Summary
Methoxylated aromatic compounds (MACs) are important components of lignin found in significant amounts in the subsurface. Recently, the methanogenic archaeon Methermicoccus shengliensis was shown to be able to use a variety of MACs during methoxydotrophic growth. After a molecular survey, we found that the hyperthermophilic non‐methanogenic archaeon Archaeoglobus fulgidus also encodes genes for a bacterial‐like demethoxylation system. In this study, we performed growth and metabolite analysis, and used transcriptomics to investigate the response of A. fulgidus during growth on MACs in comparison to growth on lactate. We observed that A. fulgidus converts MACs to their hydroxylated derivatives with CO2 as the main product and sulfate as electron acceptor. Furthermore, we could show that MACs improve the growth of A. fulgidus in the presence of organic substrates such as lactate. We also found evidence that other archaea such as Bathyarchaeota, Lokiarchaeota, Verstraetearchaeota, Korarchaeota, Helarchaeota and Nezhaarchaeota encode a demethoxylation system. In summary, we here describe the first non‐methanogenic archaeon with the ability to grow on MACs indicating that methoxydotrophic archaea might play a so far underestimated role in the global carbon cycle.
Introduction
Aromatic compounds are produced by plants, animals and microorganisms and are therefore quite abundant on earth. The polyaromatic compound lignin can be found in significant amounts in the subsurface. Lignin is a major component of photosynthetic biomass and makes up approximately 25% of the dry weight of vascular plants (Zeikus, 1981). It is further estimated that approximately one third of the organic matter present in marine sediments is of terrestrial origin (Burdige, 2005). Overall, lignin analysis indicated that peat and coastal marine sediments contained about 20%–50% of recognizable vascular plant carbon and soils of offshore marine sediments about 0%–10% (Ertel and Hedges, 1984).
There are many possibilities for substitutions on the aromatic ring and one of those possible ring modifications is the addition of methoxy groups resulting in so‐called methoxylated aromatic compounds. Lignin contains about 3% methoxy groups respectively (Lee et al., 2019) and methoxylated aromatic compounds as major components of lignin are quite abundant in natural environments (Hedges et al., 1982; Colberg, 1988). Alkyl‐methoxyphenols have been found to be typical pyrolysis products of lignin‐derived materials (Salmon et al., 1997). It is well known that methoxylated aromatic compounds can be degraded by bacteria. Already in 1979, it was shown that methoxylated aromatic compounds can be converted to methane by the syntrophic association of several anaerobic microorganisms (Healy and Young, 1979). Acetogenic bacteria were the first anaerobes discovered to use methoxylated aromatic compounds for energy conservation (Bache and Pfennig, 1981) via conversion of the methyl group to acetate in the acetyl‐CoA (Wood‐Ljungdahl) pathway. Some bacteria such as Sporobacter termitidis (Grech‐Mora et al., 1996), Sporobacter olearium (Mechichi et al., 1999) and Parasporobacterium paucivorans (Lomans et al., 2001) are able to cleave the aromatic ring after O‐demethylation and convert methoxylated aromatic compounds to acetate, methanethiol or dimethylsulfide. O‐demethylation is an essential step preceding aromatic ring cleavage. Next to these ring‐cleaving methoxydotrophic acetogens, several acetogens have been described to O‐demethylate methoxylated aromatic compounds and to release the corresponding hydroxylated derivatives into the environment without cleaving the aromatic ring. The methoxy group is transferred into the acetyl‐CoA pathway resulting in formation of products such as acetate. Examples of this type of methoxydotrophic acetogens are Sporomusa termitida (Breznak et al., 1988), Clostridium thermoaceticum (Wu et al., 1988) and Acetobacterium woodii (Bache and Pfennig, 1981). Acetogens use two methyltransferases, one corrinoid protein and one activating enzyme that recycles the corrinoid protein for transfer of the methyl group from methoxylated compounds (Kaufmann et al., 1997). These enzymes catalyse the O‐demethylation of the methoxylated compound and methyl transfer to the corrinoid protein as well as subsequent methyl transfer to tetrahydrofolate.
In contrast to the well‐studied methoxydotrophic growth of acetogenic bacteria, archaea were not well investigated for their ability of converting methoxylated aromatic compounds. It was only recently, that the thermophilic methanogen Methermicoccus shengliensis was shown to be able to use a variety of methoxylated aromatic compounds for growth and produces methane from the methoxy group (Mayumi et al., 2016). M. shengliensis appears to use a similar O‐demethylation system as acetogenic bacteria, composed of the so‐called Mto proteins (Kurth et al., submitted): MtoB is the O‐demethylase that transfers the methyl group to the corrinoid protein MtoC, MtoD is the reductive activase of MtoC, and MtoA is a methyltransferase that most likely transfers the methyl group to tetrahydromethanopterin (H4MPT). Discovery of a methoxydotrophic methanogen together with the prevalence of methoxylated compounds on earth lead us to assume that methoxydotrophic archaea might play a so far underestimated role in the global carbon cycle, especially in the subsurface (Welte, 2016). To further support this hypothesis, we aimed to identify additional methoxydotrophic archaea. A BlastP (NCBI)) analysis of the genes encoding the Mto proteins in M. shengliensis (BP07_03250‐60) revealed that the hyperthermophilic archaeon Archaeoglobus fulgidus possesses a similar gene cluster, encoding the Mto proteins (AF_0006‐AF_0013). Similar to Methermicoccus, A. fulgidus (Stetter et al., 1987) belongs to the phylum Euryarchaeota and is related to methanogens. The organism grows anaerobically at extremely high temperatures around 80°C and has been described to be present in marine hydrothermal systems (Stetter et al., 1987) and oil reservoirs (Beeder et al., 1994; Stetter and Huber, 1998). In marine hydrothermal systems, aromatic compounds such as benzenes and phenols have been described as the major organic compounds alongside aliphatic hydrocarbons and carboxylic acids (Konn et al., 2009). Concentrations of about 2–4 μg/g soil have been detected in a hydrothermal chimney and sediment (Wang et al., 2020). Furthermore, aromatic compounds are a major component (20%–43%) of crude oil (Libes, 2009; Meslé et al., 2013). A. fulgidus has been described to couple the reduction of sulfate or thiosulfate with the oxidation of many different organic carbon sources such as small organic acids like lactate, pyruvate, formate (Stetter et al., 1987; Stetter, 1988) or amino acids like phenylalanine (Parthasarathy et al., 2013). The organism also oxidizes fatty acids (C4 to C18) and n‐alk‐1‐enes (C12:1 to C21:1) in the presence of thiosulfate as a terminal electron acceptor producing CO2 and sulfide (Khelifi et al., 2010). Moreover, A. fulgidus has been shown to grow on CO and sulfate thereby producing CO2, sulfide and acetate (Henstra et al., 2007; Hocking et al., 2015) and on H2 plus CO2 with thiosulfate as electron acceptor (Hocking et al., 2014). Furthermore, A. fulgidus can use perchlorate and nitrate as electron acceptor during hydrocarbon conversion, indicating its very versatile metabolism (Liebensteiner et al., 2013, 2014). A. fulgidus converts organic acids to CO2 via an acetyl‐CoA pathway that involves similar enzymes and cofactors as found in methanogens (Möller‐Zinkhan et al., 1989; Möller‐Zinkhan and Thauer, 1990). A. fulgidus does not encode methyl‐CoM reductase and thus lacks the potential to produce methane (Klenk et al., 1997). In this study, we performed growth experiments, analysed the substrate consumption and product formation and the difference in gene expression of A. fulgidus grown on methoxy compounds versus lactate. We demonstrate that A. fulgidus can grow on methoxylated aromatic compounds and thereby identify the first non‐methanogenic archaeon capable of methoxydotrophic growth.
Results
Growth of A. fulgidus on methoxylated aromatic compounds versus lactate
After a genome analysis, we identified an O‐demethylation system in A. fulgidus. To experimentally verify if A. fulgidus can use this system, we grew the microorganism on 2‐methoxyphenol (MP), and compared this to growth on lactate (Fig. 1). Thus, we could show that A. fulgidus is able to grow on MP and converts it to 2‐hydroxyphenol (HP) (Fig. 1A–C). When 7.5 and 12 mM MP were added, MP was completely converted to HP. However, the increase in doubling time (from 9.4 to 20 h) with higher MP concentrations (Fig. 1A–C) points to an inhibiting or toxic effect of high concentrations of methoxylated aromatics (or their products) on the growth of A. fulgidus. At 30 mM MP, no growth could be observed. Overall, growth on MP is comparable to growth on lactate (Fig. 1A, B, D), with a similar doubling time (9.4 vs. 14.4 h) of cultures with 7.5 mM MP and a similar final optical density (OD) of cultures with 12 mM MP compared to the lactate containing cultures (see below and Fig. 3 for details). When A. fulgidus is cultured in medium containing both lactate and MP, MP improves the growth of the organism resulting in a higher final OD and decreased doubling time (Fig. 1E). Next to 2‐methoxyphenol, growth on methoxylated aromatics such as 2,6‐dimethoxyphenol, methoxyhydroquinone and 2‐methoxybenzoate was observed. No growth could be observed on methanol, indicating that there might be no methanol‐converting enzyme present in A. fulgidus.
The metabolite production and electron acceptor use of A. fulgidus during methoxydotrophic growth were investigated. Therefore CO2, acetate, formate, sulfate and sulfide concentrations were measured in experiments with methoxy compounds and lactate (Fig. 2). It appeared that similar amounts of CO2 are produced in cultures grown on MP and lactate (Fig. 2A). In a resting cell experiment (Fig. 2B), cells grown on lactate produce (a little) more CO2 in the exponential phase than cells grown on methoxyphenol. The reason might be that – during growth – also acetate and formate are produced (Fig. 2C and D), but during the resting cell experiment CO2 might be the main product. Another reason could be that cells grown on methoxyphenol were not that metabolically active during the resting cell experiment due to the toxic effect of MP which might be enhanced in the stabilizing buffer used for the experiment compared to medium. The stabilizing buffer contains potassium phosphate, magnesium sulfate, sodium chloride and sucrose, but lacks ammonium, trace elements, yeast extract and CO2. The cells are able to metabolize the substrates in this buffer, but are unable to grow. Extrapolation of the resting cell experiment results would lead to CO2 production of about 370 μmol CO2 per culture produced during growth on MP and 420 μmol during growth on lactate. In medium without added CO2 or bicarbonate A. fulgidus was only able to grow when lactate was the substrate but not with MP. This indicates that CO2 is required for assimilation when MP is the substrate. Next to CO2, acetate and formate were major products during growth on lactate (Fig. 2C and D). However, during growth on MP only small amounts of acetate (<20 μM) and formate (<50 μM) were produced (Fig. 2C and D). During both MP and lactate conversion, sulfate is consumed and thereby used as electron acceptor (Fig. 2E). Concomitant sulfide production was also observed (Fig. 2F). Both sulfate consumption and sulfide production were lower in MP grown cells compared to lactate grown cells. In both cases, lower concentrations of sulfide could be measured than sulfate consumed, which might be due to the reactivity of sulfide and/or the use of sulfide for assimilation.
To get a better insight into the metabolism of A. fulgidus grown on MP compared to lactate, the concentrations measured for MP, HP, lactate (all shown in Fig. 1) and for CO2, acetate, formate, sulfate, sulfide (all shown in Fig. 2) per culture were incorporated into a schematic overview (Fig. 3). During growth on lactate mainly acetate, CO2 and formate are produced. Electrons liberated during lactate conversion to pyruvate and acetyl‐CoA as well as during the reductive acetyl‐CoA pathway, resulting in CO2 formation, are used for sulfate reduction. During growth on MP, part of the methoxy group is oxidized to CO2 resulting in liberation of electrons which can be used for sulfate reduction and the other part is combined with CO2 to acetyl‐CoA, from which cell components for assimilation are synthesized. As shown before, only very small amounts of formate or acetate are produced during growth on MP, demonstrating that CO2 is the main product. Furthermore, it is possible that amino acids such as glutamate that are present in the yeast extract of the medium might be co‐assimilated, resulting in mixotrophic growth, as it has been described previously that A. fulgidus has the genetic potential to degrade a variety of hydrocarbons and organic acids (Klenk et al., 1997).
A metabolite analysis of A. fulgidus cells grown under different conditions (Supporting Information Fig. S1) revealed that A. fulgidus cells contained less pyruvate, succinate, citrate, fumarate when grown on MP compared to growth on lactate, which can be partly explained by the growth of A. fulgidus on MP and its conversion via the reductive acetyl‐CoA pathway instead of growth on organic acids. Furthermore, 2‐oxoglutarate was only detected in lactate‐grown cultures. In contrast, glutamate was detected in all cultures in comparable amounts.
Transcriptomic analysis
After analysing which products were formed during growth on MP and lactate, we also wanted to investigate how the gene expression differs under the two growth conditions and which genes are important for methoxydotrophic growth (Supporting Information Tables S1 and S2). The three most upregulated gene clusters under methoxydotrophic growth compared to growth on lactate are shown in Fig. 4. The first gene cluster (Fig. 4A) contains the genes that were identified for M. shengliensis to be important for growth on methoxy compounds (Kurth et al., submitted). This gene cluster encodes the O‐demethylase MtoB, which is responsible for O‐demethylation of the methoxy compound, the cobalamin binding protein MtoC that accepts the methyl group from MtoB, the reductive activase of MtoC named MtoD, the methyl transferase MtoA which most likely transfers the methyl group from MtoC to tetrahydomethanopterin (H4MPT) and major facilitator superfamily transporters that might be involved in import of the methoxylated aromatic compounds and export of the hydroxylated derivatives. The role of these enzymes is depicted in Fig. 5.
Another highly upregulated gene cluster encodes for two F420‐non‐reducing hydrogenases, Vht and Vhu, and for a heterodisulfide reductase (Hdr) complex. The cytoplasmic Vhu hydrogenase (also referred to as Mvh hydrogenase) is assumed to be associated with the Hdr complex (Hocking et al., 2014). The Vht hydrogenase contains a membrane subunit and is most likely located in the pseudoperiplasm. As no hydrogen gas was added to the cultures and no production of hydrogen could be detected, there is most likely an internal hydrogen cycling occurring in the cells. H2 might be produced by the Hdr/Vhu complex and reoxidized by the periplasmic Vht hydrogenase, contributing to the proton gradient and reducing menaquinone. The third gene cluster that is highly overexpressed under MP growth encodes the 2‐oxoglutarate/2‐oxoacid ferredoxin oxidoreductase KorABDG. This enzyme can be part of the tricarboxylic acid (TCA) cycle and catalyses the reversible conversion of 2‐oxoglutarate to succinyl‐CoA and reduction of ferredoxin, therefore potentially playing a role in regenerating/providing reducing equivalents. The 2‐oxoglutarate might derive from glutamate which is present in the yeast extract provided to the medium. Next to those three gene clusters also genes encoding for proteins involved in lipid metabolism, more precisely fatty acid activation and β‐oxidation, are highly upregulated. Those highly upregulated genes encode for proteins such as the long‐chain‐fatty‐acid‐CoA ligase FadD, the acyl‐CoA dehydrogenase Acd, the enoyl‐CoA hydratase Fad, the 3‐hydroxyacyl‐CoA dehydrogenase Hbd, the 3‐ketoacyl‐CoA thiolase AcaB and FadA, the medium‐chain acyl‐CoA ligase AlkK and the 4‐hydroxybutyrate CoA transferase Cat2 (Fig. 6, Supporting Information Tables S1 and S2). Other genes that are strongly induced under MP growth are genes encoding branched‐chain amino acid ABC transporter subunits (Supporting Information Table S2) involved in amino‐acid uptake, genes encoding acyl‐CoA synthetase Acs, which might play a role in acetate activation or fatty acid activation, as well as genes encoding putative acyl‐CoA transferase/formyl‐CoA transferases. Similar observations were made in a transcriptomic study with A. fulgidus cell grown on H2/CO2 versus lactate (Hocking et al., 2014) and might therefore be associated with the growth of A. fulgidus on substrates other than organic acids and putatively the co‐assimilation of lipids, amino acids and other organic compounds, resulting in mixotrophic growth.
Genes that are downregulated during growth on MP (Supporting Information Table S3) encode proteins involved in ammonia uptake (Amt) and glutamine metabolism/nitrogen regulation (GlnA, GlnB), ferrous iron transport (FeoB), phosphate transport (PstSABC) as well as pyruvate metabolism (PorABDG). Ammonia and glutamine metabolism might be downregulated because of co‐assimilation of amino acids such as glutamate, which would match with the upregulation of korABDG. Genes encoding the pyruvate ferredoxin oxidoreductase PorABDG are most likely downregulated as less pyruvate is produced due to the lack of lactate conversion. The downregulation of genes involved in ferrous iron and phosphate uptake might correlate with a decreased production of iron–sulfur and polyphosphate bodies that have been described for A. fulgidus cells (Toso et al., 2016). The iron–sulfur bodies store iron, sulfur plus copper and the polyphosphate bodies contain phosphorus plus magnesium, calcium, and aluminium. Those iron–sulfur and polyphosphate bodies are assumed to be involved in energy storage and/or metal sequestration/detoxification.
Proteins involved in the metabolism of methoxylated aromatics, acetyl‐CoA/Wood‐Ljungdahl pathway, lactate metabolism, TCA cycle, sulfate reduction, energy metabolism and regeneration of reducing equivalents are shown in Fig. 7 (for details see also Fig. 6 and Supporting Information Table S1) with the respective transcription profile for growth on MP versus lactate. There is no significant change in transcription regarding genes encoding proteins involved in sulfate reduction and acetyl‐CoA pathway. This matches with the observation that sulfate serves as electron acceptor and CO2 is produced under both growth conditions. Regarding energy metabolism and regeneration of reducing equivalents, only genes encoding for the Hdr complex and the two hydrogenases (Vht and Vhu) are upregulated on MP. In view of the TCA cycle, some of the genes encoding proteins involved in the stepwise conversion from 2‐oxoglutarate to pyruvate are upregulated (KorABDG, SdhABCD, Fum, Pyc), whereas genes encoding proteins involved in citrate and isocitrate formation are downregulated (Cit, Acn). Those observations are discussed below.
Discussion
Methoxydotrophic growth – O‐demethylation of methoxylated aromatic compounds
In this study, we demonstrate that A. fulgidus can grow on methoxylated aromatic compounds such as 2‐methoxyphenol. Similar to some acetogenic bacteria, e.g. Sporomusa termitida (Breznak et al., 1988), Clostridium thermoaceticum (Wu et al., 1988) and Acetobacterium woodii (Bache and Pfennig, 1981), as well as the methanogenic archaeon M. shengliensis (Kurth et al., submitted; Mayumi et al., 2016), A. fulgidus converts methoxylated aromatic compounds to their hydroxylated derivatives (Fig. 1). Surprisingly, both the archaea M. shengliensis and A. fulgidus use an O‐demethylation system that is similar to that of acetogenic bacteria (Fig. 5 and Kurth et al., submitted). The enzymes that are part of this system are encoded in a gene cluster that is highly induced under methoxydotrophic conditions (Fig. 4A). These MtoABCD proteins facilitate O‐demethylation of the methoxy compound and methyl transfer via a corrinoid protein to most probably tetrahydromethanopterin (H4MPT) (Kurth et al., submitted). The acetyl‐CoA pathway of A. fulgidus has been shown to rather involve tetrahydromethanopterin than tetrahydrofolate as C1‐carrier (Möller‐Zinkhan et al., 1989) which differs to acetogenic bacteria but strengthens the hypothesis that MtoA transfers the methyl group to H4MPT in A. fulgidus. The produced methyl‐H4MPT can then be oxidized to CO2 via the reductive acetyl‐CoA pathway, generating reducing equivalents which provide electrons for sulfate reduction directly via ferredoxin or indirectly via reduced menaquinone (Fig. 7). We could further show that growth characteristics for MP as substrate were comparable to those for lactate (Fig. 1). However, MP concentrations of 12 mM and higher had an inhibiting effect on growth, which might be due to the toxic effect of aromatic hydrocarbons or their products. At lower concentrations, however, methoxy compounds improved the growth of A. fulgidus in the presence of lactate. As A. fulgidus thrives in environments such as hydrothermal marine systems (Stetter et al., 1987) and oil reservoirs (Beeder et al., 1994; Stetter and Huber, 1998) where aromatic compounds are present (Konn et al., 2009; Libes, 2009; Meslé et al., 2013) the ability to use methoxylated aromatics for growth might lead to a growth advantage over organisms that are incapable of methoxydotrophic growth. Furthermore, the use of methoxylated aromatics as co‐substrate to organic acids such as acetate or lactate, amino acids, fatty acids or sugars might be more prevalent than so far assumed in marine environments and subsurface sediments as methoxy compounds are quite abundant on earth.
Bioinformatic analysis revealed that also other archaea that thrive in hydrothermal deep‐sea sediments such as members of the phyla Bathyarchaeota, Lokiarchaeota, Korarchaeota, Helarchaeota, Verstraetearchaeota and Nezhaarchaeota contain mtoABC homologues in their genomes (Fig. 8). The latter three organisms are assumed to be involved in methane and/or alkane metabolism (Hua et al., 2019; Seitz et al., 2019; Wang et al., 2019). Bathyarchaeota are very abundant in marine subsurface sediments and have the potential for acetogenesis and for the fermentative utilization of a variety of organic substrates (He et al., 2016). Furthermore, they have been described to be able to grow on lignin (Yu et al., 2018). Also for Lokiarchaeota, it is assumed that they have the potential to degrade lignin besides other substrates, such as humic acids, lactate, aromatic compounds and proteins (Yin et al., 2020). The presence of mto homologues in those archaea therefore might suggest that they are able to grow on MACs.
Metabolism – products formed and electron acceptor used during methoxydotrophic growth
We observed that next to 2‐hydroxyphenol, CO2 is the main carbon compound produced by A. fulgidus during growth on MP, whereas substantial amounts of acetate and formate are produced besides CO2 during growth on lactate (Fig. 2). During methoxydotrophic growth, the methoxy/methyl group ends up as methyl‐H4MPT in the acetyl‐CoA pathway and is then either oxidized to CO2 resulting in generation of reducing equivalents or combined with CO2 to form acetyl‐CoA which is required for assimilation (Fig. 3). When lactate is used as carbon and energy source, reducing equivalents are generated during oxidation of lactate to acetyl‐CoA via pyruvate, but also during oxidation of acetyl‐CoA to CO2 in the reductive acetyl‐CoA pathway. Moreover, ATP can directly be generated from the conversion of acetyl‐CoA to acetate. Formate and CO2 are side products from the oxidation of pyruvate to acetyl‐CoA. The produced acetyl‐CoA can further also be used for assimilation. Production of acetate, formate, and CO2 from lactate has already been shown previously and the stoichiometry of the catabolic reaction seems to strongly dependent on the sulfate concentration (Habicht et al., 2005). In our study, sulfate was reduced to sulfide under both growth conditions and therefore serves as electron acceptor.
Energy metabolism and regeneration of reducing equivalents
Regarding energy metabolism and regeneration of reducing equivalents, mainly genes encoding for the Hdr complex and the two hydrogenases (Vht and Vhu) are upregulated (Fig. 7 and Supporting Information Table S1). This might be due to an increased concentration of reduced ferredoxin (Fdred) in the cells which most likely result from increased production of Fdred in the reductive acetyl‐CoA pathway (CO2 is the main carbon compound produced during growth on MP), the putative increased production of Fdred by 2‐oxoglutarate ferredoxin oxidoreductase KorABDG (upregulation of korABDG genes) and a decrease in sulfate reduction (less sulfate is reduced during growth on MP) which might involve Fdred as electron donor as Qmo and DsrAB have Fd binding sites (Hocking et al., 2014). Although less Fdred is assumed to be produced by pyruvate ferredoxin oxidoreductase PorABDG (downregulation of porABDG genes), there might still be an increased concentration of Fdred in cells grown on MP compared to cells grown on lactate. Fdred is the most likely electron donor for the Hdr/Vhu complex, as cultures are not grown on H2. Reoxidation of Fdred by the Hdr/Vhu complex putatively involves oxidation of DsrC (two SH‐groups) and reduction of H+ to H2, which could then be oxidized by the pseudoperiplasmic Vht hydrogenase contributing to the proton motive force. The internal hydrogen cycling under methoxydorophic growth conditions is supported by the observation that there was no net production or consumption of hydrogen in the cultures. For the sulfate‐reducing bacterium Desulfovibrio gigas, it has been described that hydrogen cycling takes place in lactate‐grown cultures and led to the assumption that hydrogen cycling with vectorial electron transfer might be a general mechanism for energy coupling in sulfate‐reducing bacteria (Odom and Peck, 1981). However, in A. fulgidus the hydrogenases are hardly induced in lactate grown cultures (this study and Hocking et al., 2014; see also Fig. 6) indicating that hydrogen cycling only plays a role when the organism grows on substrates other than organic acids and H2. Under growth on H2/CO2 and partly also under growth on CO compared to growth on lactate the genes encoding the aforementioned hydrogenases and Hdr proteins are also upregulated (Fig. 6 and Hocking et al., 2014, 2015) indicating that they play a general role in energy metabolism and regeneration of reducing equivalents during autotrophic or mixotrophic growth of A. fulgidus. Internal hydrogen cycling has also been observed in acetogens such as Acetobacterium woodii (Wiechmann et al., 2020).
Regarding the TCA cycle, some of the genes encoding proteins involved in the stepwise conversion from 2‐oxoglutarate to pyruvate are upregulated (KorABDG, SdhABCD, Fum, Pyc), whereas genes encoding proteins involved in citrate and isocitrate formation are downregulated (Cit, Acn) (for comparison Fig. 7 and Supporting Information Table S1). This might be due to the upregulation of genes encoding the 2‐oxoglutarate ferredoxin oxidoreductase KorABDG, which might play a role in Fdred production and therefore providing/regenerating reducing equivalents. The metabolite analysis of A. fulgidus cells (Supporting Information Fig. S1) revealed that A. fulgidus cells contained less of some TCA cycle metabolites such as succinate, or fumarate when grown on MP compared to growth on lactate. Next to the lack of lactate and pyruvate also an upregulation of genes encoding for TCA cycle proteins might explain this finding and fits to the transcriptomic results mentioned before. The absence of 2‐oxoglutarate in MP‐grown cells (Supporting Information Fig. S1) is in agreement with the upregulation of the korABDG genes and further indicates that KorABDG indeed converts 2‐oxoglutarate to succinyl‐CoA resulting in Fdred production and does not primarily catalyse the reverse reaction. Furthermore, less Fdred is produced by PorABDG due to the lack of pyruvate providing compounds such as lactate which was evidenced in this study by downregulation of the porABDG genes and the metabolite analysis (Supporting Information Table S1 and Fig. S1). KorABDG might compensate for that by providing Fdred. However, the source of 2‐oxoglutarate could not be detected yet. We assume that glutamate or other amino acids might be converted to 2‐oxoglutarate as amino acids are present in the yeast extract provided to the medium. However, putative glutamate converting enzymes such as the aspartate aminotransferase AspBC are not upregulated under methoxydotrophic growth. However, a quarter of the A. fulgidus genome encodes functionally uncharacterized proteins (Klenk et al., 1997) so we might have overlooked a hitherto undescribed glutamate converting enzyme. A gene encoding an aspartate aminotransferase family protein/glutamate decarboxylase is highly upregulated on MP (AF_2295) which could have a role in glutamate conversion. It might also be possible that glutamate is transformed into γ‐aminobutyrate and that KorABDG plays a role in the GABA shunt. For Mycobacterium tuberculosis it has been shown that α‐ketoglutarate dehydrogenase defends the bacterium against glutamate anaplerosis and oxidative stress caused by reactive nitrogen species (Maksymiuk et al., 2015) indicating that the genes encoding enzyme might be induced during methoxydotrophic growth of A. fulgidus due to stress response. Furthermore, this enzyme seems to have a more important role during growth on MACs than growth on H2/CO2 or CO as genes encoding this enzyme are not upregulated under those conditions (Hocking et al., 2014, 2015) (see also Fig. 6) demonstrating that its upregulation might correlate with a stress response caused by methoxydotrophic growth. Also, the genes encoding the cytochrome bd ubiquinol oxidase subunits AF_2296 and AF_2297 are strongly upregulated under methoxydotrophic growth (Supporting Information Table S2) which might be due to an oxidative stress responds.
Lipid and amino acid metabolism
A. fulgidus possesses 57 genes encoding β‐oxidation enzymes indicating that the organism is able to degrade a variety of hydrocarbons and organic acids (Klenk et al., 1997). In this study, we observed that a vast number of genes encoding for proteins involved in lipid metabolism, amino acid uptake, and acetate/fatty acid activation are upregulated in A. fulgidus cells grown on methoxylated aromatics versus lactate. In a transcriptomic study with A. fulgidus cells grown on H2/CO2 versus lactate, similar observations were made (Hocking et al., 2014; see also Fig. 6). The upregulation of those genes might enable the organism to co‐assimilate lipids, amino acids and other organic compounds, resulting in mixotrophic growth. Furthermore, some of the upregulated genes (AF_0333, AF_0885, AF_1027) might encode for enzymes that are part of a 3‐hydroxypropionate/4‐hydroxybutyrate (3HP/4HB) cycle (Hocking et al., 2014) identified in Metallosphaera sedula (Berg et al., 2007) and might represent a secondary carbon fixation pathway in A. fulgidus. However, in a study with Archaeoglobus lithotrophicus, no enzyme activities associated with the dicarboxylate/hydroxybutyrate or the hydroxypropionate/hydroxybutyrate cycles were detected (Estelmann et al., 2011).
Conclusion
In summary, we describe the first non‐methanogenic methoxydotrophic archaeon. Similar to the so far first and only described methoxydotrophic archaeon M. shengliensis, which uses methoxylated aromatics for methane production, a bacterial‐like demethoxylation system is used in A. fulgidus. In contrast to M. shengliensis, A. fulgidus converts the methoxy group primarily to CO2 and not to CH4 by using the reductive acetyl‐CoA pathway, hereby representing a novel type of archaeal metabolism. We showed that A. fulgidus can grow on a variety of methoxylated aromatic compounds with a comparable growth rate and growth yield as on lactate and we demonstrated that those compounds improve the growth when lactate is present as a substrate. Other archaea that thrive in hydrothermal deep‐sea sediments such as Bathyarchaeota, Lokiarchaeota, Verstraetearchaeota, Korarchaeota, Helarchaeota and Nezhaarchaeota also appear to have the genetic potential for methoxydotrophic growth. As methoxylated aromatic compounds are quite abundant on earth, especially in the subsurface, we hypothesize that methoxylated aromatic compounds serve as a growth substrate, either on their own or as co‐substrate, for more microorganisms than previously assumed and that methoxydotrophic growth might play an underestimated role in the global carbon cycle.
Experimental procedures
Cultivation of Archaeoglobus fulgidus
Archaeoglobus fulgidus VC‐16 (DSM 4304) was cultivated in anoxic, carbonate buffered medium (50 ml medium in 120 ml glass bottles) under an atmosphere of N2:CO2 80:20 (1 atm), at pH 6.8, similar as described by Hocking et al. (2014). The composition of the media was as follows: 0.32 g/l KCl, 4.0 g/l MgCl2 × 6 H2O, 0.25 g/l NH4Cl, 0.14 g/l CaCl2 × 2 H2O, 0.11 g/l K2HPO4, 0.2 g/l KH2PO4, 18.0 g/l NaCl, 0.3 g/l yeast extract, 2.5 g/l NaHCO3, a 100 × trace element solution (1.5 g/l nitrilotriacetic acid, 3 g/l MgSO4 × 7 H2O, 0.45 g/l MnSO4 × 2 H2O, 1 g/l NaCl, 0.1 g/l FeSO4 × 7 H2O, 0.18 g/l CoSO4 × 6 H2O, 0.1 g/l CaCl2 × 2 H2O, 0.18 g/l ZnSO4 × 7 H2O, 0.01 g/l CuSO4 × 5 H2O, 0.02 g/l KAI(SO4)2 × 12 H2O, 0.01 g/l H3BO3, 0.01 g/l Na2WO4 × 2 H2O, 0.01 g/l Na2MoO4 × 2 H2O, 0.025 g/l NiCl2 × 6 H2O, 0.01 g/l Na2SeO3) and 0.5 ml/l 0.2% resazurin. Before inoculating, sterile anoxic solutions of cysteine (0.5 mM), Na2S (0.5 mM), MgSO4 (16 mM), L‐lactate (35 mM) or 2‐methoxyphenol (2‐MP; 7.5 to 30 mM) were added to the autoclaved medium. Cultivation was performed at 80°C. Next to 2‐methoxyphenol also 7.5 mM 2‐methoxybenzoate, 3,4,5‐trimethoxybenzoate, 2,6‐dimethoxyphenol, 3,5‐dimethoxy‐4‐hydroxycinnamic acid, 4‐methoxyphenylacetic acid, methoxyhydroquinone, methyl 2‐methoxybenzoate and 15 mM methanol were tested as growth substrate. Growth could only be observed with certainty for 2‐methoxyphenol, 2,6‐dimethoxyphenol, methoxyhydroquinone and 2‐methoxybenzoate (Supporting Information Fig. S2). Furthermore, it was tested if A. fulgidus can grow without CO2 with lactate or 2‐MP as substrate. Medium without CO2 was prepared as described above but leaving out NaHCO3, adding 4.6 g/l piperazine‐N,N′‐bis(2‐ethanesulfonic acid) (PIPES), adjusting the pH to 6.9 and gassing with N2 instead of N2‐CO2.
Following growth and substrate consumption of A. fulgidus
Growth was followed by measuring the optical density at 600 nm (OD600) with a Cary 60 UV–Vis spectrophotometer (Agilent Technologies, USA) at distinct time points. To prevent interference of the absorbance of resazurin, which is present in the medium, sodium dithionite was added to the cuvettes before measuring OD600. For all growth conditions, triplicates were used and those triplicates were also used for analysis of substrate consumption/product formation which is described in the following section.
Determination of CO2 and H2
The CO2 and H2 concentration in the headspace was measured by gas chromatography with a gas chromatograph (Hewlett Packard 5890a, Agilent Technologies, Santa Clara, CA, USA) equipped with a Porapak Q 100/120 mesh and a thermal conductivity detector (TCD) using N2 as carrier gas. Each measurement was performed by injection of 50 μl headspace gas with a gas‐tight syringe. CO2 concentrations were corrected for the volume removed from the bottle due to OD600 measurements. No H2 production or consumption could be observed.
Determination of methane
To analyse if the cultures produce methane, 50 μl headspace volume were injected with a gas‐tight glass syringe (Hamilton, Reno, NE) into an Agilent 6890 series gas chromatograph coupled to a Agilent 5975C mass spectrometer with triple‐Axis detector (GC–MS) (Agilent, Santa Clara, CA) equipped with a Porapak Q column heated at 80°C. No methane production could be observed.
Determination of 2‐methoxyphenol and 2‐hydroxyphenol
To measure concentrations of 2‐methoxyphenol and 2‐hydroxyphenol by HPLC an Agilent 1100 HPLC system equipped with a diode array detector (detecting wavelength 260 nm) and a Merck C‐18e column (250 mm × 4.6 mm, 5 μm particle size) was used. The flow rate was 0.75 ml/min and a linear gradient was applied: 75% trifluoroacetic acid (TFA) (0.1% in water), 25% acetonitrile to 50% TFA (0.1% in water), 50% acetonitrile in 15 min. A solution of 2‐methoxyphenol and 2‐hydroxyphenol in water (0.1 mg/ml) was used as standard. Twenty microlitres of sample was used for injection.
Acetate determination
For the determination of acetate concentrations, a slightly modified method of Kage et al. (2004) was used. Two hundred microlitres of pentafluorobenzylbromide (PFBBr) solution (100 mM in acetone) and 40 μl phosphate buffer (0.5 M, pH 6.8) were added to 40 μl sample, mixed and incubated for 1 h at 60°C in an eppendorf tube with safety cap. After cooling down to room temperature, 400 μl hexane (containing 50 μg/ml methylstearate as internal standard) was added and vortexed for 1 min. Thereafter, the sample was centrifuged at 15 000 × g for 1 min. From the hexane layer (top), 100 μl was transferred to a GC vial. One microlitre of the sample was used for analysis by GCMS. To determine precise acetate concentrations, a calibration curve was made. A stock solution of 100 mM sodium acetate in water was prepared and diluted in a range between 1 and 40 mM acetate. Of each of these dilutions, 40 μl was used for preparation of a calibration curve. Samples were derivatized as described above for the samples. For analysis of PFBBr derivatives, an Agilent 7890A gas chromatograph equipped with an autosampler (7693A) and with a JMS‐T100GCv JEOL (JEOL) mass spectrometer was used. The gas chromatograph contains a HP‐5MS column 30 m × 0.25 mm × 0.25 μm. The following conditions were applied for GC‐TOF‐MS acetate analysis: The oven temperature was set to 50°C for 2 min, followed by a temperature gradient of 20°C/min to 300°C for 1 min. The split ratio was 1:10 and the detector voltage 2000 V. Peaks were detected by total ion current (TIC) and a selected trace with mass range m/z 239.9–240.1 used for detection and quantification of the acetate‐PFB derivative. Data were evaluated with Xcalibur (version 2.1, Thermo Scientific) after conversion/export to net CDF by MassCenter JEOL.
Sulfide determination
Ten microlitres of samples were used immediately for sulfide determination with the methylene blue method by using a sulfide reagent set (HACH, USA; method 8131) according to the manufacturer's instructions. Samples were diluted 100‐fold. For calculation of the sulfide concentration the Henrys law constant of 0.001 (mol s2 m−2 kg−1) was used (Sander, 2015). A factor of 2.9 was calculated with the help of this constant and by adjusting for the 80°C incubation temperature to calculate the sulfide concentration in the headspace with help of the following equation KRT = c(liquid)/c(gasphase), where K is Henrys law constant, R the gas constant and K the temperature.
Sulfate determination
Twenty microlitres of samples were used to measure sulfate concentrations with a Sulfate Assay kit (MAK132, Sigma‐Aldrich) according to the manufacturer's instructions. Samples were diluted 10‐fold.
Formate determination
Five microlitres of samples were used for measuring formate with a Formate Assay kit (MAK059, Sigma‐Aldrich) according to the manufacturer's instructions. Samples were diluted 10‐fold.
Lactate determination
Lactate was measured after the method described by Borshchevskaya et al. (2016). Twenty‐five microlitres of sample was mixed with 1 ml 0.2% iron (III) chloride hexahydrate. Using 10 g/l acetate and formate instead of sample leads to Abs390 nm value similar to those of the medium background, showing that those compounds do not interfere with the assay. With help of this assay, it was observed that about 23 mM (1.2 mmol per bottle) lactate out of 42 mM (2.1 mmol per bottle) lactate were consumed during the growth of A. fulgidus.
Resting cell experiment
A. fulgidus cells grown in 50 ml medium (see above) with 12 mM 2‐MP or 35 mM lactate as substrate were harvested anaerobically in the exponential phase and washed with stabilization buffer (2 mM KH2PO4/K2HPO4, 2 mM MgSO4, 400 mM NaCl, 200 mM sucrose, pH 6.8, gassed with N2). The cell pellets were resuspended in 40 ml stabilization buffer (see above) and transferred into 120 ml anaerobic glass bottles. The cultures were incubated for 30 min at 80°C. Afterwards, 6 mM 2‐MP or 17 mM lactate and 8 mM MgSO4 were added and the cultures were incubated for 5 h at 80°C. The CO2 gas produced by the cultures was analysed every hour by injecting 50 μl headspace volume with a gas‐tight glass syringe (Hamilton, Reno, NE) into an Agilent 6890 series gas chromatograph coupled to a mass spectrometer (GC–MS) (Agilent, Santa Clara, CA) equipped with a Porapak Q column heated at 80°C. For calculating the CO2 in the culture headspace, a calibration curve was generated by injecting different volumes of calibration gas (Linde Gas Benelux) that contained 1% CO2 and 1% CH4 into the GC–MS. The CO2 values (in %) were corrected for the CO2 in the medium in form of HCO3 − by measuring the headspace CO2 in 40 ml buffer before and after acidification with HCl. The experiment was performed in triplicate. Values for CO2 production were adjusted to the protein content of each sample. For the protein determination, 500 μl of cells were sampled at t 0 and boiled for 15 min at 110°C. Afterwards, 2 ml −20°C cold acetone was added and the samples incubated at −20°C for 1 h. The samples were centrifuged at 20 000 × g for 15 min, the supernatant removed and the pellets dried for 30 min at room temperature. After resuspending the pellets in 50 μl H2O, the protein content was measured by the Bradford Protein Assay (5000006, Bio‐Rad) according to the manufacturer's instructions.
Metabolite analysis of A. fulgidus cells grown under different conditions
A. fulgidus was grown in triplicates in 50 ml medium (see above) with either 12 mM 2‐MP (Mp), 35 mM lactate (Lac) or 12 mM 2‐MP plus 35 mM lactate (M + L). As a control, a culture without substrate was used (no change in OD600). Cells were harvested aerobically in the exponential phase (OD600 MP: 0.06, Lac: 0.13, M + L: 0.15) at 20 000 × g and 4°C for 15 min. Pellets were washed with 1 ml cold PBS and centrifuged for 1 min at 12 000 × g. The remaining pellet was lysed using 500 μl of H2O:methanol:acetonitrile(40:40:20, V:V:V). After centrifugation for 1 min at 12 000 × g, the supernatant was transferred into a fresh tube and stored at −20°C until metabolite analysis. Aqueous normal phase metabolomics was performed on 2 μl sample using a 1290 Infinity II LC system coupled to a 6546 Q‐ToF MS (Agilent Technologies) as previously described (Jansen et al., 2020). In brief, samples were injected onto a Diamond Hydride Type C column (Cogent) and separated using a gradient of water and acetonitrile with 0.2% formic acid. Detection was performed in the negative ionization mode from m/z 50–1200. For the detection of glutamate, samples were diluted 20‐fold in acetonitrile:methanol:water (40:40:20, V:V:V) to overcome sodium‐related interferences. Metabolites were identified based on MS fragmentation and quantified using Qualitative Analysis 10.0 (Agilent Technologies). Metabolite signals were normalized for OD600.
RNA isolation from A. fulgidus cells
Cultures for RNA extractions/transcriptomics were grown in 250 ml medium with either 10 mM 2‐MP or 35 mM lactate. Cells were harvested anaerobically in the exponential phase at 10 000 × g, 20 min and 4°C. The pellet was frozen in liquid nitrogen and stored at −80°C until RNA isolation. RNA isolation was performed with the RiboPure‐Bacteria Kit (Thermo Fischer Scientific) according to the manufacturer's instructions. Quantity and quality of RNA from lactate and 2‐MP grown cells (in triplicates) were checked with an Agilent 2100 Bioanalyzer and the RNA Integrity Number was between 7.2 and 8.2.
Transcriptome sequencing and analyses
For library preparation, the TruSeq® Stranded mRNA Library Prep protocol (Illumina, San Diego, CA, USA) was used according to the manufacturer's instructions. Total RNA was used for library preparation. The library concentration measured with a Qubit fluorometer and the average fragment size obtained with the Agilent 2100 Bioanalyzer were used to calculate the correct dilution factor required for normalization of the library. After dilution to 4 nM and denaturation using the Denature and Dilute Libraries Guide (Illumina, San Diego, CA), the library was sequenced using an Illumina MiSeq machine (San Diego, CA) to generate 150 bp single‐end reads.
To analyse transcriptomic data, raw reads from the MiSeq platform were initially trimmed based on a quality limit of 0.02 and minimal length of 50 bp using the CLC Genomics Workbench 12 (Qiagen, Aarhus, Denmark). Next, RNA reads were mapped to the draft genome of A. fulgidus DSM 4304 AE000782.1 (insertion cost, 3; deletion cost, 3; length fraction, 0.8; similarity fraction, 0.95). Further analysis was conducted with RStudio using R package ‘Deseq2’ (Love et al., 2014). The gene expression values were expressed as RPKM (Reads per kilo base of exon model per million mapped reads) and log2fold change values. For the generation of the heat map, RPKM values were imported into RStudio v. 1.2.5033 (using R v. 4.0.3), and the packages RColorBrewer v. 1.1.2, gplots v. 3.1.1 and vegan v. 2.5.6 were used, with the function ‘heatmap.2’.
Protein sequence analyses
We identified relevant archaeal sequences via BlastP using A. fulgidus amino acid sequences of MtoABCD, blasting them against the non‐redundant blast database and we selected sequences with at least 35% amino acid identity coming from one same genome (Candidatus Bathyarchaeota archaeon SpSt‐709: DTEF01, Candidatus Verstraetearchaeota archaeon SJ3.Bin21: JAAOZJ01, Candidatus Nezhaarchaeota archaeon WYZ‐LMO8: QNVF01, Candidatus Lokiarchaeota archaeon Hel_238_bin90: JABXKC01, Candidatus Helarchaeota archaeon CR_Bin_143: JABXJV01, Candidatus Korarchaeota archaeon B41_G2: QMVX01). Improved protein annotation was obtained via NCBI blast analysis (https://blast.ncbi.nlm.nih.gov/Blast.cgi?PAGE=Proteins). The phylogenetic tree was generated via multiple alignment of amino acid sequences retrieved from NCBI with MUSCLE (Edgar, 2004) v. 3.8.31 (sequence accession numbers are provided in the tree). Alignment columns were stripped with trimAI (Capella‐Gutiérrez et al., 2009) v. 1.4.rev22 using the ‐gappyout option, and the tree was built with FastTree (Price et al., 2010) v.2.1.10 using the Jones‐Taylor‐Thorton maximum likelihood model. The tree was visualized with iToL (Letunic and Bork, 2019) v.4 and edited on Adobe Illustrator CC 2018 (San Jose, California, USA).
Supporting information
Acknowledgements
CUW, JMK and MSMJ were supported by the Nederlandse Organisatie voor Wetenschappelijk Onderzoek through the Soehngen Institute of Anaerobic Microbiology (SIAM) Gravitation Grant 024.002.002. MSMJ was further supported by the Netherlands Earth System Science Center Gravitation Grant 024.002.001 and the European Research Council Advanced Grant Ecology of Anaerobic Methane Oxidizing Microbes 339880. JMK was supported by the Deutsche Forschungs Gesellschafts (DFG) Grant KU 3768/1‐1. We thank Theo van Alen and Geert Cremers for technical assistance. We further thank Ines A.C. Pereira and Sofia Venceslau for sending us A. fulgidus strain VC‐16, Garrett Smith for helping with the transcriptomic analysis and William Hocking for providing the raw data of the Hocking et al. (2014) and (2015) studies.
Data availability
The transcriptomics data have been deposited at the Sequence Read Archive (SRA) from NCBI with BioProject accession number PRJNA695423 under the following link: https://www.ncbi.nlm.nih.gov/sra/PRJNA695423.
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Associated Data
This section collects any data citations, data availability statements, or supplementary materials included in this article.
Supplementary Materials
Data Availability Statement
The transcriptomics data have been deposited at the Sequence Read Archive (SRA) from NCBI with BioProject accession number PRJNA695423 under the following link: https://www.ncbi.nlm.nih.gov/sra/PRJNA695423.