Please use this identifier to cite or link to this item: http://cmuir.cmu.ac.th/jspui/handle/6653943832/65267
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dc.contributor.authorMilan C. Samarakoonen_US
dc.contributor.authorKevin D. Hydeen_US
dc.contributor.authorSinang Hongsananen_US
dc.contributor.authorEric H.C. McKenzieen_US
dc.contributor.authorHiran A. Ariyawansaen_US
dc.contributor.authorItthayakorn Promputthaen_US
dc.contributor.authorXiang Yu Zengen_US
dc.contributor.authorQing Tianen_US
dc.contributor.authorJian Kui (Jack) Liuen_US
dc.date.accessioned2019-08-05T04:31:06Z-
dc.date.available2019-08-05T04:31:06Z-
dc.date.issued2019-05-01en_US
dc.identifier.issn18789129en_US
dc.identifier.issn15602745en_US
dc.identifier.other2-s2.0-85064831249en_US
dc.identifier.other10.1007/s13225-019-00423-8en_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85064831249&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/65267-
dc.description.abstract© 2019, School of Science. Inaccurate taxonomic placement of fossils can lead to the accumulation of errors in molecular clock studies and their generated evolutionary lineages. There are limited fossil data that can be used in divergence time estimations. Therefore, reliable morphological characterization and taxonomical identification of fossil fungi are extremely important. Most fossils of Dothideomycetes and Sordariomycetes are from the early Cenozoic (66–23 Mya), with fewer from the late Mesozoic (174–145 Mya). However, it is hard to distinguish some fossil descriptions as photographs and illustrations are unclear; thus, the validity of using these fossils in calibrations of molecular clocks is problematic. This study brings scattered paleobiological data on selected fossil Ascomycota, using descriptions, fossil images and illustrations, coupled with recent age estimations, and taxonomic and phylogenetic affinity of extant species. As an integrated approach, this study summarizes a historical fossil outline with a reliable minimum age for 16 calibrating points viz. crown of Aigialus, Anzia, Aspergillus, Asterina, Calicium chlorosporum–C. nobile, Capnodiales, Chaenotheca, Colletotrichum, Diaporthales, Meliola, Ophiocordyceps, Microthyriales, Microthyrium, Muyocopron, Pezizomycotina and Stigmatomyces. A scheme of Ascomycota ancient lineages is also provided in order to improve divergence time estimations.en_US
dc.subjectAgricultural and Biological Sciencesen_US
dc.subjectEnvironmental Scienceen_US
dc.titleDivergence time calibrations for ancient lineages of Ascomycota classification based on a modern review of estimationsen_US
dc.typeJournalen_US
article.title.sourcetitleFungal Diversityen_US
article.volume96en_US
article.stream.affiliationsMae Fah Luang Universityen_US
article.stream.affiliationsKunming Institute of Botany Chinese Academy of Sciencesen_US
article.stream.affiliationsManaaki Whenua - Landcare Researchen_US
article.stream.affiliationsUniversity of Electronic Science and Technology of Chinaen_US
article.stream.affiliationsNational Taiwan Universityen_US
article.stream.affiliationsShenzhen Universityen_US
article.stream.affiliationsChiang Mai Universityen_US
article.stream.affiliationsGuizhou Academy of Agricultural Sciencesen_US
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