Steemans Philippe, Hérissé Alain Le, Melvin John, Miller Merrell A, Paris Florentin, Verniers Jacques, Wellman Charles H
Palaeobotany, B-18, University of Liège, 4000 Liège, Belgium.
Science. 2009 Apr 17;324(5925):353. doi: 10.1126/science.1169659.
Colonization of the land by plants most likely occurred in a stepwise fashion starting in the Mid-Ordovician. The earliest flora of bryophyte-like plants appears to have been cosmopolitan and dominated the planet, relatively unchanged, for some 30 million years. It is represented by fossilized dispersed cryptospores and fragmentary plant remains. In the Early Silurian, cryptospore abundance and diversity diminished abruptly as trilete spores appeared, became abundant, and underwent rapid diversification. This change coincides approximately with the appearance of vascular plant megafossils and probably represents the origin and adaptive radiation of vascular plants. We have obtained a diverse trilete spore occurrence from the Late Ordovician that suggests that vascular plants originated and diversified earlier than previously hypothesized, in Gondwana, before migrating elsewhere and secondarily diversifying.
植物在陆地上的定殖很可能是从中奥陶世开始以逐步的方式发生的。最早的苔藓类植物群似乎曾遍布全球,并在约3000万年的时间里相对不变地主导着地球。它以化石形式的分散隐孢子和零碎的植物残骸为代表。在志留纪早期,随着三缝孢子的出现、大量繁殖并迅速分化,隐孢子的丰度和多样性突然降低。这一变化大致与维管植物大化石的出现同时发生,可能代表了维管植物的起源和适应性辐射。我们从晚奥陶世获得了多样的三缝孢子出现情况,这表明维管植物在冈瓦纳大陆起源并分化的时间比之前假设的更早,之后迁移到其他地方并再次分化。