正trichum s.l.和Ulota s.l.(正tricaceae,苔藓植物)的系统发育:气孔进化的新认识

IF 3.7
Qing‐Hua Wang, S. Dong, Jin-Long Zhang, Yang Liu, Yu Jia
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引用次数: 3

摘要

Orthotrichum Hedw。绿藓(Ulota Mohr)和绿藓(Ulota Mohr)是旱生藓科植物中物种最多的两个属。利用3个数据矩阵重构了这两个属的系统发育:(i)细胞体基因组和33个分类群;(ii)来自3个基因组和144个分类群的6个位点;(3) 2个质体位点和163个分类群。目前的系统发育,基于迄今为止最多的基因或分类群取样,基本上证实了正trichum和雨燕属的新分类,并表明除雨燕属外,所有的雨燕属都属于新分类。,形成一个分支和三个谱系,包括隐孔正trichum分支。我们提供了新的形态学特征,支持这两个属的目前划分。气孔的祖先状态重建表明,土藓属植物的浅孔具有多形特征,半浸入式气孔由浸入式气孔演化而来。赤杨的浸没气孔独立出现过一次,而半浸没气孔可能出现过多次。分子测年分析表明,浸没式气孔的出现可能与渐新世早期至中新世晚期的干旱环境有关,而半浸没式气孔的出现可能与中新世中期至上新世的半干旱或半干旱环境有关。生境的祖先状态重建表明,土生生境是一种非胚性的、多次独立进化的生境,支持了前者的假设。从形态统计学角度考虑,土藓属植物隐孔的发育可能增强了其对干旱生境的适应能力,并可能促进其在进化过程中的生境转移。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Phylogeny of Orthotrichum s.l. and Ulota s.l. (Orthotrichaceae, Bryophyta): Insights into stomatal evolution
Orthotrichum Hedw. s.l. and Ulota Mohr s.l. are two of the most speciose genera of the xerophytic moss family Orthotrichaceae. We reconstructed the phylogeny of these two genera using three data matrices: (i) organellar genomes and 33 taxa; (ii) six loci from three genomes and 144 taxa; and (iii) two plastid loci and 163 taxa. The present phylogeny, based on the maximum sampling of genes or taxa to date, generally confirms the new classification of Orthotrichum and Ulota, and indicated that all Ulota species, except Ulota phyllantha Brid., form a clade and three lineages comprise the cryptoporous Orthotrichum clade. We provided new morphological characters that support the present division of the two genera. Ancestral state reconstruction of stoma indicates that superficial stomata in Orthotrichum represent a plesiomorphic character and semi‐immersed stomata were derived from immersed stomata. The results also suggest that immersed stomata independently arose once in Orthotrichum, whereas semi‐immersed stomata probably arose more than once. Molecular dating analysis reveals that the occurrence of immersed stomata is probably related to arid environments during the early Oligocene to late Miocene, whereas the appearance of semi‐immersed stomata might be associated with the mesic–xeric or semiarid environments during the middle Miocene to Pliocene. Ancestral state reconstruction of habitat indicates that the saxicolous habitat is apomorphic and independently evolved multiple times in Orthotrichum and Ulota, which supports the former hypothesis. Considering morphological statistics, the development of the cryptopore in Orthotrichum could provide increased resilience to dry habitats, and might promote their habitat shift during evolution.
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