GM_PCs, while only 397 were common to 2010_GM_PC and 2011_GM_SE. These observations were further mirrored in Fig. 8 where some of the 2010_GM_PC and 2010_GM_SE genera that had gone undetected in 2011_GM_SE resurfaced in the 2012 GM_PC and/or GM_SE samples (see the hypothetical migration paths in dotted lines in Fig. 8). This suggested that within 2011_GM_SE, members coming from both 2010_GM_SE and 2010_GM_PC were equally starved for space and pushed below detectable levels.
The crux of the above analyses showed that a considerable portion of the 2011_GM_SE diversity was actually derived from 2010_GM_PC. At the same time, the apparent decline in the taxonomic diversity of the SE green mats in 2012 (or for that matter decline in the relative abundance of Chloroflexi, Deinococcus-Thermus and Acidobacteria in 2012_GM_SE) could be attributable to the partitioning of a substantial portion of 2011_GM_SE diversity into two discrete meta-communities. Since 2012_GM_PC was significantly richer than 2011_GM_SE in terms of the species diversity of Chloroflexi, Deinococcus-Thermus or Acidobacteria (see Fig. 7) it was natural to presume that between 2011 and 2012 bulk of these bacteria relocated to their preferred PC niches. In a nutshell, potential species loss notwithstanding, the overall diversity of the PT GMMC, over the three years, actually augmented from the 2010 level. The final quotient of the entire diversity dynamics of the PT GMMC is summarized below.
In 2010, the GMMC harbored a sum total of 2078 OTUs, while in 2012 the number went up to 2636 (Fig. 9B). These numbers, in conjunction with the data presented in Fig. 7, indicated a net increase in the alpha diversity of the GMMC, both in terms of OTU count and taxonomic spread of OTUs. Notably, the number of OTUs (618) common between 2010 and 2012 GMMC exceeded the overlaps between the GMMCs of 2010 and 2011 (409 OTUs) as well as 2011 and 2012 (451 OTUs). On the other hand, when the entire OTU set of the 2010 GMMC was compared with that of 2011_GM_SE, 1669 OTUs were unique to the former and only 839 were exclusive to the latter. The 839 OTUs detected exclusively in the 2011_GM_SE were most likely to represent foreign recruits that were not present in the PT GMMC earlier. While some idea about the generic identity of these OTUs can be made from the 32 names highlighted in yellow in Fig. 8, it is not impossible that some of these 839 were also present in the GMMC in 2010 but were overwhelmed by the preponderant Proteobacteria. Conversely, there were several pointers demonstrating that a substantive fraction of the 1669 OTUs found to be unique to the 2010 GMMC (versus 2011_GM_SE) were not totally lost from the 2011 community but marginalized below detection limits.
Remarkably again, in Fig. 9B, the number of OTUs common to 2011_GM_SE and the whole GMMC of 2012 (451) was higher than the overlap between 2010 GMMC and 2011_GM_SE (409 OTUs). This implied that many new recruits of 2011 were retained in the GMMC through 2012, a fact that concurred with the genus-level comparisons (note that in Fig. 8, 11 out of the 32 unique genera of 2011_GM_SE were also detected in 2012 GM_PC and/or GM_SE). Comparison between 2011_GM_SE and the 2012 GMMC further showed that 797 OTUs may have been lost in transition from 2011 to 2012, while 2185 OTUs apparently joined the GMMC during that period (idea about the generic identity of these OTUs can be made from the names highlighted by bright green, white and purple in Fig. 8). However, the net influx between 2010 - 2012 could have actually been lower than 2185, since this number also included those 2010 OTUs which were marginalized in 2011 (note that in Fig. 9B only 2018 OTUs were unique to the 2012 GMMC in comparison to 2010 GMMC). Most importantly, net diversity addition in the GMMC over three assessment years was surely higher than the net loss represented by the 1460 OTUs unique to the 2010 GMMC in comparison to the 2012 GMMC.
GMMCs have been explored extensively from diverse high temperature habitats using multiple methodologies26,27,28,29,30. However, this study is distinctive in using large volume of metagenomic sequence in combination with an equally substantive amount of 16S rDNA sequence to unearth microbial diversity associated with a relatively uncommon type of circum-neutral hot spring system. Though globally infrequent, such hot springs, which are typically poor in TDS, silicate and chloride, but often rich in sodium/calcium and various compounds of sulfur, are common in the geothermal areas of North-Western Himalayas and Tibet8,31,32,33. But very few explorations have hitherto been conducted to characterize their microbiota34,35. However, the main importance of the present study was its elucidation of the survival dynamics of a GMMC in the face of drastic environmental changes. In conclusion, that survival story can be summed up as follows.
In 2010 a graded continuum of intricate ecological conditions existed along large swathes of the western slope of the PT sinter accretion. This resulted in wide habitat heterogeneity within the ecocline comprised of several gradients of opportunity (mainly in the form of various nutrients dissolved in the hot water outflow) as well as resistance (mainly in the form of thermal stress). While some of the opportunity gradients lay parallel to the gradient of environmental resistance, others were aligned antiparallel to the latter. Since almost none of the GMMC constituents were hyperthermophilic, the temperature gradient, running from the proximal channels to the slope environment, acted as a potential gradient of environmental resistance for nearly all the members of the community. In this scenario, ecological growth of the GMMC in time and space was mainly driven by the dispersion of populations, which in turn depended on the innate ability (resilience) of the species to cope with the environmental resistance. Eventually, on the multivariate ecological continuum (or the ecocline) the diverse biotypes (taxonomic and/or metabolic types) potentially consolidated their positions at their respective optimum niches, while their populations tapered off gradually on either side of the consolidation zones.
Then between November 2010 and 2011 the large geyser atop the PT got extinguished, thereby causing the hot water flow on western slope of the mound to dry up completely. Even as substratum desiccation turned the existing habitat of the GMMC hostile, during the same period a slender prospect of survival (habitable space) opened up in the form of two new vents in the southern slope of the PT. Amidst this spatial drift, as well as shrinkage, of habitable space (defined by the shorter length and breadth of the new OFC) dispersal emerged as the main driver of ecological sustenance of the community. While some incumbent populations of the sprawling 2010 GMMC compromised their niche specialization (e.g. Deinococcus-Thermus) others gave up their dispersion (e.g. Proteobacteria) to launch spatiotemporal dispersal and build a minimally-dispersed seed-like community (viz. the 2011_GM_SE) on the southern-slope OFC. The apparent aim of the whole process was to conserve maximum-possible phylogenomic diversity from both ends of the 2010 GMMC continuum. However, in course of this en masse dispersal several incumbent populations of the 2010 GMMC got eliminated or acutely marginalized, even as many of them managed to maintain significant representation in the GM_SE construct of 2011. Besides embracing internally-displaced populations from the 2010 GMMC, 2011_GM_SE showed exceptional receptivity in countenancing external immigrants. This openness potentially enhanced the ecological fitness (survival value) of the community by inducting new metabolic pathways and/or variants of existing ones. Presumably, 2011_GM_SE must have positioned itself at such an optimum point on the new ecocline that allowed its diverse constituents to make best use of all available environmental opportunities and overcome existing resistances. Growth (dispersive scope) of 2011_GM_SE, however, was constrained by additional environmental resistances such as limited habitable space and scarce nutrients due to diminutive volume, flow rate and chemical-content of the hydrothermal discharge. Presumably in order to sustain the equilibrium of its existence this recuperating GMMC limited its dispersion to a restricted zone of the already short ecological continuum and therefrom started developing resilience adequate enough to encounter the existing resistances and prepare for future growth.
Finally in 2012, geothermal activity in the southern-slope of the PT gained impetus (in the form of new vents and increased flow rates and mineral contents of discharges), thereby widening the available ecological niches. The eco-physiologically miscellaneous components of 2011_GM_SE took this opportunity to split into discrete GM_PC and GM_SE metacommunities. As many expatriated 2010_GM_PC populations vacated the SE refuge, community growth space in the SE niche increased further. Thus, many GM_SE natives (e.g. many Proteobacteria) who were reduced to minuscule minorities in 2011_GM_SE regained preeminence in 2012_GM_SE. However, the second round of population dispersal was more complex than the 2010–2011 transition since many more new species joined the GMMC, especially through the revived GM_PC window. In this way the GMMC seeds were again successfully sown at either end of the thermo-nutritional gradient. Whether this niche-partitioned GMMC can regain dispersive growth and regenerate an expansive continuum depend on the vitality of the spring system.
Sampling and in situ analyses
Samples were collected in sterile polypropylene bottles and transported immediately to the laboratory in insulated 4 °C coolers. At all the five data points sampling was done thrice by scraping off 2.5 cm2 of mat material in each round from three horizontally discrete points (5 to 10 cm apart) equidistant from the water source and having identical temperature and pH. Utmost care was taken to ensure that the green mat structures were exclusively scraped off from the surface with minimum infiltration of underlying sediments. Immediately upon reaching the laboratory, all sub-samples of a given mat sample were mixed thoroughly by rehydrating with sterile 0.9% NaCl solution. Total community DNA (metagenome), in quantities sufficient for all downstream experiments, was extracted from these composite samples using PowerMax soil DNA isolation kit (MoBio).
S2O32− and SO42− concentrations in the thermal fluid were measured in situ by iodometric titration and gravimetric precipitation (as BaSO4) respectively36,37,38,39,40. S2− in the thermal waters was measured using the chemical principle that N, N-dimethyl-p-phenylene diamine dihydrochloride combines quantitatively with H2S in the presence of FeCl3 catalyst and HCl to give a blue colored complex. Fe3+ concentration in the waters was determined by thiocyanate colorimetry. Quantitative spectrophotometric determination of Fe2+ was done by reacting the same with o-phenanthroline in situ and eliminating the interference of Fe3+ by complexing it with sodium fluoride41. Details of analytical methods are provided as Supplementary Information.
Metagenomes were shotgun sequenced by the Ion Torrent Personal Genome Machine (Ion PGM) or the Ion Proton platform42 (Life Technologies) using 200 bp read chemistry on the Ion 318 or the PI V2 chip respectively (details in Supplementary Information). The metagenomic sequence sets were quality-filtered and clipped to eliminate low quality regions, using sff_extract. The sequence files were deposited to the NCBI Sequence Read Archive with the run accession numbers SRR1662204, SRR1662223 and SRR1662248 under the BioProject accession number PRJNA268268.
Read sets were annotated and analyzed using MG-RAST43 to gain quantitative insights into the community structures and functions. Within this analysis pipeline, sequences were trimmed so as to contain no more than five consecutive bases below the phred score of 15. Reads were taxonomically classified using the “Organism Abundance” tool of MG-RAST following either the “Best Hit Classification” (BHC) or the “Lowest Common Ancestor” (LCA) approach. For higher-level classifications (up to class) shotgun metagenomic read sets were searched by blastx against the non-redundant (nr) protein database following the BHC approach with minimum alignment length of 45 bp (15 amino acids) and minimum identity cutoff of 60%. Alternatively, to classify reads up to the genus level similar blastx searches were conducted using the LCA algorithm with minimum alignment length of 30 amino acids and minimum identity cutoff of 70%. Each read set was also searched for small subunit (ssu) rRNA genes against the RDP database using blastn with minimum alignment length of 50 bp and 70% minimum identity cutoff. Sequences were potentially assigned to genera only when they shared >95% rRNA sequence identity with known species. Maximum e-value cutoff used in all these analyses was 1e-5.
Presence of only those genera which accounted for ≥0.01% of all classifiable metagenomic reads was considered to be significant within any given community. This convention led to the short-listing of around 300 (out of a total 600), 500 (out of a total 1700) and 400 (out of a total 1900) genus-level entities from the ‘organism abundance’ list of the 2010, 2011 and 2012 GM_SE metagenomes respectively. Genera falling below this cutoff were thought to be present in the community in very low proportions and thus kept out of all ecological interpretations.
Ecological diversity was quantified from shotgun metagenomic data by rendering the phylum-level distribution of reads (a measure of relative abundance of phyla) to Simpson Dominance and, Shannon–Wiener Diversity and Evenness indices44 (detailed formulae are given in Supplementary Information).
Several correlation and ordination methods were used to identify potential bacterial groups that had added importance in the present GMMC dynamics. Pearson (linear) correlations between phyla/class-level metagenomic data and physicochemical properties of the hydrothermal fluid were calculated by XLSTAT (http://www.xlstat.com/en/download.html). PCoA and CCA were carried out in STATISTICA 10.0 for Windows (http://statistica.software.informer.com/10.0/) and validated using PAST 3.0245. PAST was also used to determine Euclidean distance and Bray-Curtis similarity between the GM_SE samples.
Species richness estimation (OTU clustering)
Amplification of V3 regions of 16S rRNA genes and sequencing of amplicon pools by Ion PGM were carried out using fusion primers46 (details in Supplementary Information). The sequence files for the GMMC samples were deposited to the NCBI Sequence Read Archive (SRA) with the run accession numbers SRR1663456, SRR1663458, SRR1663464, SRR1663465 and SRR1663466 under the BioProject accession number PRJNA268268. The sequence files for the two mat-adjacent sediment samples were deposited to the SRA with the run accession numbers SRR1800757 and SRR1802680 under the BioProject accession number PRJNA268268.
Raw V3 region-specific reads were first filtered for high quality value (QV 20) and length threshold of 100 bp46. Selected reads were then converted to fasta from fastq using Fastx_toolkit (v0.0.13.2). Subsequent preprocessing using the “preproc” module of ESPRIT47 involved screening of only those reads which had intact 16S rDNA universal primer sequence plus the barcode adaptor and the barcode. Adaptor sequences were then trimmed; reads containing unidentified bases (N) filtered out together with those which were identical to another read or were mere subsets of a longer read. After preprocessing, denoising of reads was achieved as follows: (i) pairwise alignment of reads by Needleman algorithm was carried out using the module “pairwise.seqs” from MOTHUR48; (ii) the alignment matrix thus created was utilized for Single Linkage Preclustering49 using a script50 provided by the VAMPS (Visualization and Analysis of Microbial Population Structure project) integrated collection of tools located at http://vamps.mbl.edu/overview.php. Pairwise distance of 0.02 (98% identity) was used as threshold criterion for selecting reads in preclustering, which were then stored in fasta format.
Reads were clustered by hierarchical clustering technique using various modules available within ESPRIT47. In brief, reads were again aligned pairwise following Needleman algorithm; clusters or operational taxonomic units (OTUs) were created with pairwise distance of 0.03 (97% identity) as the criterion; and eventually the total number of OTUs identified in a community gave the estimate of its species richness. The clusters or OTUs thus formed were also used to draw statistical inferences. OTUs were filtered using a Perl script to remove all the singletons. Singletons were removed from *.Cluster as well as *.Cluster_List to make new_Cluster & new_Cluster_List files. The new Cluster files were run in the statistical module of ESPRIT to get ACE and Rarefaction analyses. Rarefaction data were further utilized in R package51 to create graphs for reads taking part in OTU formation versus number of OTUs formed. Consensus sequences were created using the clusters (minus singletons) and the fasta and frequency files created during the clustering operations. All consensus sequences generated for a given dataset were taxonomically classified with the help of the “RDP Classifier” located at http://rdp.cme.msu.edu/classifier/classifier.jsp.
How to cite this article: Ghosh, W. et al. Resilience and receptivity worked in tandem to sustain a geothermal mat community amidst erratic environmental conditions. Sci. Rep. 5, 12179; doi: 10.1038/srep12179 (2015).
Wèachtershèauser, G. in Origin of life in an iron-sulfur world, 206–218 (Cambridge University Press, Cambridge; New York, 1998).
Martin, W., Baross, J., Kelley, D. & Russell, M. J. Hydrothermal vents and the origin of life. Nat. Rev. Microbiol. 6, 805–814 (2008).
Martin, W. & Russell, M. J. On the origin of biochemistry at an alkaline hydrothermal vent. Phil. Trans. R. Soc. B. 362, 1887–1925 (2007).
Farmer, J. D. Hydrothermal Systems: Doorways to Early Biosphere Evolution. GSA Today 10, 1–9 (2000).
Hessler, R. R. et al. Temporal change in megafauna at the Rose Garden hydrothermal vent (Galapagos Rift; eastern tropical Pacific). Deep Sea Research Part A. Oceanographic Research Papers. 35, 1681–1709 (1988).
Johnson, K. S., Childress, J. J., Hessler, R. R., Sakamoto-Arnold, C. M. & Beehler, C. L. Chemical and biological interactions in the Rose Garden hydrothermal vent field, Galapagos spreading center. Deep Sea Research Part A. Oceanographic Research Papers 35, 1723–1744 (1988).
Shank, T. M. et al. Time-Series Exploration and Biological, Geological and Geochemical Characterization of the Rosebud and Calyfield Hydrothermal Vent Fields at 86°W and 89.5°W on the Galapagos Rift in Eos Trans. American Geophysical Union, 83(47), Fall Meet. Suppl., Abstract T11C-1257. San Francisco, CA: AGU. (2002, December 6-10).
Rai, A. P. Compilation of data on chemical analysis of water and gas samples from North West Himalaya and adjoining areas, (Geological Survey of India, Kolkata, 2001).
Overmann, J. & Garcia-pichel, F. The Phototrophic Way of Life in The Prokaryotes. Vol. 2 (eds Dworkin, M. et al. ). 32–85 (Springer, New York, 2006).
Ward, N. L. et al. Three genomes from the phylum Acidobacteria provide insight into the lifestyles of these microorganisms in soils. Appl. Environ. Microbiol. 75, 2046–56 (2009).
Johnson, D. B., Bacelar-Nicolau, P., Okibe, N., Thomas, A. & Hallberg, K. B. Ferrimicrobium acidiphilum gen. nov., sp. nov. and Ferrithrix thermotolerans gen. nov., sp. nov.: heterotrophic, iron-oxidizing, extremely acidophilic actinobacteria. Int. J. Syst. Evol. Microbiol. 59, 1082–1089 (2009).
Ghosh, W. & Dam, B. Biochemistry and molecular biology of lithotrophic sulfur oxidation by taxonomically and ecologically diverse bacteria and archaea. FEMS Microbiol. Rev. 33, 999–1043 (2009).
Hanada, S . & Pierson, B. K. The Family Chloroflexaceae in The Prokaryotes, Vol. 7, (eds Dworkin, M. et al. ) 815–842 (Springer, New York, 2006).
Schwartz, E. & Friedrich, B. The H2-Metabolizing Prokaryotes in The Prokaryotes. Vol. 2, (eds Dworkin, M. et al.) 496–563 (Springer, New York, 2006).
Kim, S. B., Falconer, C., Williams, E. & Goodfellow, M. Streptomyces thermocarboxydovorans sp. nov. and Streptomyces thermocarboxydus sp. nov., two moderately thermophilic carboxydotrophic species from soil. Int. J. Syst. Bacteriol. 48, 59–68 (1998).
Kim, S. B. & Goodfellow, M. Streptomyces thermospinisporus sp. nov., a moderately thermophilic carboxydotrophic streptomycete isolated from soil. Int. J. Syst. Evol. Microbiol. 52, 1225–8 (2002).
Emerson, D., Fleming, E. J. & McBeth, J. M. Iron-oxidizing bacteria: an environmental and genomic perspective. Annu. Rev. Microbiol. 64, 561–583 (2010).
Heidelberg, J. F. et al. Genome sequence of the dissimilatory metal ion-reducing bacterium Shewanella oneidensis. Nat. Biotechnol. 20, 1118–1123 (2002).
Drake, H. L., Küsel, K. & Matthies, C. Acetogenic Prokaryotes in The Prokaryotes, Vol. 2, (eds Dworkin, M. et al. ) 354–420 (Springer, New York, 2006).
Whitman, W. B., Bowen, T. I. & Boone, D. R. The Methanogenic Bacteria in The Prokaryotes, Vol. 3, (eds Dworkin, M. et al. ) 165–207 (Springer, New York, 2006).
Holtmann, G. & Bremer, E. Thermoprotection of Bacillus subtilis by exogenously provided glycine betaine and structurally related compatible solutes: involvement of Opu transporters. J. Bacteriol. 186, 1683–93 (2004).
Nau-Wagner, G. et al. Genetic control of osmoadaptive glycine betaine synthesis in Bacillus subtilis through the choline-sensing and glycine betaine-responsive GbsR repressor. J. Bacteriol. 194, 2703–14 (2012).
Imhoff, J. F. The Phototrophic Alpha-Proteobacteria in The Prokaryotes. Vol. 5, (eds Dworkin, M. et al. ) 41–64 (Springer, New York, 2006).
Bowman, J. P. The Methanotrophs—The Families Methylococcaceae and Methylocystaceae in The Prokaryotes, Vol. 5, (eds Dworkin, M. et al. ) 266–289 (Springer, New York, 2006).
Lieberman, R. L. & Rosenzweig, A. C. Crystal structure of a membrane-bound metalloenzyme that catalyses the biological oxidation of methane. Nature 434, 177–182 (2005).
Yamamoto, H. et al. Phylogenetic Evidence for the Existence of Novel Thermophilic Bacteria in Hot Spring Sulfur-Turf Microbial Mats in Japan. Appl. Environ. Microbiol. 64, 1680–1687 (1998).
Takacs, C. D. et al. Phylogenetic characterization of the blue filamentous bacterial community from an Icelandic geothermal spring. FEMS Microbiol. Ecol. 35, 123–128 (2001).
Hiraishi, A., Umezawa, T., Yamamoto, H., Kato, K. & Maki, Y. Changes in Quinone Profiles of Hot Spring Microbial Mats with a Thermal Gradient. Appl. Environ. Microbiol. 65, 198–205 (1999).
Reysenbach, A. L., Wickham, G. S. & Pace, N. R. Phylogenetic analysis of the hyperthermophilic pink filament community in Octopus Spring, Yellowstone National Park. Appl. Environ. Microbiol. 60, 2113–9 (1994).
Skirnisdottir, S. et al. Influence of sulfide and temperature on species composition and community structure of hot spring microbial mats. Appl. Environ. Microbiol. 66, 2835–41 (2000).
Ghosh, W. et al. Molecular and Cellular Fossils of a Mat-Like Microbial Community in Geothermal Boratic Sinters. Geomicrobiology Journal 29, 879–885 (2012).
Shanker, R. et al. Geothermal Atlas of India 144 (Geological Survey of India, Kolkata, 1991).
Thussu, J. L. Geotherman Evergy Resources of Indian. (Geological Survey of India, Kolkata, 2002).
Huang, Q. et al. Archaeal and bacterial diversity in hot springs on the Tibetan Plateau, China. Extremophiles 15, 549–63 (2011).
Song, Z.Q. et al. Bacterial and archaeal diversities in Yunnan and Tibetan hot springs, China. Environ. Microbiol. 15, 1160–75 (2013).
Mazumdar, A. & Strauss, H. Sulfur and strontium isotopic compositions of carbonate and evaporite rocks from the late Neoproterozoic-early Cambrian Bilara Group (Nagaur-Ganganagar Basin, India): Constraints on intrabasinal correlation and global sulfur cycle. Precambrian Research 149, 217–230 (2006).
Dam, B., Mandal, S., Ghosh, W., Das Gupta, S. K. & Roy, P. The S4-intermediate pathway for the oxidation of thiosulfate by the chemolithoautotroph Tetrathiobacter kashmirensis and inhibition of tetrathionate oxidation by sulfite. Res. Microbiol. 158, 330–8 (2007).
Ghosh, W., Bagchi, A., Mandal, S., Dam, B. & Roy, P. Tetrathiobacter kashmirensis gen. nov., sp. nov., a novel mesophilic, neutrophilic, tetrathionate-oxidizing, facultatively chemolithotrophic betaproteobacterium isolated from soil from a temperate orchard in Jammu and Kashmir, India. Int. J. Syst. Evol. Microbiol. 55, 1779–87 (2005).
Kelly, D. P. & Wood, A. P. Synthesis and Determination of Thiosulfate and Polythionates. Methods in Enzymology 243, 475–501 (1994).
Alam, M., Pyne, P., Mazumdar, A., Peketi, A. & Ghosh, W. Kinetic enrichment of 34S during proteobacterial thiosulfate oxidation and the conserved role of SoxB in S-S bond breaking. Appl. Environ. Microbiol. 79, 4455–64 (2013).
Herrera, L., Ruiz, P., Aguillon, J. C. & Fehrmann, A. A new spectrophotometric method for the determination of ferrous iron in the presence of ferric iron. Journal of Chemical Technology & Biotechnology 44, 171–181 (1989).
Rothberg, J. M. et al. An integrated semiconductor device enabling non-optical genome sequencing. Nature 475, 348–52 (2011).
Meyer, F. et al. The metagenomics RAST server - a public resource for the automatic phylogenetic and functional analysis of metagenomes. BMC Bioinformatics 9, 386 (2008).
Magurran, A. E. Measuring Biological Diversity, (Blackwell Publishing Limited, Oxford, UK, 2003).
Hammer, Ø., Harper, D. A. T. & Ryan, P. D. PAST: Paleontological statistics software package for education and data analysis. Palaeontologia Electronica 4, 9 (2011).
Yergeau, E. et al. Next-generation sequencing of microbial communities in the Athabasca River and its tributaries in relation to oil sands mining activities. Appl. Environ. Microbiol. 78, 7626–37 (2012).
Sun, Y. et al. ESPRIT: estimating species richness using large collections of 16S rRNA pyrosequences. Nucleic Acids Res. 37, e76 (2009).
Schloss, P. D. et al. Introducing mothur: open-source, platform-independent, community-supported software for describing and comparing microbial communities. Appl. Environ. Microbiol. 75, 7537–41 (2009).
Junemann, S. et al. Bacterial community shift in treated periodontitis patients revealed by ion torrent 16S rRNA gene amplicon sequencing. PLoS One 7, e41606 (2012).
Huse, S. M., Welch, D. M., Morrison, H. G. & Sogin, M. L. Ironing out the wrinkles in the rare biosphere through improved OTU clustering. Environ. Microbiol. 12, 1889–98 (2010).
Dixon, P. VEGAN, a package of R functions for community ecology. Journal of Vegetation Science 14, 927–930 (2003).
This work was financed by the Science & Engineering Research Board, Department of Science & Technology, Government of India (GOI). Rimi Roy and Prosenjit Pyne were endowed with fellowships by the CSIR, GOI. Chayan Roy and Moidu Jameela Rameez received fellowships from the UGC, GOI. We thank Prof. Ranadhir Chakraborty and Sri Saurav Sarkar for their thoughtful discussions.
The authors declare no competing financial interests.
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Ghosh, W., Roy, C., Roy, R. et al. Resilience and receptivity worked in tandem to sustain a geothermal mat community amidst erratic environmental conditions. Sci Rep 5, 12179 (2015). https://doi.org/10.1038/srep12179
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