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.2012 Jun 29;336(6089):1715-9.
doi: 10.1126/science.1221748.

The Paleozoic origin of enzymatic lignin decomposition reconstructed from 31 fungal genomes

Dimitrios Floudas  1Manfred BinderRobert RileyKerrie BarryRobert A BlanchetteBernard HenrissatAngel T MartínezRobert OtillarJoseph W SpataforaJagjit S YadavAndrea AertsIsabelle BenoitAlex BoydAlexis CarlsonAlex CopelandPedro M CoutinhoRonald P de VriesPatricia FerreiraKeisha FindleyBrian FosterJill GaskellDylan GlotzerPaweł GóreckiJoseph HeitmanCedar HesseChiaki HoriKiyohiko IgarashiJoel A JurgensNathan KallenPhil KerstenAnnegret KohlerUrsula KüesT K Arun KumarAlan KuoKurt LaButtiLuis F LarrondoErika LindquistAlbee LingVincent LombardSusan LucasTaina LundellRachael MartinDavid J McLaughlinIngo MorgensternEmanuelle MorinClaude MuratLaszlo G NagyMatt NolanRobin A OhmAleksandrina PatyshakuliyevaAntonis RokasFrancisco J Ruiz-DueñasGrzegorz SabatAsaf SalamovMasahiro SamejimaJeremy SchmutzJason C SlotFranz St JohnJan StenlidHui SunSheng SunKhajamohiddin SyedAdrian TsangAd WiebengaDarcy YoungAntonio PisabarroDaniel C EastwoodFrancis MartinDan CullenIgor V GrigorievDavid S Hibbett
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Free article

The Paleozoic origin of enzymatic lignin decomposition reconstructed from 31 fungal genomes

Dimitrios Floudas et al. Science..
Free article

Abstract

Wood is a major pool of organic carbon that is highly resistant to decay, owing largely to the presence of lignin. The only organisms capable of substantial lignin decay are white rot fungi in the Agaricomycetes, which also contains non-lignin-degrading brown rot and ectomycorrhizal species. Comparative analyses of 31 fungal genomes (12 generated for this study) suggest that lignin-degrading peroxidases expanded in the lineage leading to the ancestor of the Agaricomycetes, which is reconstructed as a white rot species, and then contracted in parallel lineages leading to brown rot and mycorrhizal species. Molecular clock analyses suggest that the origin of lignin degradation might have coincided with the sharp decrease in the rate of organic carbon burial around the end of the Carboniferous period.

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