Evidence of fungal activity in silicified gymnosperm wood from the Eocene of southern Patagonia (Argentina)
Evidence of fungal activity expressed as typical decay patterns is described from silicified podocarpaceous wood from the Eocene of Patagonia, Argentina. Decay features consist of tracheids of the secondary xylem that are degraded, resulting in thin-celled, lignin-free, translucent, circular to elli...
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2009
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| LEADER | 12194caa a22010937a 4500 | ||
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| 001 | PAPER-8535 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518203820.0 | ||
| 008 | 190411s2009 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-70349510112 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Pujana, R.R. | |
| 245 | 1 | 0 | |a Evidence of fungal activity in silicified gymnosperm wood from the Eocene of southern Patagonia (Argentina) |
| 260 | |c 2009 | ||
| 270 | 1 | 0 | |m Pujana, R.R.; Museo Argentino de Ciencias Naturales, Ángel Gallardo 470, C1405DJR Ciudad de Buenos Aires, Argentina; email: rpujana@macn.gov.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a Evidence of fungal activity expressed as typical decay patterns is described from silicified podocarpaceous wood from the Eocene of Patagonia, Argentina. Decay features consist of tracheids of the secondary xylem that are degraded, resulting in thin-celled, lignin-free, translucent, circular to elliptical areas, some of which have cells devoid of all cell wall components including lignin, hemicellulose, and cellulose, and other areas that show only partial simultaneous decay of all cell wall layers. These patterns conform to the white rot and its variant white pocket rot decay patterns produced by basidiomycetes and ascomycetes in gymnosperm and angiosperm wood in modern terrestrial ecosystems. Coagulated opaque bodies in the lumen of some cells and enlarged secondary walls may represent host reactions to infection or remains of metabolic products of fungal enzymatic activity. Similar decay patterns and reaction features have been described from fossil woods ranging in age from the Devonian to the present. This record expands the fossil record of wood rot fungi and underscores their importance as drivers of biological cycles in ancient terrestrial ecosystems. © 2009 Elsevier Masson SAS. All rights reserved. |l eng | |
| 593 | |a Museo Argentino de Ciencias Naturales, Ángel Gallardo 470, C1405DJR Ciudad de Buenos Aires, Argentina | ||
| 593 | |a Department of Geological Sciences, Southern Methodist University, PO Box 750395, Dallas, TX 75275-0395, United States | ||
| 593 | |a DBBE, Facultad de Ciencias Exactas y Naturales, UBA, Intendente Güiraldes 2160, C1428EGA Ciudad de Buenos Aires, Argentina | ||
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a SOUTH AMERICA | |
| 690 | 1 | 0 | |a EOCENE |
| 690 | 1 | 0 | |a FUNGAL ACTIVITY |
| 690 | 1 | 0 | |a PATAGONIA |
| 690 | 1 | 0 | |a PODOCARPACEOUS WOOD |
| 690 | 1 | 0 | |a CELLULOSE |
| 690 | 1 | 0 | |a EOCENE |
| 690 | 1 | 0 | |a FOSSIL RECORD |
| 690 | 1 | 0 | |a FUNGUS |
| 690 | 1 | 0 | |a GYMNOSPERM |
| 690 | 1 | 0 | |a LIGNIN |
| 690 | 1 | 0 | |a WOOD |
| 690 | 1 | 0 | |a XYLEM |
| 690 | 1 | 0 | |a PATAGONIA |
| 690 | 1 | 0 | |a ASCOMYCOTA |
| 690 | 1 | 0 | |a BASIDIOMYCOTA |
| 690 | 1 | 0 | |a FUNGI |
| 690 | 1 | 0 | |a GYMNOSPERMAE |
| 690 | 1 | 0 | |a MAGNOLIOPHYTA |
| 700 | 1 | |a Massini, J.L.G. | |
| 700 | 1 | |a Brizuela, R.R. | |
| 700 | 1 | |a Burrieza, H.P. | |
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