2007
DOI: 10.1016/j.mycres.2007.02.004
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Evidence of mycoparasitism and hypermycoparasitism in Early Cretaceous amber

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Cited by 53 publications
(33 citation statements)
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“…Archaeomarasmius legettii (94-90 Myr) 73 was used to define minimum age constraint (92 Myr) for the origin of marasmioid clade (as used in a previous study 74 ). Palaeoagaricites antiquus (100-110 Myr) is the oldest fossil can be placed within Agaricales 75 , hence we constrained the MRCAs of this order to a minimum age of 108 Myr. To define the minimum age constraint of the origin of Boletales to 84 Myr, we referred to published analyses 27 .…”
Section: Methodsmentioning
confidence: 99%
“…Archaeomarasmius legettii (94-90 Myr) 73 was used to define minimum age constraint (92 Myr) for the origin of marasmioid clade (as used in a previous study 74 ). Palaeoagaricites antiquus (100-110 Myr) is the oldest fossil can be placed within Agaricales 75 , hence we constrained the MRCAs of this order to a minimum age of 108 Myr. To define the minimum age constraint of the origin of Boletales to 84 Myr, we referred to published analyses 27 .…”
Section: Methodsmentioning
confidence: 99%
“…Similar structures occasionally are encountered in the leaf fossil record (Labandeira et al, 2007; DT49 on p. 13). Other defenses are formation of sheaths surrounding individual hyphae or fascicles of hyphae, and deposition of gums and resins (Cleary et al, 2012b), which have a rich fossil record as amber and copal that frequently incorporate the vector of the fungus (Poinar and Buckley, 2007), but rarely reveal evidence of the fungal disease (Poinar and Poinar, 2005). Profuse production of gums and resins often occurs in woody tissues of conifers and flowering plants as a defense from pathogenic fungi and those wood-boring insects that particularly target cambial tissues as a larval food resource (Villari et al, 2012).…”
Section: How Do Pathogens Attack Plant-organs and Tissues And How Do mentioning
confidence: 99%
“…In contrast to these fungal-plant associations, the fossil record of fungal-animal interactions consists of fungi associated with coral and marine shell borings and microarthropod fecal pellets from the Silurian (Sherwood-Pike and Gray, 1985), and trichomycetes (ubiquitously associated with arthropods today) that occur with Triassic insect exoskeletons (White and Taylor, 1989). Fungi are also described with plants in dinosaur coprolites from the Upper Cretaceous (Maastrichtian) Lameta Formation of India (Sharma et al, 2005) and co-occur with microbes, algae, and arthropods in Cretaceous and Eocene amber (Taylor, 1990;Schmidt et al, 2006;Poinar and Buckley, 2007). The sample in this study represents the first report of fungi preserved in a fossil turtle egg.…”
Section: The Fossil Record Of Fungimentioning
confidence: 72%