| Literature DB >> 28293293 |
Mathieu Fanuel1, Sona Garajova2, David Ropartz1, Nicholas McGregor3,4, Harry Brumer3,4,5,6, Hélène Rogniaux1, Jean-Guy Berrin2.
Abstract
BACKGROUND: The enzymatic conversion of plant biomass has been recently revolutionized by the discovery of lytic polysaccharide monooxygenases (LPMO) that catalyze oxidative cleavage of polysaccharides. These powerful enzymes are secreted by a large number of fungal saprotrophs and are important components of commercial enzyme cocktails used for industrial biomass conversion. Among the 33 AA9 LPMOs encoded by the genome of Podospora anserina, the PaLPMO9H enzyme catalyzes mixed C1/C4 oxidative cleavage of cellulose and cello-oligosaccharides. Activity of PaLPMO9H on several hemicelluloses has been suggested, but the regioselectivity of the cleavage remained to be determined.Entities:
Keywords: AA9; Biomass; Biorefinery; LPMO; Lignocellulose; Mass spectrometry; Polysaccharides
Year: 2017 PMID: 28293293 PMCID: PMC5346257 DOI: 10.1186/s13068-017-0749-5
Source DB: PubMed Journal: Biotechnol Biofuels ISSN: 1754-6834 Impact factor: 6.040
Fig. 1ESI-MS spectra showing the degradation products generated from several cellulosic and hemicellulosic substrates by PaLPMO9H under ascorbate conditions. a Cellulose; b lichenan; c MLG; d GM; e XyG. Species were detected as sodium adducts ([M+Na]+) except for XXXGXXXG which was detected as [M+2Na]2+. The main degrees of polymerization (DP) were annotated. Right panel enlarged view of the DP4 species, for all substrates; stars the non-modified product. Peaks indicated by an arrow were attributed to the oxidized species (−2, +16, +32 Da relative to the non-modified species) and were further characterized by tandem MS (full arrow data presented in the following sections; empty arrows data not shown). Labels of the oxidized species were proposed based on tandem MS results. For cellulose: “diol C4+ diol Cx” indicates a double oxidation (diols): one has been localized at C4 of the non-reducing end, while the second one could not be precisely localized and is either localized at the reducing end or non-reducing end
Fig. 2Ion mobility recorded in positive ionization mode for the non-modified DP4 species (m/z 689.2 Da) released from the incubation of PaLPMO9H with cellulose (black trace), MLG (green trace), and lichenan (red trace). Drift times are indicated in bins (arbitrary units). The shoulder peak in the case of cellulose DP4 was attributed to a slight heterogeneity in the gas-phase isoforms
Fig. 3Tandem MS spectra of the oxidized species (ketone and gem-diol, detected at m/z 687.17 and 705.18, respectively) generated from lichenan by PaLPMO9H under ascorbate conditions. These spectra represent the fragmentation of the isoforms with a drift time of 76 bins in ion mobility. These isoforms were attributed to structures composed of only (1→4)-linked β-d-glucose residues. c Tandem MS spectrum of the ketone form; d tandem MS spectrum of the gem-diol form. Observed fragments are depicted on the structures in a and b for spectra c and d, respectively
Fig. 4Tandem MS spectrum of the species displaying a +16 Da mass shift from the unmodified DP4 produced by PaLPMO9H from XXXGXXXG (detected at m/z 645.16). The observed fragments indicate the co-existence of two oxidized forms: a gem-diol at the non-reducing end and an aldonic acid at the reducing end. Observed fragments are depicted on the structures in a and b. Red fragments are specific of the aldonic acid, purple fragments are specific of the gem-diol and blue fragments are common to both oxidized species. Fragments labeled with a star could not be attributed to either expected structures. Their masses match with an oxidation at one laterally branched xylose residue, which origin remains undetermined
Fig. 5Schematic display of the broad substrate specificity of PaLPMO9H according to the symbol nomenclature described in [28]. Oxidation is represented at specific carbon position (indicated by a number) when this position has been precisely determined by tandem MS. The chemical forms of oxidation that were characterized in this study are displayed (i.e. diol and aldonic acid for the +16 Da species, ketone for the −2 Da species). No lactone is represented, as we exclusively observed ketones for the −2 Da species. In the case of MLG and lichenan, oxidation at the non-reducing end may be localized at C3 or C4, but this was not determined. One example was arbitrarily chosen to represent the possible structures with internal β-(1→3) bonds: this bond might actually be at any backbone position