Genomic and transcriptomic analysis of lignocellulolytic capacity.
First, we subjected two
Termitomyces species, excavated in South Africa in 2011 and 2015, to whole-genome sequencing using Illumina sequencing technology (LGC Genomics [Berlin, Germany]) and RNA sequencing using the BGISeq-500 platform (BGI, Hong Kong). Annotated genomes of both species were obtained using AUGUSTUS 3.3.3 after RNA-seq data were mapped to the genomes and used for algorithm training. The resulting draft genome of
Termitomyces sp. strain T153 (
Macrotermes natalensis) had an estimated size of 84.1 Mb (scaffold
N50 = 23.88 kb), with more than 13,000 genes (GenBank accession no.
JACKQL000000000). Similarly, the draft genome of
Termitomyces sp. strain T112 (
Macrotermes natalensis) had an estimated size of 79.8 Mb (scaffold
N50 = 33.34 kb) and also >13,000 genes (accession no.
JACKQM000000000). For further analysis, we also reannotated seven
Termitomyces genomes deposited in GenBank, including our previously reported
Termitomyces sp. strain J132 (alias P5) from
Macrotermes natalensis (
3), using the same settings in AUGUSTUS 3.3.3 (Tables S2 and S3 at
https://doi.org/10.5281/zenodo.4431413). To gain insights into the functional capacity for biomass degradation, we first identified CAZyme families within each genome using a local installation of the dbCAN2 server (
25–27).
Comparison of all nine
Termitomyces genomes revealed that all species had relatively similar predicted proteomes with comparable numbers of polysaccharide-degrading enzymes, such as exo-cellobiohydrolases, endoglucanases assigned to different glycoside hydrolase (GH) families, and lytic polysaccharide monooxygenase (LPMOs), but no particular enrichment or reduction of CAZy families compared to those of other basidiomycete reference genomes was found (
Fig. 2; see Fig. S1 and S2 at
https://doi.org/10.5281/zenodo.4431413) (
28).
We then specifically searched
Termitomyces genomes for the presence/absence of gene sequences encoding highly oxidizing enzymes that could contribute to the depolymerization and catabolic degradation of lignin (
Fig. 2; see Table S4 at
https://doi.org/10.5281/zenodo.4431413) (
18). It is worth noting that
Termitomyces genomes contained, on average, 16 gene sequences encoding laccases (AA1) (
29–32), oxidases with low redox potential that use diphenols and related substances as electron donors and oxygen as the acceptor, thereby creating reactive C and O-based radical species in the process. In addition, we identified one putative MnP (AA2) per genome, an enzyme that generates highly reactive Mn
3+ species that, once chelated, are able to diffuse through the dense network of lignocellulose, causing oxidation degradation due to their higher redox potential (
23). Furthermore, a subset of gene sequences encoding alcohol oxidases and dehydrogenases (AA3 and AA5) are known to catalyze the oxidation of (aryl)-alcohols or carbohydrates with the concomitant formation of hydroquinones and/or H
2O
2 (
33,
34). Unlike in previous studies (
1), we also identified sequences encoding a DyP and an UPO (Tables S5 and S6 at
https://doi.org/10.5281/zenodo.4431413), both of which are known for their versatile substrate spectrum. However, homologous sequences to other class II peroxidases (PODs), such as LiPs, were not detectable. Along these lines, iron reductase domains (AA8, EC 1.16.1) and putative benzoquinone reductases (AA6, EC 1.6.5.6) that are key to maintaining efficient Fenton chemistry-based redox cycles by reductive Fe
2+ sequestration and regeneration of organic benzoquinone-based redox shuttles were identified.
Subsequently, the expression levels of candidate genes related to lignin depolymerization were analyzed in RNA-seq data obtained from three regions in the fungus comb (
Fig. 3) (
7): fresh comb (within which most plant biomass decomposition is likely to occur), old comb (where decomposition might still occur but to a lesser extent), and nodules as (which feed young workers and serve for fungal spore and enzyme transport) (
Fig. 3; Table S27 at
https://doi.org/10.5281/zenodo.4431413).
Here, we found differentiating transcription levels of genes encoding oxidative enzymes (such as laccases, a MnP, and a UPO) and enzymes of the CAZy families AA3 and AA5, as well as enzymes that protect against reactive intermediates (e.g., benzoquinone reductase [EC 1.6.5.7], superoxide dismutase [EC 1.15.1.1], glutathione peroxidase [EC1.11.1.9], and peroxiredoxin [EC 1.11.1.15]) across all three data sets. The combined genetic and transcriptomic survey revealed that
Termitomyces has the capacity to produce lignocellulolytic enzymes and may even be able to induce and catalyze Fenton chemistry (
35).
Fenton chemistry of Termitomyces.
Fenton chemistry involves the reaction between Fe
2+ and H
2O
2, yielding Fe
3+ and a highly reactive hydroxyl radical (
•OH), a powerful oxidant (E
0 = 2.8 V versus that of a normal hydrogen electrode) that is able to unselectively oxidize hydrocarbons and nonphenolic aromatic units within lignocellulose-rich material. Brown-rot fungi are known to make use of Fenton chemistry to depolymerize lignocellulose biomass (
36) and modulate the redox potential of Fe
2+/3+ species by secretion of dicarboxylic acids that act as chelators to form diffusible Fe complexes and as proton donors for catalytic degradation processes (
37). Additionally, redox-active fungal quinones (Q) and hydroxyquinones (H
2Q), such as 2,5-dimethoxy-1,4-benzoquinone (2,5-DMQ), 2,5-dimethoxy-1,4-hydroquinone (2,5-DMH
2Q), and its regioisomer 4,5-dimethoxy-1,2-benzendiol (4,5-DMH
2Q), have been discussed to serve as redox shuttles (3 H
2Q + 2 O
2 → 3 Q + 2 H
2O + 2 HO
•) in the Fenton chemistry of rotting fungi (e.g.,
Serpula lacrymans, the
Gloeophyllales, and the
Polyporales) (
38–40), as they have the ability to switch between oxidation states via one-electron transfer reactions that allow for the concomitant formation of Fe
2+ from Fe
3+ and hydroxyl radicals (HO
•) from H
2O
2 and O
2 (see
Fig. 5 and
6).
Thus, we evaluated whether
Termitomyces employs any of those measures to enable lignin depolymerization by using
Termitomyces sp. T153 and P5 as model strains. First, we employed a standardized colorimetric ferrozine assay to determine if extracellular Fe
3+ is reduced to Fe
2+ within the surrounding mycelium, a prerequisite to initiate Fenton chemistry (
41,
42). As depicted in
Fig. 4A, topical application of a ferrozine solution caused a clear color change within minutes, which was indicative of the immediate reduction of Fe
3+ to Fe
2+. Next, we determined the pH range within the fungal mycelium, as enzyme activities, the redox potential of H
2O
2, and metal complexes are strongly pH dependent (
35). We found indications that
Termitomyces acidifies the surrounding medium (
Fig. 4D), which would benefit enzyme activities of lignin-degrading enzymes with a pH optimum of 4.5 to 5.0 (
14,
21). As the Fenton reaction also requires H
2O
2, we tested if
Termitomyces generates sufficient extracellular H
2O
2 to initiate the reaction. Based on an H
2O
2-dependent colorimetric assay, we found that
Termitomyces generates approximately 4 to 6 μg extracellular H
2O
2 per gram mycelium during growth on solid support (mycelium age, 7 to 21 days) (Tables S18 to S20 at
https://doi.org/10.5281/zenodo.4431413).
In a next step, we evaluated if
Termitomyces produces redox-active H
2Q/Q using gas chromatography coupled with mass spectrometry (GC-MS). Although the formation of previously reported 2,5-DM(H
2)Q was not observed, we were intrigued to detect 2-methoxy-1,4-benzoquinone (2-MQ), its reduced H
2Q named 2-methoxy-1,4-dihydroxybenzene (2-MH
2Q), and the fully methylated derivative 1,2,4-trimethoxybenzene (compound
5), as well as other structurally related (di)methoxylated hydroxybenzenes (e.g., compounds
1, 3, and
12) (
Fig. 5). Additionally, we verified the identities of the newly detected quinone derivatives 2-MQ and 2-MH
2Q by synthesis and comparison of GC-MS retention times (Fig. S20 and S21 and Tables S16, S17, and S24 at
https://doi.org/10.5281/zenodo.4431413).
To evaluate the ability of H
2Qs to reduce Fe
3+ to Fe
2+, we employed the established ferrozine-based Fe
3+ reduction assay (
43). Overall, 2,6-DMH
2Q (compound
18), a regioisomer of 2,5-DMH
2Q, was the most reactive derivative that was able to reduce Fe
3+ to Fe
2+ within seconds and was therefore used as positive control in further experiments (
Fig. 6). In comparison, 2-MH
2Q (compound
19) showed a reduced reactivity, which is likely a reflection of the decreasing electron density of the aromatic system due to the lack of one additional electron-donating –OCH
3 group. Other tested (methoxylated) hydroxybenzenes showed a reduced reactivity compared to those of compounds
18 and
19. Subsequently, we expanded our studies to combinations of redox-active derivatives and were able to observe in most cases the superposition of redox activities but no indications of synergistic activity (Fig. S9 and Table S21 at
https://doi.org/10.5281/zenodo.4431413).
As Fenton chemistry produces highly reactive hydroxyl radicals (
•OH), we then confirmed the presence of these short-lived radicals in our H
2Q-mediated Fenton reactions using a fluorometric assay based on the reaction with terephthalic acid (TPA). As in literature reports for 2,6-DMH
2Q (compound
18) (
37–40), the newly identified and structurally related H
2Q compound
19 catalyzed the formation of
•OH in the presence of H
2O
2 and Fe
3+ within seconds. In contrast, derivatives such as 1,2-dihydroxybenzene (compound
10) and syringic acid (compound
13) caused the formation of hydroxyl radicals with lower initial reactivities, but they formed over a period of more than 90 min (Fig. S5 at
https://doi.org/10.5281/zenodo.4431413). Having verified that
Termitomyces produces reactive H
2Qs that are able to induce the formation of Fenton reagents (Fe
2+, H
2O
2, and
•OH), we then elaborated on the influence of fungus-derived dicarboxylic acids (oxalic acid, tartaric acid, malic acid, fumaric acid, and succinic acid) (
44–46) on the Fenton reaction (
Fig. 7). While at low concentrations of oxalic acid (0.1 mM) most H
2Qs were still able to reduce the formed Fe
3+ complexes, increasing concentrations caused the formation of stable Fe complexes with altered redox potentials, such that only the most reactive, 2,6-DMH
2Q (compound
18), was able to reduce Fe
3+ to Fe
2+ (Fig. S10 to S12 at
https://doi.org/10.5281/zenodo.4431413) (
46). At 10 mM oxalic acid, a significant amount of autoxidation-related Fe
3+ reduction was observed. A similar reactivity trend, albeit with a stronger autoxidation effect, was observed when tartaric acid was investigated as a chelating agent (
47). In contrast, the presence of malic, fumaric, or succinic acid only moderately altered the redox potential of the Fe-complexes, and only low rates of autoxidation were observed (Fig. S14 to S16 at
https://doi.org/10.5281/zenodo.4431413).
While laboratory culture conditions generally supply sufficient Fe concentrations for growth, we questioned whether or not the natural fungal comb environment provides the necessary metal ions for Fenton chemistry (
48). To answer this question, we analyzed the element composition of fungus comb, gut fluids of termite workers, and soil samples derived from within and outside termite colonies from different locations using inductively coupled plasma atomic emission spectrometry (ICP-AES) (
49). All tested samples contained Al, Fe, and Ti as some of the most abundant main elements, in addition to significant amounts of Mn. However, amounts of elements important for growth (C, H, P, K, Ca, Mg) were low in all soil samples, with a particularly strong depletion of phosphorus, but potassium was enriched compared to levels in comb and gut samples (Fig. S22 to S29 and Tables S15, S25, and S26 at
https://doi.org/10.5281/zenodo.4431413). Sequential ion extraction of soil samples was performed to analyze the soluble metal ion content, and only low concentrations of most metal ions were detectable (
50,
51). Although these findings indicate that fungus comb and the gut environment accommodate large amounts of insoluble Fe/Al oxides, the nano- and microscopic surface areas of these minerals may act as the necessary catalytic centers for Fenton-like redox chemistry (
52).
Enzyme activity tests catalyzing the degradation of model lignin compounds.
We then questioned if enzymatic degradation of lignin or lignin-like model substances by
Termitomyces is measurable using colorimetric assays or MS-based analytical tools (
53). For a first test, we supplemented the culture medium of
Termitomyces sp. T153 with the pigment-based model substance Azure B (
54), previously used to measure the redox activity of LPs due to its stability toward oxidative activities of MnPs. Over a time course of seven days, we were able to monitor the decolorization of Azure B by
Termitomyces, an effect which became more pronounced with the increasing biomass and age of the fungus culture (Fig. S16 at
https://doi.org/10.5281/zenodo.4431413). To evaluate if the degrading activity was due to the activity of secreted oxidative enzymes and/or H
2Q-mediated Fenton-based chemistry, we tested both effectors separately and in combination. While quantification of enzymatic effects was hampered by technical challenges due to intrinsic light absorption of enzymes concentrates, H
2Q-mediated Fenton chemistry clearly induced the degradation of Azure B within 5 to 10 min in a comparison with the control (Fenton reagents without H
2Qs) (Fig. S16 at
https://doi.org/10.5281/zenodo.4431413) (
55). We then evaluated whether or not laccase activity was detectable within the secretome using a syringaldazine-based assay and compared the activity to the reactivity of a commercial laccase from
Trametes versicolor (
56). However, only residual laccase activity was detectable compared to the activity in the positive control and thus was unlikely accountable for the degradation of Azure B.
Lastly, we evaluated if
Termitomyces exhibits MnP enzymatic activity, which is marked by the oxidation of Mn
2+ to Mn
3+ and the release of the highly reactive oxidant as a carboxylic acid chelate, using a previously reported leukoberbelin blue test (
57). As shown in
Fig. 8, leukoberbelin-containing
Termitomyces cultures and cell-free culture supernatant resulted in the formation of the blue leukoberbelin complex within minutes, which indicated the formation of Mn
3+/4+ species. When
Termitomyces was grown on potato dextrose agar (PDA) plates containing both elevated Mn
2+ concentrations (200 to 500 μM) and indicator dye, the formation of blue leukoberbelin-Mn
3+/4+ complexes was detectable within a few days, and longer incubation times resulted in macroscopic MnO
x precipitates forming around fungal hyphae within 10 to 17 days (
Fig. 4C). We further confirmed the expression of the gene encoding the putative MnP by reverse transcription-PCR (RT-PCR) (Fig. S18 and S19 at
https://doi.org/10.5281/zenodo.4431413).