Experimental recreation of the evolution of lignin-degrading enzymes from the Jurassic to date
© The Author(s) 2017
Received: 22 November 2016
Accepted: 28 February 2017
Published: 16 March 2017
Floudas et al. (Science 336: 1715) established that lignin-degrading fungi appeared at the end of Carboniferous period associated with the production of the first ligninolytic peroxidases. Here, the subsequent evolution of these enzymes in Polyporales, where most wood-rotting fungi are included, is experimentally recreated using genomic information.
With this purpose, we analyzed the evolutionary pathway leading to the most efficient lignin-degrading peroxidases characterizing Polyporales species. After sequence reconstruction from 113 genes of ten sequenced genomes, the main enzyme intermediates were resurrected and characterized. Biochemical changes were analyzed together with predicted sequences and structures, to understand how these enzymes acquired the ability to degrade lignin and how this ability changed with time. The most probable first peroxidase in Polyporales would be a manganese peroxidase (Mn3+ oxidizing phenolic lignin) that did not change substantially until the appearance of an exposed tryptophan (oxidizing nonphenolic lignin) originating an ancestral versatile peroxidase. Later, a quick evolution, with loss of the Mn2+-binding site, generated the first lignin peroxidase that evolved to the extant form by improving the catalytic efficiency. Increased stability at acidic pH, which strongly increases the oxidizing power of these enzymes, was observed paralleling the appearance of the exposed catalytic tryptophan.
We show how the change in peroxidase catalytic activities meant an evolutionary exploration for more efficient ways of lignin degradation by fungi, a key step for carbon recycling in land ecosystems. The study provides ancestral enzymes with a potential biotechnological interest for the sustainable production of fuels and chemicals in a biomass-based economy.
KeywordsFungal genomes Ancestral sequence reconstruction Fungal evolution Lignin biodegradation resurrected enzymes Ligninolytic peroxidases Catalytic properties pH stability
The large diversity of living organisms that we observe today is associated to the evolution of proteins, making the analysis of how proteins change with time a central issue in molecular evolution. However, the study of ancestral proteins has an important difficulty: they are extinct. Therefore, the use of the tools provided by bioinformatics is mandatory . To this point, ancestral sequence reconstruction can give us hints about ancient protein functions, and resurrection of the extinct proteins in the laboratory, using ad hoc expression hosts, will allow to directly analyze their properties and confirm evolutionary hypotheses. During the past years, several examples have shown the power of this technique, from resurrection of the most ancient proteins in the Precambrian [2–4] to the explanation of how enzymes evolved and acquired the specific mechanisms and functions that they have today [5–8].
Resurrected proteins are of interest not only because of the essential information about evolution that they can provide, but also due to the biotechnological potential that they have . Ancestral proteins often have higher stability  and, likely, new activities , which can make of them interesting biocatalysts. Also, if we identify the elements that confer this stability or new activity we can improve extant enzymes by rational design. Or even more, the famous James Gould  sentence “replaying the tape of life” will no longer be a metaphor if we evolve the ancient proteins in the laboratory [13, 14].
A central problem of white biotechnology for establishing a sustainable bioeconomy in the twenty-first century is processing recalcitrant lignin in vascular plant feedstocks . Biological decay of lignin is essential for carbon recycling in nature, and lignin removal often also represents a key step for the sustainable production of fuels and chemicals in lignocellulose biorefineries . Oxidation of the predominantly nonphenolic lignin polymer is a unique ability of extracellular enzymes produced by white-rot basidiomycetes . These fungi secrete three families of ligninolytic peroxidases: (i) Lignin peroxidases (LiPs), which are able to oxidize nonphenolic lignin model compounds ; (ii) Manganese peroxidases (MnPs), which oxidize Mn2+ to Mn3+ whose chelates act as diffusing oxidizers of phenolic lignin ; and (iii) Versatile peroxidases (VPs), which combine the catalytic activities (and oxidation sites) of LiPs, MnPs, and plant peroxidases acting on phenols and some dyes [20, 21]. Often white-rot basidiomycetes also produce generic peroxidases (GPs) with catalytic properties similar to the plant peroxidases . These four peroxidase types, which constitute the class II of the peroxidase–catalase superfamily , are well characterized today and they differ in the substrate oxidation sites they have .
In the last years, the evolution of lignin-degrading organisms and enzymes has been investigated using genomic information. Molecular clock analyses and reconstruction of ancestral states of catalytic sites showed that the origin of lignin biodegradation occurred in the late Carboniferous with the appearance of the first ligninolytic peroxidase in the common ancestor of Agaricomycetes (Polyporales included) [25, 26]. This event provided to the first white-rot fungi the ability to attack the lignocellulosic biomass of vascular plants, enabling carbon recycling in land ecosystems. In the present work we target, by complete sequence reconstruction, the evolution that led to the highly specialized LiP of Phanerochaete chrysosporium (isoenzyme H8) [18, 27], the first sequenced basidiomycete as a model ligninolytic organism . With this aim, we resurrected the most relevant enzymes of the evolutionary line from the common ancestor of class-II peroxidases in the order Polyporales, where most wood-rotting fungi are included , and studied their catalytic and stability properties with the aim of recreating in the laboratory the natural evolution of lignin-degrading enzymes, which contributed to land colonization by vascular plants .
Reconstruction of ancestral sequences from Polyporales genomes
The posterior probabilities for three of the most probable ancestral sequences (CaCD, AVP, and ALiP) are high (mean ≥ 0.95) while those of the first ancestor (CaPo) were lower (mean 0.82) (Additional file 1: Fig. S2). To check the possible functional variability of the four reconstructed nodes, a total of 5000 sequences (including the most probable ones) were obtained for each of them by Monte Carlo sampling  from the PAML results, and manually inspected for the presence/absence of the two substrate oxidation sites described below (Glu37/Glu41/Asp183 binding Mn2+, and Trp172 oxidizing nonphenolic lignin). For the three more recent nodes 100% of the sequences showed the following invariable oxidation site/s: Trp172 in ALiP, both Trp172 and Glu37/Glu41/Asp183 in AVP, and Glu37/Glu41/Asp183 in CaCD sequences. Therefore, only the most probable sequences were resurrected for each of them.
For node CaPo, all sequences lack Trp172 and have at least two of the above acidic residues, a situation associated to Mn2+ oxidation ability by normal or atypical MnPs (lacking one of these residues) [25, 31]. To verify the activity of the predicted atypical MnPs, the corresponding sequences were classified into two subsets (with either Asp37 or Arg183) that were submitted to a random sampling. In this way, the CaPo-bis and CaPo-tris alternative sequences (“near-ancestors”) were selected, which were resurrected together with the most probable CaPo ancestor with a typical Mn2+-oxidation site. Although the resulting sequences were not resurrected, parallel random samplings were also performed on the CaCD, AVP, and ALiP sets for in silico analysis, showing invariable catalytic sites (their sequences and posterior probability values are shown in Additional file 1: Figs. S1 and S2, respectively, together with those of the CaPo node).
In silico analysis of ancestral heme pocket and substrate oxidation sites
Molecular models of the selected ancestral proteins, together with multiple alignments, reveal that their 12 helices, two sites binding structural Ca2+ ions, and four disulfide bonds did not change during evolution, despite the differences in sequence (only 61–87% identity) between the ancestors and between them and the extant LiPH8 (see Fig. 2 legend). This comparison also reveals that most of the essential amino acids for LiPH8 function were already present at the first stages of evolution, including proximal His177 (near the heme iron), Asp239, and Phe194 at one side of heme, and distal His48, Arg44 (both contributing to H2O2 reaction in extant peroxidases), Asn85, and Phe47 at the opposite side. Hypothetical His177-Asp239 and Ser/Thr178-Asp202 H-bonds would control the position of the proximal histidine with respect to the heme iron (Additional file 1: Fig. S3). The proximal Ca2+ hypothetical ligands—Ser178 (CaPo and CaCD) or Thr178 (AVP and ALiP), Asp195, Thr197, Thr200 (CaPo, CaCD), or Leu200 (AVP and ALiP), and Asp202—show some differences with those in LiPH8 (Ser177, Asp194, Thr196, Ile199, and Asp201), while the distal Ca2+ ligands would be exactly the same. However, the above differences would not affect proximal Ca2+ binding since backbone carbonyls are involved at those positions where differences are predicted.
Kinetic properties of resurrected peroxidases
Kinetic parameters—K m (µM), k cat (s−1), and k cat /K m (s−1 mM−1)—for the oxidation of Mn2+, phenolic (DMP) and nonphenolic (VA) aromatics, and dyes (means and 95% confidence limits) by the resurrected enzymes and extant LiPH8 (a comparison of all catalytic efficiencies is shown in Fig. 4)
700 ± 48
275 ± 41
62 ± 10
185 ± 3
170 ± 6
106 ± 4
k cat /K m
260 ± 15
617 ± 80
1710 ± 240
DMPb (low efficiency)
32,900 ± 2700
66,800 ± 3800
32,500 ± 12,100
221 ± 9
109 ± 4
31 ± 5
k cat /K m
6.7 ± 0.3
1.6 ± 0.03
1.0 ± 0.2
DMP (high efficiency)
5.3 ± 1.1
34.0 ± 5.4
4.0 ± 0.07
4.5 ± 0.1
18.3 ± 0.7
6.9 ± 0.5
k cat /K m
837 ± 162
537 ± 55
600 ± 36
299 ± 104
773 ± 155
79.3 ± 18
7.1 ± 0.5
21.3 ± 1.0
16.2 ± 0.8
k cat /K m
24 ± 7
28 ± 5
205 ± 4
ABTSb (low efficiency)
3170 ± 270
1280 ± 350
2150 ± 420
539 ± 24
103 ± 10
25 ± 2
k cat /K m
170 ± 8
80 ± 15
12 ± 1
ABTS (high efficiency)
5.4 ± 0.7
13.7 ± 3.5
21.3 ± 2.3
2.1 ± 0.1
12.5 ± 0.7
6.5 ± 0.2
k cat /K m
400 ± 44
911 ± 212
300 ± 25
4.8 ± 0.8
12.6 ± 3.6
2.4 ± 0.2
5.4 ± 0.8
k cat /K m
504 ± 50
428 ± 68
Direction of evolution
The above substrates are oxidized at different sites, and the kinetic analysis shows how these sites have evolved giving rise to different peroxidase families. The sites for oxidation of Mn2+ and high redox-potential substrates such as VA (and RB5) have been already described above. Phenols, such as DMP (and the generic oxidoreductase substrate ABTS) can be oxidized: (i) with high efficiency at the same tryptophan oxidizing the high redox-potential substrates; and (ii) with low efficiency at one of the heme access channels [39, 40].
As regard for the high redox-potential substrates, the turning point where the LiP/VP usual substrate VA (and the recalcitrant dye RB5) begins to be oxidized in this evolutionary line is AVP, with the appearance of the exposed Trp172 at a position that coincides with the catalytic tryptophan in extant VP and LiP [35–37]. The catalytic efficiency towards VA is maintained from AVP to ALiP and then sharply increases (sevenfold) from ALiP to LiPH8. The k cat value did not change, and the higher catalytic efficiency is due to an improvement in VA affinity (tenfold lower K m value). The appearance of Trp172 also resulted in efficient oxidation of the low redox-potential substrates, fully substituting the low efficiency site in ALiP and extant LiP. The activity of the catalytic tryptophan in the advanced stages of peroxidase evolution will be affected by the electrostatic charge of its surface environment (Additional file 1: Fig. S4): VA cation radical will be stabilized by the strongly acidic environment in LiPH8 that, in contrast, will prevent the oxidation of anionic RB5.
Stability of ancestral peroxidases
Over the last years there has been a profound mining of basidiomycete genomes to find new enzymes and obtain evolutionary information [25, 31, 41, 42]. Our analysis of the lineage from the most ancestral peroxidase in Polyporales, a basidiomycete order that appeared near 150 mya at the end of the Jurassic [25, 26], to P. chrysosporium LiP [18, 27] reveals how these enzymes acquired the ability to degrade lignin and how this ability changed with time. At the same time, the reconstruction of ancestral peroxidases provides proteins of biotechnological interest in lignocellulose biorefineries  (e.g., CaPo is a thermostable enzyme and a good candidate for further directed evolution, as it has the potential to become every peroxidase in the phylogenetic tree).
In the above analysis, we used PAML , a common software for ancestral protein reconstruction, and the published ML phylogenetic tree of class-II peroxidases in Polyporales , whose accuracy is assured by a precise annotation of the peroxidase genes. The program uses the best evolutionary model for the sequences analyzed (WAG model in this case) to predict the most probable amino acid at every position of each node in the phylogenetic tree (providing a complete matrix with the probabilities of every other amino acids). The reconstruction procedure has inherent limitations for sequence prediction in the most ancestral nodes (such as CaPo) that can be partially overcome by sequence sampling from the PAML matrix and in silico and/or experimental evaluation of ancestor variability (reconstruction robustness) with respect to the property/ies most relevant for each phylogenetic analysis (catalytic properties defining the different peroxidase types, in the present study).
Ligninolytic peroxidases are high redox-potential enzymes being this characteristic related to the distance between the heme iron and the proximal histidine (Nε) acting as its fifth ligand [43, 44]. This distance is shorter in the peroxidases of prokaryotic origin, such as cytochrome c peroxidase (CcP), and significantly increased in fungal peroxidases. This is due to an H-bond between a backbone carbonyl (LiPH8 Asp201) and the hydroxyl of a Ser/Thr residue (LiPH8 Ser177, absent from CcP) that displaces the contiguous proximal histidine increasing the electron deficiency of iron in ligninolytic and other eukaryotic peroxidases. The distance between the His177Nε and the heme iron in the molecular models of the ancestral peroxidases are not significantly different from those found in LiP, due to conserved Ser/Thr178-Asp202 and His177-Asp239 H-bonds, although significantly larger than in CcP (Additional file 1: Fig. S3). Therefore, no strong changes in peroxidase redox-potential are expected to be produced during LiP evolution in Polyporales, and the VA oxidation ability of AVP (and ALiP) would be mainly related to the appearance of the surface catalytic tryptophan.
It is important that the heme peroxidase redox-potential, and lignin-degrading ability of basidiomycete peroxidases, drastically increases when pH decreases . Therefore, the improved stability at acidic pH in the most recent stages of peroxidase evolution in Polyporales (from AVP to extant LiP) represents an important evolutionary adaptation to the acidic conditions where ligninolysis occurs in nature . Concerning thermal stability, AVP appears as the most thermostable ancestral peroxidase in Polyporales, especially when compared with its descendants. Experimental evidence is required to know if genetic drift [47, 48] caused the increased stability of AVP related with the appearance and subsequent evolution of the catalytic tryptophan. After that, the loss of the Mn2+-binding site caused a decrease in stability, since the Mn-binding site can (in the presence of Mn2+ or other cations) contribute to anchor the heme cofactor [19, 34], but proteins were still stable in order to be selected in evolution. In agreement with the present results, increased thermal stability has been reported for both an ancestral plant peroxidase  and a LiP containing several ancestral mutations .
The kinetic constants of the resurrected peroxidases show the high evolvability of these enzymes incorporating new activities. Although some exceptions have been reported [51, 52], it is generally assumed that ancestral enzymes have a wide substrate specificity and are specialized after duplication events [4, 6, 53]. However, peroxidases in Polyporales show a different evolutionary history. The first ancestor (CaPo) is able to oxidize only low redox-potential substrates, and Mn2+ with low catalytic efficiency. This low Mn2+-oxidizing activity is in agreement with the GP-type ancestor of Dikarya peroxidases . Similar substrate specificity has been reported for the extant short MnPs, where CaPo and CaCD would be included according to their short C-terminal tail . This suggests that short MnPs are old enzymes, whose efficiency oxidizing Mn2+ was improved later. Then, the efficiency oxidizing Mn2+ increased in AVP (the first VP in Polyporales) with activity on this cation similar to extant VP . What is surprising, as mentioned above, is that the AVP appearance, a relatively recent event in the mid-term evolution of Polyporales peroxidases, resulted in the enzyme with the widest specificity: AVP is able to oxidize every substrate assayed. Then, evolution focused in the direction of more efficient oxidation of nonphenolic lignin at Trp172, as shown using VA, and resulted in the appearance of LiP, the most specialized ligninolytic enzyme only reported in the order Polyporales [25, 31, 42]. However, this “unusual” evolutionary behavior is most probably related to the existence of three different substrate oxidation sites in these peroxidases, whose appearance/disappearance caused qualitative changes in catalytic activities (compared with enzymes with a progressively specialized unique catalytic site).
From an organismal point of view, the above evolutionary trend can be seen as a search for new and more efficient tools to degrade lignin. From their appearance in the late Jurassic, Polyporales had ligninolytic peroxidases, as shown by the ancestral enzyme reconstruction. The oldest ancestors would use Mn2+, being Mn3+ able to oxidize the minor phenolic moiety of lignin . Trp172 appeared later giving versatile AVP that oxidizes Mn2+ (more efficiently than its MnP-type ancestors), phenols, and most probably also nonphenolic lignin, as shown by its ability to oxidize high redox-potential substrates. When ALiP appeared, the Mn2+-binding site was lost, as well as the low efficiency site oxidizing phenols. In this way, non-competitive inhibition of lignin oxidation was prevented. Although the ability to oxidize Mn2+ was lost in the evolutionary line leading to LiPH8, a family of highly efficient Mn2+-oxidizing peroxidases (cluster C) evolved from the first peroxidase ancestor CaPo. Finally, after the appearance of the exposed tryptophan in AVP, the peroxidase catalytic efficiency oxidizing VA was improved, first by increasing the k cat in ALiP and later by improving the K m in LiPH8, which means a peroxidase specialization towards lignin degradation.
We predict that the evolutionary pathway leading to the most efficient lignin-degrading enzymes (LiP family, only found in Polyporales) included successive incorporation of: (i) a surface tryptophan to an ancestral short MnP resulting in an ancestral VP; and (ii) loss of the Mn2+-binding site generating the first LiP. The experimental evaluation of catalytic properties of the resurrected ancestral enzymes was consistent with the bioinformatic analysis and prove the above hypothesis. Interestingly, an increase of stability at acidic pH was found simultaneously with the appearance of the catalytic tryptophan, enabling these enzymes to act under the acidic conditions characterizing lignin decay. The evolutionary and experimental studies also show that some ancestral peroxidases are of biotechnological interest because of their stability and potential evolvability.
113 predicted peroxidase sequences (mature proteins) from the genomes of ten Polyporales (phylum Basidiomycota) species (namely B. adusta, C. subvermispora, D. squalens, F. pinicola, Ganoderma sp., P. brevispora, P. chrysosporium, P. placenta, T. versicolor, and W. cocos) available at the DOE JGI Mycocosm portal (as http://genome.jgi.doe.gov/Bjead1_1/Bjead1_1.home.html, http://genome.jgi.doe.gov/Cersu1/Cersu1.home.html, http://genome.jgi.doe.gov/Dicsq1/Dicsq1.home.html, http://genome.jgi.doe.gov/Fompi3/Fompi3.home.html, http://genome.jgi.doe.gov/Gansp1/Gansp1.home.html, http://genome.jgi.doe.gov/Phlbr1/Phlbr1.home.html, http://genome.jgi.doe.gov/Phchr2/Phchr2.home.html, http://genome.jgi.doe.gov/Pospl1/Pospl1.home.html, http://genome.jgi.doe.gov/Trave1/Trave1.home.html and http://genome.jgi.doe.gov/Wolco1/Wolco1.home.html, respectively), all of them containing one or several peroxidases of the peroxidase–catalase superfamily , have been used in this study (Additional file 2 ).
The amino-acid sequences were aligned with MUSCLE as implemented in MEGA 7 . ML analysis was then performed using RAxML  under the GTR model with GAMMA-distributed rate of heterogeneity, using the WAG evolution model, as suggested by ProtTest .
Ancestral sequence reconstruction
PAML 4.7 package  was used to obtain the posterior amino-acid probability per site in each ancestor under the WAG model of evolution, and the most probable whole sequences for each of the nodes, using as inputs the ML phylogeny and the MUSCLE alignment previously obtained (PAML reconstructions using the LG and Dayhoff evolution models were also performed for comparison). Marginal reconstruction was selected for the present work.
Five thousand sequences (including the most probable ancestor predicted by PAML) were selected for each of the nodes by successive Monte Carlo sampling steps (using an ad hoc program kindly provided by Dr J.M. Sanchez-Ruiz and 0.2 and 0.5 probability thresholds, referred to the highest probability at every position) . These sequences were manually corrected for C-terminal and other insertions or deletions (the former often originating from intron to exon transitions) according to the sequences of the ancestor progeny, and inspected for the presence/absence of the substrate oxidation sites (Glu37, Glu40, and Asp183 involved in Mn2+ binding, and Trp172 responsible for VA oxidation).
The 5000 CaPo sequences were classified into three subsets corresponding to sequences containing: (i) the three acidic residues forming a typical Mn2+-binding site (including the most probable ancestor); (ii) an atypical Mn2+-binding site formed by only two of the above acidic residues, without a basic residue in the third position (including CaPo-tris selected later); and (iii) a site formed by two of the above acidic residues plus a basic residue in the third position (including CaPo-bis selected later), with Trp172 being absent in all the cases. The Monte Carlo sampling provided a significant number of alternative sequences with an arginine (or lysine) residue in position 183 (forming the above subset-iii) whose presence prevented binding and oxidation of the Mn2+ cation (as confirmed after CaPo-bis resurrection). However, for the most probable sequence, PAML reconstructed an aspartic acid at this position (resulting in a functional Mn2+-binding site after CaPo resurrection) in agreement with the extant peroxidases from the ten Polyporales genomes analyzed (with only 5% sequences containing a basic residue at this position).
Each of the CaPo subsets was submitted to a random sampling, together with the whole sets for the three other nodes (where no subsets were defined because the 5000 sequences from each of them showed the same catalytic sites), yielding 12 representative sequences, including the four most probable ones, that were analyzed in silico.
Then, the DNA sequences encoding the most probable amino-acid sequences for the four reconstructed nodes, together with the two alternative sequences from the CaPo subsets, were synthesized by ATG:biosynthetics (Merzhausen, Germany) after optimizing the codon usage for high expression in E. coli using OPTIMIZER .
Molecular models of the predicted proteins were obtained at the Swiss-Model automated protein homology modeling server  using related crystal structures, selected using the GMQE parameter, as templates (PDB entries 4BM1, 3FJW, and 1QPA corresponding to Pleurotus ostreatus MnP, P. eryngii VP, and P. chrysosporium LiP, respectively). All protein models had great quality taking into account the Swiss-Model parameters (good QMEAN and high GMQE). The electrostatic surfaces were computed with the PyMOL Molecular Graphics System, version 1.8 Schrödinger, LLC (http://pymol.org) using default parameters.
E. coli expression
After gene synthesis, the coding sequences of the most probable CaPo, CaCD, AVP, and ALiP ancestral sequences, plus the two additional CaPo sequences described above (CaPo-bis and CaPo-tris), and the extant LiPH8 were cloned into the expression vector pET23b(+) (Novagen). The resulting plasmids were transformed into E. coli DH5α for propagation and conservation, and into BL21(DE3)pLysS (ancestors) or W3110 (LiPH8) for expression. With this purpose, cells were grown in Terrific broth until an OD600 0.5 to 0.6 to reach an adequate expression level, induced with 1 mM isopropyl-β-d-thiogalactopyranoside, and grown for another 4 h.
The apoenzymes accumulated in inclusion bodies, as reveled by sodium dodecyl sulfate–polyacrylamide gel electrophoresis, and were activated in vitro [41, 58]. After solubilization in 8 M urea, the refolding conditions for the ancestral proteins included: 0.16 M urea, 5 mM CaCl2, 15 µM hemin, 0.4 mM oxidized glutathione, 0.1 mM dithiothreitol, and 0.1 mg/mL of protein in 50 mM Tris–HCl, pH 9.5. The refolding conditions for LiPH8 were: 2.1 M urea, 5 mM CaCl2, 10 µM hemin, 0.7 mM oxidized glutathione, 0.1 mM dithiothreitol, and 0.2 mg/mL of protein, in buffer 40 mM Tris–HCl, pH 9.5 . The active enzymes were purified using a Resource-Q column (GE-Healthcare, USA) with 0–400 mM NaCl salt gradient and 2 mL/min flow in 10 mM sodium acetate, pH 5.5, containing 1 mM of CaCl2.
Five different substrates were selected for the kinetic characterization of the resurrected peroxidases: (i) Mn2+, which is oxidized to Mn3+ (Mn3+-tartrate complex ε238 6500 M−1 cm−1); (ii) VA, whose oxidation product is veratraldehyde (ε310 9300 M−1 cm−1); (iii) DMP, which dimerizes to coerulignone (ε469 55,000 M−1·cm−1); (iv) ABTS, which is oxidized yielding the cation radical (ε436 29,300 M−1 cm−1); and (v) RB5, whose disappearance/discoloration after oxidation was measured (ε598 30,000 M−1 cm−1). These reactions were analyzed using a Thermo Scientific Biomate5 spectrophotometer, at 25 °C and the optimal pH and H2O2 concentration for each enzyme, determined using 50 mM Britton–Robinson (B&R) buffer (pH 2–10) and 2.5 mM ABTS as substrate (see Table 1 footnote). The sigmoid kinetic curves obtained for oxidation of DMP and ABTS enabled calculation of two sets of constants for AVP, corresponding to low and high efficiency oxidation sites, as reported for extant VP .
pH and temperature stability
To study the effect of pH on enzyme stability, the resurrected peroxidases and extant LiPH8 were incubated in B&R buffer, pH 2–10, at 25 °C for 4 h. Then, the residual activity was estimated by the oxidation of ABTS (2.5 mM), under the conditions described above. For every enzyme, the activity after 1 min incubation at 25 °C in pH 5 buffer was taken as 100%, and the percentages of residual activity at the different pH conditions were referred to this value.
To study their thermal stability, the enzymes were incubated in 10 mM acetate, pH 5.5, for 10 min at 5 °C intervals in the range 25–85 °C. Residual activity was measured and calculated as described above. Temperature stability was presented as the 10 min T 50, i.e., the temperature at which 50% of the activity was lost after 10 min incubation.
The effect of temperature on circular dichroism spectra was addressed studying the changes at 222 nm from 20 to 95 °C, 30 °C/h, using a Jasco J-815 spectropolarimeter equipped with a Peltier temperature controller and a thermostated cell holder on a 0.1 cm path length quartz cell. A final concentration of 6 µM pure enzyme in 10 mM acetate, pH 5.5 was used. T m represents the temperature at the midpoint of the unfolding transition in the thermal melting profiles.
The effect of Mn2+ in the enzyme thermal inactivation and structure unfolding was analyzed by adding 1 mM SO4Mn to the incubation mixture, and measuring the residual activity by oxidation of 6 mM Mn2+, as described above.
common ancestor of cluster-D peroxidases
common ancestor of Polyporales peroxidases
cytochrome c peroxidase
- k cat :
- K m :
isoenzyme H8 of P. chrysosporium LiP
Reactive Black 5
IAF performed experimental work; FJRD and ATM designed research; all authors analyzed data and wrote the paper. All authors read and approved the final manuscript.
The authors thank Valeria Risso and José M. Sánchez-Ruiz (Granada, Spain) for providing the program used for Monte Carlo sampling and their helpful suggestions on ancestral sequence reconstruction, and David S. Hibbett (Clark University, USA) for his comments on phylogenetic analysis. IAF thanks a MINECO FPI Fellowship. We acknowledge support of the publication fee by the CSIC Open Access Publication Support Initiative through its Unit of Information Resources for Research (URICI), and the EC OpenAIRE FP7 post-grant Open Access Pilot.
The authors declare that they have no competing interests.
Availability of data and materials
All data generated or analyzed during this study are included in this published article and its supplementary information files.
This work was supported by the INDOX (KBBE-2013-613549) and EnzOx2 (H2020-BBI-PPP-2015-2-720297) EU projects and the NOESIS (BIO2014-56388-R) project of the Spanish Ministry of Economy and Competitiveness (MINECO). The work conducted by JGI was supported by the Office of Science of the U.S. Department of Energy under Contract DE-AC02-05CH11231.
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