13 research outputs found

    Wood Decay in Silicified Gymnosperms from Antarctica

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    This is the publisher's version, also available electronically from http://www.jstor.org.Gymnospermous secondary xylem degraded by wood-decaying fungi was examined in silicified fossils from Antarctica. AraucarioxyIon-type wood from the Triassic and specimens of Vertebraria from the Permian demonstrate similar patterns of decay. Specimens are characterized by irregularly shaped areas lacking cells and are infected with branched, septate hyphae with clamp connections. The decay in these fossils is comparable in appearance to present-day rots caused by basidiomycetes. Two patterns of decay are evident: (1) A wall component, presumably lignin, is removed from the wall and middle lamella of infected tracheids, leaving a considerably thinner cellulose framework; and (2) the primary and secondary walls typically separate, and all wall layers are progressively reduced in thickness and eventually removed. The middle lamella, particularly where it is thickest in the corners between cells, persists longer than other layers. Indications of host response to fungal attack include the production of possible wall appositions. Evidence of wood decay occurs as early as the Upper Devonian, and all reported cases from the fossil record are similar to those found today

    A possible endogonaceous fungus from the Triassic of Antarctica

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    Studies of Paleozoic fungi. IV. Wall ultrastructure of fossil endogonaceous chlamydospores

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    Fossil endogonaceous chlamydospores are described from the aerial axes and roots of several Paleozoic plants preserved in calcilutite nodules and calcareous coal balls. Specimens come from six Paleozoic localities extending from the uppermost Lower Devonian through the Upper Pennsylvanian. Although fossil chlamydospores are markedly similar to the modern Endogonaceae in transmitted light, ultrastructural comparisons have not previously been made. The fine structure of the walls of these spores is consistent with past interpretations which relate them to the modern Endogonaceae, but thorough comparisons cannot be made due to the lack of comparable ultrastructural information from extant VA mycorrhizae. The evidence from mycorrhizal associations in the fossil record is evaluated

    Studies Of Paleozoic Fungi. Iv. Wood‐Decaying Fungi In Callixylon Newberryi From The Upper Devonian

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    Peer Reviewedhttps://deepblue.lib.umich.edu/bitstream/2027.42/141580/1/ajb208449.pd

    Geotrichites glaesarius, a conidial fungus from Dominican amber

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    Geotrichites glaesarius, a new fungal anamorph, is described from Dominican amber of late Oligocene or early Miocene age. A well-developed mycelium is present on the surface of an arachnid cadaver; hyphae are not present in the body cavity. Septate hyphae are either erect or decumbent, and extensively branched. Oblong arthroconidia are borne terminally on undifferentiated hyphae. Conidiogenesis appears to be of the holoarthric type with conidia sometimes joined by narrow connectives. The fungus is apparently saprophytic and resembles several modern moniliaceous fungi, particularly Geotrichum candidum
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