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From Wikipedia, the free encyclopedia

Temporal range: Middle Devonian to Early Carboniferous
Eospermatopteris erianus.jpg
Scientific classification e
Kingdom: Plantae
Division: Pteridophyta  (?)
Class: Cladoxylopsida


Incertae sedis:

The cladoxylopsids are a group of plants known only as fossils that are thought to be ancestors of ferns and horsetails.

They had a central trunk, from the top of which several lateral branches were attached. Fossils of these plants originate in the Middle Devonian to Early Carboniferous periods (around 390 to 320 million years ago), mostly just as stems.

Cladoxylopsida contains two orders. The order Hyeniales is now included in Pseudosporochnales.[1]

Intact fossils of the Middle Devonian cladoxylopsid Eospermatopteris show it to have been a tree, the earliest identified in the fossil record as of 2007.

A recent (2017) discovery in Xinjiang in China of early Late Devonian (Frasnian, ca. 374 Ma) silicified fossil cladoxylopsid tree trunks (diameter up to c.70 cm) with preserved cellular anatomy showed an internal arrangement with many xylem bundles in the outer part and none in the interior; each bundle was surrounded by its own cambium layer, by which the tree's trunk widened.[2][3][4]

External links

Links with images:


  1. ^ Thomas N. Taylor, Edith L. Taylor, Michael Krings: Paleobotany. The Biology and Evolution of Fossil Plants . Second Edition, Academic Press 2009, ISBN 978-0-12-373972-8 , p. 387-401, 1028
  2. ^ (Proceedings of the National Academy of Sciences of the United States of America) Unique growth strategy in the Earth’s first trees revealed in silicified fossil trunks from China, by Hong-He Xu, Christopher M. Berry, William E. Stein, Yi Wang, Peng Tang, and Qiang Fu
  3. ^ (with image of trunk cross-section)
  4. ^

Media related to Cladoxylopsida at Wikimedia Commons

This page was last edited on 22 March 2018, at 03:56
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