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革菌目和产生褐腐的伞菌目的各演化支相对年龄的分子系统发育。

Molecular phylogenetics of the Gloeophyllales and relative ages of clades of Agaricomycotina producing a brown rot.

机构信息

Biology Department, Clark University, Worcester, Massachusetts 01610, USA.

出版信息

Mycologia. 2011 May-Jun;103(3):510-24. doi: 10.3852/10-209. Epub 2010 Dec 26.

Abstract

The Gloeophyllales is a recently described order of Agaricomycotina containing a morphologically diverse array of polypores (Gloeophyllum), agarics (Neolentinus, Heliocybe) and resupinate fungi (Veluti-Veluticeps, Boreostereum, Chaetodermella), most of which have been demonstrated to produce a brown-rot mode of wood decay and are found preferentially on coniferous substrates. Multiple phylogenetic studies have included taxa of Gloeophyllales, but none have sampled the order thoroughly, and so far only ribosomal RNA genes have been used. Consequently the limits and higher level placement of the Gloeophyllales are obscure. We obtained sequence data for three protein-coding genes (rpb2, atp6, tef1) and three rRNA regions (nuc-ssu, nuc-lsu, 5.8S) in 19 species of Gloeophyllales representing seven genera and analyzed them together with a diverse set of Agaricomycotina, emphasizing Polyporales. Boreostereum, which is suspected to produce a white rot, is the sister group of the rest of the Gloeophyllales, all of which produce a brown rot. Gloeophyllum contains at least two independent clades, one of which might correspond to the genus Osmoporus. White rot and resupinate fruiting bodies appear to be plesiomorphic in Gloeophyllales. Relaxed molecular clock analyses suggest that the Gloeophyllales arose in the Cretaceous, after the origin of Pinaceae.

摘要

硬皮马勃目是最近描述的伞菌目,包含形态多样的多孔菌(硬皮马勃属)、伞菌(Neolentinus、Heliocybe)和反褶菌(Veluti-Veluticeps、Boreostereum、Chaetodermella),其中大多数被证明具有褐腐木材腐朽模式,主要存在于针叶树上。多项系统发育研究都包括硬皮马勃目的分类群,但没有一个研究能彻底采样该目,到目前为止,仅使用了核糖体 RNA 基因。因此,硬皮马勃目的界限和高级分类位置尚不清楚。我们获得了 19 种硬皮马勃目代表 7 个属的 3 个蛋白质编码基因(rpb2、atp6、tef1)和 3 个 rRNA 区(nuc-ssu、nuc-lsu、5.8S)的序列数据,并与各种伞菌目进行了分析,重点是多孔菌目。Boreostereum 被怀疑产生白腐,它是其余硬皮马勃目的姐妹群,所有这些都产生褐腐。硬皮马勃属包含至少两个独立的分支,其中一个可能对应 Osmoporus 属。白腐和反褶菌果实可能是硬皮马勃目的原始特征。放松的分子钟分析表明,硬皮马勃目起源于白垩纪,在松科起源之后。

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