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首页> 外文期刊>American journal of botany >Character evolution of modern fly-speck fungi and implications for interpreting thyriothecial fossils
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Character evolution of modern fly-speck fungi and implications for interpreting thyriothecial fossils

机译:现代飞标真菌的性格演变及解释硫代硫型化石的影响

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Premise Fossils show that fly-speck fungi have been reproducing with small, black thyriothecia on leaf surfaces for ~250 million years. We analyzed morphological characters of extant thyriothecial fungi to develop a phylogenetic framework for interpreting fossil taxa. Methods We placed 59 extant fly-speck fungi in a phylogeny of 320 Ascomycota using nuclear ribosomal large and small subunit sequences, including newly determined sequences from nine taxa. We reconstructed ancestral character states using BayesTraits and maximum likelihood after coding 11 morphological characters based on original observations and literature. We analyzed the relationships of three previously published Mesozoic fossils using parsimony and our morphological character matrix, constrained by the molecular phylogeny. Results Thyriothecia evolved convergently in multiple lineages of superficial, leaf-inhabiting ascomycetes. The radiate and ostiolate scutellum organization is restricted to Dothideomycetes. Scutellum initiation by intercalary septation of a single hypha characterizes Asterinales and Asterotexiales, and initiation by coordinated growth of two or more adjacent hyphae characterizes Aulographaceae. Scutella in Microthyriales are initiated apically on a lateral hyphal branch. Patterns of hyphal branching in scutella contribute to distinguishing among orders. Parsimony resolves three fossil taxa as Dothideomycetes; one is further resolved as a member of a Microthyriales-Zeloasperisporiales clade within Dothideomycetes. Conclusions This is the most comprehensive systematic study of thyriothecial fungi and their relatives to date. Parsimony analysis of the matrix of character states of modern taxa provides an objective basis for interpreting fossils, leading to insights into morphological evolution and geological ages of Dothideomycetes clades.
机译:前提化石表明,飞斑真菌在叶面上繁殖,叶面〜2.5亿年。我们分析了现存硫卓氏菌真菌的形态特征,开发了解释化石分类群的系统发育框架。方法使用核核糖体大小和小亚基序列,在320 ascoycota的系统发育中放置59个菌蝇斑真菌,包括来自九个征集的新确定序列。我们在基于原始观察和文献的编码后,使用拜访者和最大可能性重建了祖传人物状态。我们使用分子系统约束,分析了三个先前公布的中生代化石的关系,由分子系统约束。结果Thyriothecia在肤浅的叶片依偎的多种谱系中融化。辐射和中司酸盐菌组织仅限于Doothideomycetes。单个菌线的静脉内荚膜的颈氏鳞状引发特征在一起,并且通过两种或多种相邻菌丝的协调生长引发的αssterinales和αsertotexial表征AUTORALCEAE。微观reliales中的Scutella在横向螺旋分支上是顶部的。 Scutella的亚腿分支模式有助于区分订单。分公司将三个化石分类群分解为DaThideomycetes;一种进一步被解析为Dirthothideycetes内的微观rsiales-Zeloasperisporiales的成员。结论这是迄今为止司艺真菌及其亲属的最全面的系统研究。现代分类群地区品质矩阵的分析分析为解释化石提供了客观基础,导致达陈胺霉菌的形态演化和地质年龄的见解。

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