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UNIVERSITY MÜNSTER |
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Ferns were widespread in the Carboniferous and Permian. Many had a tree-like growth habit like modern tropical tree ferns. However, though superficially looking very similar, modern tree ferns are not directly related to Palaeozoic forms. The classification of fossil ferns is very difficult and many aspects are still uncleared. Several classification schemes have been published. A major problem is the often fragmentary nature of the material. Some groups are exclusively based on anatomically preserved axes, whereas foliage and fructifications are still unknown. Another problem is that the systematics of ferns is largely based on modern representatives and Palaeozoic forms often do not fit well is this very tight scheme.
Most groups of Palaeozoic ferns are extinct. The Marattiales and the Osmundales are the oldest still existing fern groups and date back to the Late Carboniferous respectively Permian. It should be realised that the vast majority of extant ferns belongs to groups that have evolved in the Mesozoic. The Polypodiaceae, the most succesful fern group today, is even much younger and dates from the Late Cretaceous our Tertiary.
Palaeozoic ferns had various growth strategies ranging from tree-like, to winding, climbing and epiphytic forms. Together with the pteridosperms they probably formed a closed canopy below the upper, rather open canopy of arborescent lycopod trees. After the extinction of most arborescent lycopods in the latest Westphalian, tree ferns became the dominant group of plants. North American Stephanian coals may consist of up to 75% of tree fern remains. Keeping this in mind, it is remarkable that illustrations of fossil ferns are rather scarce on the internet.
Sometimes it is very difficult to distinguish true fern foliage from seed fern foliage; especially when fructifications are still unknown. In such cases fern(-like) foliage is accommotated in the informal category pteridophylls.
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| Psaronius is a genus for anatomically preserved tree fern stems of Late Carboniferous-Permian Marattiales. Late Palaeozoic Marattiales were real tree ferns unlike the modern representatives of this group. Psaronius stems typically have a well-developed root mantle which gives them stability. Foliage of Psaronius is of the Pecopteris type; Scolecopteris is a typical fertile form. This was one of the most common, widespread and diverse groups of ferns during the latest Carboniferous. They prefered humid habitats and were part of peat-forming communities. | ||||
| Psaronius | Virtual Paleobotany Laboratory |
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| Psaronius | Virtual Paleobotany Laboratory | root mantle |
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| Psaronius | K. Pigg's "Plant Fossils and Evolution" |
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| Psaronius | K. Pigg's "Plant Fossils and Evolution" | cross sections |
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| Psaronius | Ulrich Dernbach |
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| Psaronius roots | Ohio State Univ. Lima |
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| Psaronius hexagonus | ? | click on image to enlarge |
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| Psaronius melanedrus | Paläobotanik Münster |
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| Tietea singularis | Ulrich Dernbach | a tree fern stem from Brazil | ||
| Pecopterisand the genera Asterotheca, Scolecopteris established for fertile material | ||||
| Pecopteris sp. | Illinois State Mus., Mazon Creek Fossils |
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| Pecopteris | Virtual Paleobotany Laboratory |
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| Pecopteris | Virtual Paleobotany Laboratory |
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| Pecopteris arborescens | Southern Illinois Univ. Museum |
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| Pecopteris mazoniana | Southern Illinois Univ. Museum |
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| Pecopteris mazoniana | Southern Illinois Univ. Museum |
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| Pecopteris mazoniana | Southern Illinois Univ. Museum |
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| Pecopteris miltonii | M. Hieb's Plant Fossils of W. Virginia |
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| Pecopteris plumosa | Geol. Dienst NRW Krefeld |
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| Pecopteris arborescens | SOES Collection |
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| Pecopteris arborescens | Fossil Guy |
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| Pecopteris sp. | Hans Steur's Paleobotany Pages | |||
| Pecopteris | M. Hieb's Plant Fossils of W. Virginia | |||
| Pecopteris | M. Hieb's Plant Fossils of W. Virginia | |||
| Pecopteris | M. Hieb's Plant Fossils of W. Virginia | |||
| Pecopteris | M. Hieb's Plant Fossils of W. Virginia |
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| Pecopteris | Virtual Paleobotany Laboratory | coal ball |
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| Pecopteris | Emporia State University |
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| Pecopteris | SOES Collection |
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| P. (Senftenbergia) plumosa | Westphalian D of Zwickau |
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| Asterotheca sp. | Illinois State Mus., Mazon Creek Fossils |
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| Scolecopteris | Ohio State University Lima | coal ball |
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| Scolecopteris (P.) mertensiodes | Westphalian D of Zwickau | type specimen |
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| Ptychocarpus (P.) unita | Westphalian D of Zwickau | identification probably incorrect |
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| Several other groups of ferns and fern-like plants have been described from Palaeozoic rocks. These include the fern-like Cladoxylales, the Zygopteridales (Coenopteridales) and true ferns like the Botryopteridaceae and Anachoropteridaceae. Because their classification the systematics are still being discussed, they are here placed in a single category; where possible affinities are indicated under comments. | ||||
| Alloiopteris coralloides | M. Hieb's Plant Fossils of W. Virginia | Zygopteridales | ||
| Alloiopteris coralloides | M. Hieb's Plant Fossils of W. Virginia |
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| Alloiopteris coralloides | Westphalian D of Zwickau | listed as Saccopteris |
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| Anachoropteris involuta | Paläobotanik Münster | coal ball - Anachoropteridaceae |
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| Ankyropteris | K. Pigg's "Plant Fossils and Evolution" | coal ball - Tedeleaceae |
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| Botryopteris | Ohio State University Lima | coal ball - Botryopteridaceae |
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| Etapteris | Virtual Paleobotany Laboratory | coal ball - Zygopteridales |
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| Oligocarpia gutbieri | Westphalian D of Zwickau |
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| Pseudosporochnus | Virtual Paleobotany Laboratory | Cladoxylales |
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| Saccopteris cristata | Westphalian D of Zwickau | Zygopteridales (Alloiopteris) |
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| Stauropteris | Virtual Paleobotany Laboratory | coal ball - Stauropteridales |
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| Guairea carnieri | Ancient microworlds | Osmundaceae - Permian |
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The last check of the list of links was done on 2 December
2002. The links give the most direct connections to pictures available
on the web; in many cases they are from sites that have additional palaeobotanical
information. The above ratings refer to:
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| © Forschungsstelle für Paläobotanik, Westfälische Wilhelms-Universität Münster |
December 2002
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