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    Author(s): Dimitrios Floudas; Manfred Binder; Robert Riely; Kerrie Barry; Robert A. Blanchette; Bernard Henrissat; Angel T. Martínez; Robert Otillar; Joseph W. Spatafora; Jagjit S. Yadav; Andrea Aerts; Isabelle Benoit; Alex Boyd; Alexis Carlson; Alex Copeland; Pedro M. Coutinho; Ronald P. deVries; Patricia Ferreira; Keisha Findley; Brian Foster; Jill Gaskell; Dylan Glotzer; Pawe³ Górecki; Joseph Heitman; Cedar Hesse; Chiaki Hori; Kiyohiko Igarashi; Joel A. Jurgens; Nathan Kallen; Phil Kersten; Annegret Kohler; Ursula Kües; T. K. ArunKumar; Alan Kuo; Kurt LaButti; Luis F. Larrondo; Erika Lindquist; Albee Ling; Vincent Lombard; Susan Lucas; Taina Lundell; Rachael Martin; David J. McLaughlin; Ingo Morgenstern; Emanuelle Morin; Claude Murat; Laszlo G. Nagy; Matt Nolan; Robin A. Ohm; Aleksandrina Patyshakuliyeva; Antonis Rokas; Francisco J. Ruiz-Dueñas; Grzegorz Sabat; Asaf Salamov; Masahiro Samejima; Jeremy Schmutz; Jason C. Slot; Franz St. John; Jan Stenlid; Hui Sun; Sheng Sun; Khajamohiddin Syed; Adrian Tsang; Ad Wiebenga; Darcy Young; Antonio Pisabarro; Daniel C. Eastwood; Francis Martin; Dan Cullen; Igor V. Grigoriev; David S. Hibbett
    Date: 2012
    Source: SCIENCE VOL 336 29 JUNE 2012 (2012) DOI:1126/science.1221748,
    Publication Series: Scientific Journal (JRNL)
    Station: Forest Products Laboratory
    PDF: View PDF  (653.69 KB)


    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 arboniferous period. no package

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    Floudas, Dimitrios; Binder, Manfred; Riely, Robert; Barry, Kerrie; Blanchette, Robert A.; Henrissat, Bernard; Martínez, Angel T.; Otillar, Robert; Spatafora, Joseph W.; Yadav, Jagjit S.; Aerts, Andrea; Benoit, Isabelle; Boyd, Alex; Carlson, Alexis; Copeland, Alex; Coutinho, Pedro M.; deVries, Ronald P.; Ferreira, Patricia; Findley, Keisha; Foster, Brian; Gaskell, Jill; Glotzer, Dylan; Górecki, Pawel; Heitman, Joseph; Hesse, Cedar; Hori, Chiaki; Igarashi, Kiyohiko; Jurgens, Joel A.; Kallen, Nathan; Kersten, Phil; Kohler, Annegret; Kües, Ursula; ArunKumar, T. K.; Kuo, Alan; LaButti, Kurt; Larrondo, Luis F.; Lindquist, Erika; Ling, Albee; Lombard, Vincent; Lucas, Susan; Lundell, Taina; Martin, Rachael; McLaughlin, David J.; Morgenstern, Ingo; Morin, Emanuelle; Murat, Claude; Nagy, Laszlo G.; Nolan, Matt; Ohm, Robin A.; Patyshakuliyeva, Aleksandrina; Rokas, Antonis; Ruiz-Dueñas, Francisco J.; Sabat, Grzegorz; Salamov, Asaf; Samejima, Masahiro; Schmutz, Jeremy; Slot, Jason C.; John, Franz St.; Stenlid, Jan; Sun, Hui; Sun, Sheng; Syed, Khajamohiddin; Tsang, Adrian; Wiebenga, Ad; Young, Darcy; Pisabarro, Antonio; Eastwood, Daniel C.; Martin, Francis; Cullen, Dan; Grigoriev, Igor V.; Hibbett, David S. 2012. The paleozoic origin of enzymatic lignin decomposition reconstructed from 31 fungal genomes. Science. 336(29): 1715-1719.


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    lignin, genome, white-rot, brown-rot, molecular clock, evolution

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