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志留纪—早泥盆世维管植物的系统发育、幕式演化和地理分布:植物大化石证据

DOI: 10.7605/gdlxb.2014.06.069, PP. 861-877

Keywords: 早期维管植物,华南,分支演化,辐射,多样性

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Abstract:

尽管近年来对志留纪—早泥盆世陆生维管植物系统发育的认识取得了很大进展,但是目前对多囊蕨类、莱尼蕨类、工蕨类的界定和类群划分尚有分歧,工蕨类和石松类的姐妹群关系仍有疑问,真叶植物基部类群有待深入研究。志留纪至早泥盆世的维管植物演化可划分为2幕,即前布拉格期序幕阶段和布拉格期爆发阶段。维管植物主要分支在第1幕均处于萌芽状态,仅出现个别先驱型分子;第2幕为维管植物分支爆发式演化的主幕。在布拉格期,规则叶序、孢子叶、似叶球状结构等石松类的典型性状最早显现,真叶植物发生明显的分支分化,大型叶及其同源器官(枝叶复合体)多次独立起源,孢子囊和叶性结构的发育相关性在多个支系中趋同演化出现。古植物地理方面,在东北冈瓦纳区的华南地区,工蕨类以孢子囊螺旋排列的类型为主,真叶植物在布拉格期显示出高度的多样性和分异度;在劳俄区,工蕨类中孢子囊成列排列的类型较为丰富,真叶植物的大量出现要晚于华南地区。羊角蕨纲、拟库克逊蕨类、莱尼蕨目的分支演化可能主要发生在南劳俄和西北冈瓦纳等中、高纬度地区。工蕨类、石松类和真叶植物的分支演化和地理辐射可能遵循“走出热带”模式,它们在低纬度地区最早发生分化并快速辐射;维管植物主要分支在布拉格期的爆发式演化,主要是热带植物群革新演化的贡献。

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