
Cordaitales are an extinct order of gymnosperms, known from the early Carboniferous to the late Permian. Many Cordaitales had elongated strap-like leaves, resembling some modern-day conifers of the Araucariaceae and Podocarpaceae. They had cone-like reproductive structures reminiscent of those of modern conifers. Some Cordaitales formed large trees that seem to have been particularly abundant on drier ground, in tropical environments. Also, some tall trees but also shrubby and mangrove-like species of Cordaitales seem to have grown in the Carboniferous coal swamps. Cordaitales were also abunda
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科达目(Cordaitales)是一目灭绝的木本植物,可能是早期的针叶树,也可能是其他针叶树、银杏和苏铁的祖先。 它们具有像现代针叶树那样的锥状生殖结构。 科达目在石炭纪时期出现,并形成了大型树木,它们的数量在干燥的地面上和热带环境中似乎特别丰富。 此外,一些高大的科达目树木,以及灌木状和红树林状的科达目植物似乎在石炭纪煤炭沼泽中生长。 在二叠纪期间,科达目也很丰富,但在三叠纪期间它们变得不那么重要,并在期间消失。 许多科达目植物长有细长的带状叶子,类似于南洋杉科和罗汉松科的一些现代针叶树。 来自石炭纪的常见属包括Mesoxylon和科达属,其他属是Noeggerathiopsis和Sumaropsis。
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Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).