Abstract
Mesophilic and thermophilic methanogens belonging to the hydrogenotrophic, methylotrophic, and acetotrophic groups were isolated from Indian hot spring environments using BY and BCYT growth media. Following initial Hinf I-based PCR–RFLP screening, 70 methanogens were sequenced to ascertain their identity. These methanogens were phylogenetically and physiologically diverse and represented different taxa distributed across three physiological groups, i.e., hydrogenotrophs (53), methylotrophs (14) and acetotrophs (3). Overall, methanogens representing three families, five genera, and ten species, including two putative novel species, were recognized. The highest number and diversity of methanogens was observed at 40 ℃, dominated by Methanobacterium (10; 3 species), Methanosarcina (9; 3 species), Methanothermobacter (7; 2 species), Methanomethylovorans (5; 1 species) and Methanoculleus (3; 1 species). Both putative novel methanogen species were isolated at 40 ℃ and belonged to the genera Methanosarcina and Methanobacterium. At 55 ℃, limited diversity was observed, and resulted in the isolation of only two genera of methanogens, i.e., Methanothermobacter (28; 2 species) and Methanosarcina (4; 1 species). At 70 ℃, only members of the genus Methanothermobacter (5; 2 species) were isolated, whereas no methanogen could be cultured at 85 ℃. Ours is the first study that documents the extensive range of cultivable methanogenic archaea inhabiting hot springs across various geothermal provinces of India.
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Introduction
Methane has been identified as one of the most important renewable biofuels and has multiple applications if produced and harvested in anaerobic digestion processes (Demirel and Scherer 2008; Pore et al. 2019). At the same time, methane is also a potent greenhouse gas (28 times CO2), contributing to global warming for over 100 years if released directly into the atmosphere (Pachauri et al. 2014). The beneficial and harmful nature of methane, therefore, necessitates the study of methanogens, which produce most of the biogenic methane (Thauer et al. 2008). Methanogens are a group of strict anaerobic archaea that play a key role in the carbon cycle by facilitating interspecies hydrogen transfer (Ishii et al. 2005; Pak and Bartha 1998). These organisms thrive in diverse habitats like oil wells, the gut of herbivores, hydrothermal vents, subsurface coal mines, rice fields, hot springs, etc. (Joshi et al. 2018; Kumar et al. 2018). Methanogens are currently documented under four phyla, namely, Euryarchaeota, Thermoproteota, Bathyarchaeota, and Verstraetearchaeota (Berghuis et al. 2019; Evans et al. 2015; Vanwonterghem et al. 2016; Zhou et al. 2018), although the cultured isolates till date are only from phylum Euroyarchaeota, Verstraetearchaeota and Thermoproteota (Cheng et al. 2023; Hatzenpichler 2023). Phylogenetically, methanogens are divided into five families, comprising 33 genera and 153 species and can survive over a broad temperature range of 0–110 ℃ and pH of 4.1–10 (Franzmann et al. 1997; Michał et al. 2018). For growth, methanogens require a redox potential lesser than − 200 mV and can be either autotrophic or fastidious in nature. Various media, both generalized and specific, have been used to match the in situ culture conditions of different methanogens inhabiting diverse environments (Cheng et al. 2007; Joshi et al. 2018; Khelaifia et al. 2013). Physiologically, methanogens are divided into three broad groups based on substrate requirements; hydrogenotrophic, methylotrophic, and acetotrophic or aceticlastic (Liu and Whitman 2008). Amongst, hydrogenotrophic methanogens utilize formate and H2: CO2 and are the most diverse, widely found, and fastest-growing (Zabranska and Pokorna 2018). The methylotrophic methanogens utilize methyl compounds like methylamines, and alcohols, including methanol, with a very few requiring a combination of hydrogen and methanol; while acetotrophic methanogens consume acetate (Demirel and Scherer 2008). Methanogens are integral to the microbial consortia in several industrially significant processes, like the degradation of organic wastes and xenobiotics and wastewater treatment (Enzmann et al. 2018). Hot springs are reported to harbour lignocellulolytic, hydrocarbon-degrading, and methane-producing microbes, serving as a promising source of thermophilic microbes and thermostable enzymes (Jardine et al. 2018; Kristjansson 1989; Mohammad et al. 2017; Tirawongsaroj et al. 2008; Yadav et al. 2018). Hot springs environments are also known to function as analogues for the hydrothermal systems of Mars, which are useful for habitability studies using methanogens (Hays et al. 2017). The Indian subcontinent is known to have more than 300 hot springs spread across seven geothermal provinces (Singh Bisht et al. 2011). Indian hot springs are majorly pristine niches and support diverse microbial communities (Narsing Rao et al. 2018; Poddar and Das 2018). The present study documents the diversity, distribution and phylogenetic relationships of culturable methanogens isolated from different Indian hot springs.
Materials and methods
Sampling, media, and enrichment
The water and sediment samples were collected from nine hot springs located across four geothermal provinces of India, namely Chumathang and Puga (Ladakh, Jammu and Kashmir); Unhavare, Tural, and Rajawadi (Western Maharashtra); two locations in Chopda, i.e., 1 and 2 (North Maharashtra); Unkeshwar (East Maharashtra) and Tattapani (Chhattisgarh). All hot springs were alkaline in nature, with pH ranging from 7.7 to 8.8, while the temperatures ranged from 40 to 80 ℃ (Table S1).
All the enrichments were set up in 60 ml glass serum bottles using two different media, i.e., BY (Joblin 2005) and BCYT (Touzel and Albagnac 1983) at four different temperatures of 40 ℃, 55 ℃, 70 ℃, and 85 ℃ (pH 6.8 ± 0.1). The BCYT medium comprised (per L) of 0.3 g KH2PO4, 0.6 g NaCl, 0.1 g MgCl2.6H2O, 0.08 g CaCl2.2H2O, 1 g NH4Cl, 0.5 g yeast extract, 0.5 g trypticase, 1 ml resazurin (0.2%, w/v), 1.5 g KHCO3, 10 ml each of trace element and vitamin solution, 1 g L-cysteine HCl, and 0.3 g Na2S.9H2O (Table S2). On the other hand, the BY medium contained (per L) 170 ml each of solution A and B, 5 g NaHCO3, 1 g yeast extract, 300 ml of centrifuged rumen fluid, 10 ml trace element solution, 1 ml resazurin (0.1%, w/v), 0.5 g L-cysteine HCl, and 10 ml vitamin solution (Table S2). The specific substrate requirements were provided for enriching each group of methanogens. For hydrogenotrophic methanogens, the medium was pressurized with H2: CO2 (80:20, v/v at 1 bar pressure) and re-pressurized weekly during incubation (Joshi et al. 2018). For the methylotrophic and acetotrophic groups, a methanol and trimethylamine mixture and sodium acetate were provided as substrates (final concentration, 50 mM), respectively. Streptomycin sulphate and benzylpenicillin were added to prevent bacterial contamination (final concentration, 200 µg/ml). The growth was monitored by checking the turbidity, fluorescence microscopy, and measurement of headspace methane using a gas chromatograph (Perkin Elmer, TCD, Argon carrier). The enrichments were checked for growth up to two months, after which they were scored positive or negative.
Isolation procedure
The positive enrichments were selected to isolate pure cultures of methanogens using serum bottle modification of the Hungate technique (Miller and Wolin 1974). For this, the dilutions were made up to 10−5, and 1 ml of inoculum from each dilution was added to 125 ml glass bottles containing 10 ml of the respective medium, substrate, and gelling agent. The agar (2%) or Gelrite (0.8% mixed with 0.1% MgCl2·6H2O) served as the gelling agents for mesophilic (40 ℃) or thermophilic (55–85 ℃) incubations, respectively. All the roll bottles were routinely checked for the growth of isolated colonies and methane production during incubation. After successful growth, the morphologically distinct colonies were picked under anaerobic conditions and grown under their respective growth conditions of media, substrate, and temperature.
Molecular characterization
The DNA of the pure cultures grown for 1 month was isolated using the cetyltrimethylammonium bromide (CTAB) method (Doyle 1991) with some modifications. Briefly, the cells were centrifuged at 10,510 rcf/10 min, and resultant pellets were suspended in 1 ml CTAB buffer and incubated at 50 ℃ with intermittent mixing until a clear solution was obtained. The solution was mixed with an equal volume of phenol: chloroform: isoamyl alcohol (P: C: I; 25:24:1), centrifuged, and the supernatant was mixed with an equal volume of C: I (24:1). Following re-centrifugation, an equal volume of isopropanol was added to the supernatant and incubated at -20 ℃ for 12 h. The visible DNA threads were centrifuged twice at 17,760 rcf/15 min, and the pellet was washed with pre-warmed 80% ethanol. The washed pellet was re-centrifuged and dried before re-suspending in 50–100 µl MilliQ water and stored at − 20 ℃ until used.
The isolated DNA of all cultures was used for the PCR amplification of the 16S rRNA gene using the primer pair 86F and 1340R (Wright and Pimm 2003). Meanwhile, the 16S rRNA gene sequences of different genera and species of methanogens were downloaded from Nuccore, NCBI. Further, the in silico restriction digestion analysis was performed using the Cleaver software to identify the most appropriate restriction enzyme (Jarman 2006). The amplified PCR products were then subjected to the PCR-restriction fragment length polymorphism (RFLP) analysis using the identified restriction enzyme as per the manufacturer's protocol.
The digested PCR products were separated by electrophoresis (60 V for 5 h; Bio-Rad PowerPac™ Basic) on 3% agarose gel containing GelRed® Nucleic Acid Gel Stain (Biotium) in FAST buffer (Brody and Kern 2004). The isolates showing different restriction patterns or having the same patterns but differing in sampling locations and growth conditions were outsourced for sequencing at 1st BASE, Singapore. Using the BioEdit software, the acquired sequences were aligned and assembled (Hall 1999). The sequence similarity searches were carried out using NCBI GenBank BLASTn, limiting to sequence from type material.
For phylogenetic analyses, the 16S rRNA gene sequences of type strains of nearest matches were downloaded from the NCBI GenBank database. All the obtained sequences were aligned using the ClustalW programme (Thompson et al. 1994) with default settings in MEGAXI (Tamura et al. 2021). The aligned sequences were used to construct a phylogenetic tree in MEGAXI using the maximum-likelihood method based on the Tamura-Nei model (Tamura and Nei 1993) and tested by 500 bootstrap replications.
Following identification, the roll tubes were prepared again to document the colony characteristics like shape, size and colour. The cellular morphology was studied using a phase contrast and fluorescence microscope (Eclipse 80i, Nikon, Japan).
Ecological distribution
To correlate the niche diversity of the obtained methanogen strains recorded in this study to closely related taxa, 16S rRNA gene sequences were queried with the GenBank dataset. All the closely related cultured and uncultured sequences were downloaded, and their phylogenetic positions were inferred using a maximum-likelihood-based phylogenetic tree using MEGAXI. Sequence comparison was conducted using BLASTn with > 90% OTU coverage, > 98.0% identity, and an e value of < 1e − 25. Additionally, the information on the habitat of related taxa was also recorded to understand the distribution across oxygen-restricted habitats.
Results and discussion
Enrichment and isolation
The abundance of archaea, in general, and methanogens, in particular, is usually less in a given niche than other microbes like bacteria (Aller and Kemp 2008; Flemming and Wuertz 2019). Hence, enrichment in the particular medium is desired to increase the population of targeted groups of methanogens. Methanogens have particular growth requirements that might differ for each genus or species (Joblin 2005; Whitman et al. 2014). The autotrophic methanogens require only the mineral medium to survive and grow, whereas the fastidious ones are known to have specific growth requirements in terms of amino acids, vitamins, trace elements, and co-enzymes (Joblin 2005; Saleem et al. 2013). These particular requirements are fulfilled by nutrient-rich components like rumen liquor, as in BY medium, which contains 28 different compound categories (Saleem et al. 2013). The rationale behind using two different media, viz. BCYT (basal mineral medium) and BY (with rumen liquor) was to facilitate the growth of both autotrophic and fastidious methanogens. Further, for the purpose of potential industrial applications, including anaerobic digestion, which generally function optimally at neutral pH; the similar pH range was selected for the enrichment process.
Of 216 total enrichments, 56 yielded positive results (Table S3). Samples from the western Maharashtra region yielded most of the positive enrichments, while the least were from the Ladakh region (Fig. 1). The maximum positive enrichments were obtained at 40 ℃ (28), followed by 55 ℃ (21), and 70 ℃ (7), whereas no enrichment was found positive at 85 ℃. It was observed that the enrichments across incubation temperatures (40–70 ℃) were obtained from the hot springs having high in situ temperature conditions (50–80℃), whereas positive enrichments at 40 ℃ were obtained majorly from lower temperature hot springs.
The substrate-wise analysis revealed the highest number of positive enrichments for hydrogenotrophic (total 26; 14 at 40 ℃, 9 at 55 ℃ and 3 at 70 ℃), followed by methylotrophic (total 18; 9 at 40 ℃, 7 at 55 ℃ and 2 at 70 ℃) and acetotrophic (total 12; 5 at 40 ℃, 5 at 55 ℃ and 2 at 70 ℃) methanogens (Table S3). In nature, the most abundant methanogens are hydrogenotrophic, as it is thermodynamically the most favourable reaction of all three (Garcia et al. 2000; Jabłoński et al. 2015). On the contrary, the process of acetotrophic methanogenesis is the least abundant in nature, as the reaction requires maximum free energy to proceed, resulting in less available energy (Deppenmeier and Müller 2008; Ferry 2011).
In the growth medium comparison, the BCYT medium supported the growth better, as indicated by 34 positive enrichments compared to 22 of the BY medium. No positive enrichment was obtained from the Tattapani sample, while Unhavare, Rajawadi and Tural hot springs yielded maximum positive enrichments across media, temperatures and substrates. The absence of growth in Tattapani enrichments can probably be attributed to the prevailing alkaline and high-temperature conditions, which might have limited the associated diversity.
The positive enrichments established at a mesophilic temperature of 40 ℃, particularly from the hot springs with a higher in situ temperature, indicate the presence of thermophilic and/ or thermotolerant methanogens capable of growing even at lower temperatures. Also, some of the hot springs are known to show seasonal and diurnal variations or the presence of gradients in the in situ temperature conditions that might also impact the population and diversity (Sigee 2005).
Thermophilic methanogens are known to have a faster growth rate and less doubling time than their mesophilic counterparts (Whitman et al. 2014); hence an earlier positive result was anticipated at higher temperatures. As expected, the enrichments set up at 55 ℃ and 70 ℃ were able to produce methane within 15 days of incubation, whereas the enrichments set up at 40 ℃ took three to four weeks to produce methane.
The isolation procedures from these enrichments led to the growth of morphologically diverse colonies of methanogens on roll bottles. Over 200 colonies were picked into their respective liquid medium and incubated at respective temperatures. Of the total colonies picked, the most diverse and most number of colonies were observed at 40 ℃, and a few at 55 ℃ but the roll tubes at 70 ℃ yielded only a single type and less number of colonies in all the samples.
Based on methane production, 120 isolates were noted positive, of which 78 were hydrogenotrophic (39 at 40 ℃, 26 at 55 ℃ and 13 at 70 ℃), 33 were methylotrophic (28 at 40 ℃ and 5 at 55 ℃) and 9 were acetotrophic (5 at 40 ℃ and 4 at 55 ℃).
Molecular characterization
The in silico analysis identified Hinf I as the most suitable restriction enzyme capable of generating different ribotypes (Table S4), thus differentiating methanogens at the genus level. The PCR amplification of isolated DNA generated PCR products of c.a. 1200 bp for all isolates. The actual restriction digestion of PCR products of one hundred and twenty isolates using Hinf I produced 6 types of restriction patterns (Fig. S1), which helped document the diversity and minimize the number of sequencing reactions. Seventy isolates were chosen for sequencing and identification based on differences in geographical locations and growing conditions.
The identification results established these isolates as members of ten different species under five genera; Methanothermobacter (Mtb.), Methanoculleus (Mcu.), Methanosarcina (Msc.), Methanomethylovorans (Mmv.) and Methanobacterium (Mbt.). All strains were members of families, Methanobacteriaceae, Methanomicrobiaceae, and Methanosarcinaceae of phylum Euryarchaeota (Table 1). Further, these cultures comprised all three groups, i.e., hydrogenotrophic (53), methylotrophic (14), and acetotrophic (3). From the hot springs of Ladakh, only the members of the thermophilic hydrogenotrophic genus Methanothermobacter were obtained; Mtb. thermautotrophicus (55 and 70 ℃, BY), and Mtb. marburgensis (55 ℃, BCYT) from Chumathang (Fig. 2a), and Mtb. thermautotrophicus (55 ℃, BCYT) from Puga (Fig. 2b). From the Unkeshwar hot spring of eastern Maharashtra, which had low in situ temperature, only hydrogenotrophic Mbt. formicicum was obtained on BY medium at 40 ℃ (Fig. 2c). From Rajawadi, Tural and Unhavare hot springs of western Maharashtra, which had in situ temperatures in the range of 50–65 ℃, three genera of methanogens viz., Methanothermobacter, Methanobacterium, and Methanomethylovorans were cultured. Amongst, maximum diversity was observed in Rajawadi (Fig. 2d), followed by Tural (Fig. 2e) and Unhavare (Fig. 2f) hot springs, from where four, three and two taxa of methanogens were isolated, respectively. At 40 ℃, members of the hydrogenotrophic genus Methanobacterium were isolated from Rajawadi (Mbt. bryantii) and Tural (Mbt. formicicum) hot springs on BY medium, and a putative novel species on BCYT medium from Rajawadi. In addition, a strict methylotrophic methanogen, Mmv. thermophila was also obtained at 40 ℃ from both these hot springs, but only on BY medium. At 55 ℃, Mtb. marburgensis was isolated from all three hot springs, whereas Mtb. thermautotrophicus was obtained only from Unhavare. Both Methanothermobacter spp. were obtained on both media. At 70 °C, only Mtb. marburgensis was isolated from the Tural hot spring, probably because of its higher in situ temperature than others. Methanogens belonging to all three groups, i.e., hydrogenotrophic, methylotrophic, and acetotrophic, were obtained from both the Chopda hot springs (northern Maharashtra) on BCYT medium; exclusively mesophilic from location 1 (Fig. 2g) but both mesophilic and thermophilic from location 2 (Fig. 2h). Two species of Methanobacterium, namely Mbt. formicicum and Mbt. bryantii and one putative novel species of methylotrophic Methanosarcina were cultured from location 1. From location 2, in addition to two species of Methanosarcina, i.e., Msc. mazei (40 °C), Msc. thermophila (40 °C, 55 ℃), and Mcu. hydrogenitrophicus (40 ℃) was also isolated. Some interesting observations were also made after analysing Venn diagrams to classify the methanogens according to the varying isolation conditions of medium, temperature, and substrate (Fig. 3). The media-wise analysis showed that three methanogens were obtained exclusively on BCYT medium, while two on BY medium (Fig. 3a). Fastidious methanogens such as Mbt. formicicum, which needs certain growth factors, amino acids, and co-enzymes, were isolated solely on BY medium (Khelaifia et al. 2013). In our earlier study, the BY medium was also found to support the growth of diverse hydrogenotrophic methanogens (Joshi et al. 2018). Also, Mmv. thermophila was cultured only on BY medium, probably owing to its specific requirement of cobalt, which is a constituent of BY medium (Jiang et al. 2005). In comparison, only the BCYT medium supported the growth of all the strains of Methanosarcina, which are known to be metabolically versatile. Msc. mazei requires trypticase and peptone for its growth and Msc. thermophila requires the growth factor p-amino benzoic acid. The presence of these components in the BCYT medium explains their successful cultivation. Interestingly, both the putative novel species were isolated only from the BCYT medium. Methanothermobacter and Methanoculleus, two genera recognized for their autotrophic nature, were cultured on both media (Whitman et al. 2014).
The temperature-based comparison revealed that except Mtb. thermautotrophicus, all other methanogen species were cultured at 40 °C (Fig. 3b). Barring, Msc. thermophila, only the members of the genus Methanothermobacter, Mtb. thermautotrophicus and Mtb. marburgensis were isolated at 55 °C and 70 ℃. Of these, Mtb. marburgensis, which optimally grows at 65 ℃, was found at all three temperatures (40, 55 and 70 ℃), signifying its broader temperature range (Wasserfallen et al. 2000). Various species of Methanobacterium, Methanosarcina, Methanoculleus, and Methanomethylovorans, including the two putative novel species, were cultured only at 40℃. Noticeably, Mmv. thermophila was obtained only at 40 °C, even though it has an optimal growth temperature in the thermophilic range (50 °C) (Jiang et al. 2005). A thermophilic acetotrophic methanogen, Msc. thermophila, which grows optimally at 50 ℃, was cultivated at 40 and 55 ℃ (Zinder et al. 1985). These results suggest that microbial diversity decreases with increasing temperature (Fig. S2). Such observations have been made in the past too, where various factors like the absence of vital enzymes at higher temperatures and specific requirements of thermophilic ecosystems to perform rare functions reportedly impact diversity (Ruhl et al. 2022; Sharp et al. 2014; Shu and Huang 2021). Also, the fact that thermophilic methanogens could be cultured even at low temperatures, but not vice versa, specifies their broader growth range. The broad temperature range of 40–75 °C for Mtb. marburgensis and Mtb. thermautotrophicus has been reported (Wasserfallen et al. 2000).
Substrate-wise, Mmv. thermophila, Msc. mazei and Methanosarcina sp. strain T40UC2 were isolated only on TMA + methanol, whereas Msc. thermophila was isolated on both, sodium acetate and TMA + methanol (Fig. 3c). The other six strains were strict hydrogenotrophs, comprising the members of the genus Methanothermobacter, Methanobacterium and Methanoculleus. Amongst, the genus Methanosarcina has been reported as the most versatile methanogen, capable of utilizing multiple substrates, even though strain level variation does occur (Maestrojuan and Boone 1991). In comparison, Mmv. thermophila is reported to be a strict methylotroph, and all hydrogenotrophs are known to utilize H2:CO2 or formate (Demirel and Scherer 2008; Jiang et al. 2005).
The relationship between the methanogens isolated in this study using 16S rRNA gene-based phylogenetic analysis was also analyzed, which revealed the grouping of all the cultures in three clusters representing three different families of methanogens, namely Methanobacteriaceae, Methanomicrobiaceae and Methanosarcinaceae (Fig. 4). It was observed that all strains of the genus Methanothermobacter were highly related despite having different origins. Similarly, two identical strains each of Mbt. bryantii (Rajawadi and Chopda 1), Mmv. thermophila (Rajawadi and Tural), and three strains of Mbt. formicicum (Chopda 1, Unkeshwar and Tural) were obtained from different locations across the Maharashtra region. We also report two putative novel species belonging to the genera Methanosarcina and Methanobacterium, forming a separate clade with Methanosarcina mazei and Methanobacterium bryantii, respectively.
The colony characters varied from pinpoint or large circular (Methanothermobacter, Methanoculleus), and irregular (Methanobacterium) to large clump-forming colonies (Methanosarcina and Methanomethylovorans). The fluorescence microscopy highlighted different cell morphology for each genus, like large clumps (Methanosarcina), small cocci (Methanoculleus), rods (Methanobacterium), long rods (Methanothermobacter) and large irregular cocci (Methanomethylovorans) (Fig. 4).
Ecological distribution
Methanogens have been found in various oxygen-restricted habitats (Liu and Whitman 2008). Though they prefer pH levels around neutral for their survival and proliferation, methanogens can grow across a broad range of temperature conditions, from psychrophilic to hyperthermophilic (Hoehler et al. 2010). Their substrate requirements also vary, but the most common and diverse methanogens represent the hydrogenotrophic group across broad pH and temperature conditions (Zabranska and Pokorna 2018). In this study, we were able to culture different strains of methanogens from Indian hot spring sediments, representing both mesophilic and thermophilic, and hydrogenotrophic, acetotrophic, and methylotrophic groups.
The majorly hydrogenotrophic genus Methanobacterium comprises 25 valid species (https://lpsn.dsmz.de/search?word=methanobacterium). Several of them are autotrophic and are found in habitats like anaerobic digesters, sewage sludge, aquatic sediments, marshy soils, gastrointestinal tracts of animals, geothermal areas, etc. (Boone 2015a; Whitman et al. 2014). In the present study, three species of this genus, including one putative novel species, were cultured from hot springs of Tural, Rajawadi, Unkeshwar and Chopda 1, showing widespread distribution in addition to previously known environments (Fig. S3). The phylogenetic analysis showed that all the isolated Mbt. formicicum strains (Unkeshwar, Chopda 1 and Tural hot springs) were related to the ones obtained from a pig slurry digester (Korea), biogas reactor (Germany), farm animals (New Zealand), sheep rumen and cow dung (India) and gas storage facility (Russia). The related uncultured clones were found in an anaerobic digester (Netherlands) and wastewater reactor (Japan). The Mbt. bryantii strains cultured from Rajawadi and Chopda hot springs were related to the strains isolated from a sewage digester (Germany), methane hydrate (India), rice field soils (France), and a goat faecal sample (India), and uncultured clones from rice paddy fields (Japan), coal bed water (China), and a faecal sample (UK). The putative novel Methanobacterium sp. strain R40H9 isolated from Rajawadi hot spring showed no similarity to cultured or uncultured sequences.
The genus Methanothermobacter comprises eight valid species (https://lpsn.dsmz.de/search?word=Methanothermobacter), all of which are thermophilic, hydrogenotrophic and autotrophic and are mainly found in oil fields and anaerobic digesters (Boone 2015b; Boone et al. 2015a). Except for Unkeshwar and Chopda, two Methanothermobacter species, Mtb. thermautotrophicus and Mtb. marburgensis were isolated from every hot spring (Fig. S4). The strains of Mtb. thermautotrophicus obtained were related to isolates from a power gas reactor (Germany), bay sediments (China), oil fields (Russia and India), and uncultured clones from oil fields (Japan and Singapore). While an uncultured affiliate was from a saline lake in Spain, the cultured affiliates of Mtb. marburgensis strains were related to isolates from sewage digesters/thermophilic biogas plants (Germany) and hot springs (China and India).
Methanoculleus is one of the most physiologically diverse genera and contains 11 valid species (https://lpsn.dsmz.de/search?word=Methanoculleus), which inhabit a range of environments with varying temperatures, substrates, and salinities, including marine, freshwater, and volcano sediments, bioreactors, etc. (Boone et al. 2015b; Lai 2019) A single species, Mcu. hydrogenitrophicus strains were obtained from only one hot spring (Chopda 2) in this study, which was related to the isolates from wetland soil (USA and India), and uncultured clones from rumen fluid (China); and cattle manure compost, rice paddy soil and groundwater from sedimentary rock (Japan) (Fig. S5).
The genus Methanomethylovorans comprises three valid species (https://lpsn.dsmz.de/search?word=Methanomethylovorans), all of which are strictly methylotrophic and reported from freshwater/ wetland sediments and anaerobic digesters (Boone et al. 2015c; Kim and Rhee 2019). In this work, only the Mmv. thermophila strains were isolated from Tural and Rajawadi hot springs and were phylogenetically identical to Mmv. thermophila type strain (thermophilic anaerobic digester, USA). Our strains also grouped alongside uncultured clones reported from hot springs (Taiwan and Armenia), oil reservoirs (USA) and anaerobic digesters (Netherlands) (Fig. S6).
Methanosarcina is metabolically the most versatile of methanogens and comprises 14 valid species (https://lpsn.dsmz.de/search?word=Methanosarcina), which can be distinctly identified because of their aggregate or clump-forming quality. The members of this genus are present across all three physiological groups and reported from diverse environments like anaerobic digesters and various sediments (Boone et al. 2015c; Wagner 2020). Methanosarcina members are known to be fast-growing and robust and were isolated only from Chopda hot springs in this study. We cultivated three species, including a putative novel one from Chopda 1 and, Msc. thermophila and Msc. mazei from Chopda 2 hot springs. The strains of Msc. thermophila were closely related to the cultured strains isolated from an anaerobic digester (USA) and a termite gut (India). The related uncultured clones were obtained from cattle manure compost (Japan). The strains of Msc. mazei were closely related to the isolates from the estuarine environment and marine sediment (Taiwan), while uncultured clones were obtained from cattle manure compost (Japan). As expected, Methanosarcina sp. strain T40UC2, isolated from Chopda 1 location, did not have any related cultured affiliates, but similar uncultured clones were found from a thermal vent of Yellowstone (USA). (Fig. S7).
In contrast to the diverse methanogens cultured in the current study, most of the comparable strains have been reported majorly from artificial environments like digesters, wastewater treatment plants, etc., which highlights the relevance of these hot springs as holding a unique collection of diverse methanogens.
Conclusion
The hot springs harbour diverse methanogenic archaeal communities, making them a unique environmental niche for studying microbial processes and potential industrial applications. We successfully cultivated five genera and ten mesophilic and thermophilic methanogen species representing hydrogenotrophic, methylotrophic and acetotrophic physiological groups. The most diverse sets of taxa were obtained at 40 ℃ on both BY and BCYT media, whereas higher incubation conditions majorly supported the growth of hydrogenotrophic methanogens. While methanogens with specific nutrient requirements were cultivated on either BY or BCYT medium, both media supported the growth of autotrophic methanogens. Some methanogen genera, like Methanoculleus, Methanosarcina, and Methanomethylovorans, were restricted to particular hot springs, whereas the methanogens belonging to Methanobacterium and Methanothermobacter were widespread over several hot springs across geothermal regions. This study also documents two putative novel species in the Methanobacterium and Methanosarcina genera, unravelling their taxonomy, diversity and distribution. To the best of our knowledge, our study represents the first report of the isolation of Mmv. thermophila, Msc. thermophila, Msc. mazei and Mbt. bryantii from hot spring habitats. This study also suggests that Hinf I can be used to differentiate different genera of methanogens using PCR–RFLP. Changing media and temperature conditions were shown to isolate distinct methanogens from the same environmental niches selectively. Further work needs to be conducted to compare the growth rate of different methanogens, following which efficient strains can accelerate rates of various microbial processes.
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Acknowledgements
The authors are thankful to Dr Karthick Balasubramanian, Agharkar Research Institute, Pune and Dr. Raymond A Duraiswami, Savitribai Phule Pune University, for sampling support. We duly acknowledge the help Mr. Sai Hivarkar and Mr. Radhakrishnan Cheran extended during the study. We also appreciate the technical assistance from Dr. Vikram Lanjekar. We are grateful to the Director, Agharkar Research Institute for providing the necessary infrastructure support.
Funding
The authors acknowledge the support of the Science and Engineering Research Board (SERB), Department of Science and Technology (DST) for financial support (Project no. YSS/2015/000718). Kasturi Deore thankfully acknowledges University Grants Commission, Delhi (India) for the junior research fellowship (Ref. No. 23/06/2013(i)EU-V).
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SSD and PKD conceived the project and designed the experiments. KSD conducted the experiments, analysed the data and wrote the first draft of the manuscript. PKD and SSD revised the manuscript. All authors have read and approved the final version of the manuscript.
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Deore, K.S., Dhakephalkar, P.K. & Dagar, S.S. Phylogenetically and physiologically diverse methanogenic archaea inhabit the Indian hot spring environments. Arch Microbiol 205, 332 (2023). https://doi.org/10.1007/s00203-023-03661-2
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DOI: https://doi.org/10.1007/s00203-023-03661-2