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Sphenophytes or Articulates are a group of spore plants with articulated axes and leaves standing in whorls. Fructifications typically consist of strobili. Sphenophytes were widespread in the Carboniferous and Early Permian. Two major groups can be distinguished, the Calamitales and the Sphenophyllales. The calamites were rhizome-borne trees with secondary growth which could reach a height of up to 20 m. Most species are indicative for humid to wet environments. They often occurred in monotypic stands along the shorelines of lakes and rivers, probably comparable to modern reed vegetations. The name Calamites was originally given to pith casts of the hollow stems, but is now also used for the whole plant. Annularia and Asterophyllites are two types of calamite foliage. The sphenophylls were herb-like plants with typical wedge-shaped leaves arranged in whorls. The only living sphenophyte is the modern Equisetum or horsetail.
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Calamites is a genus for the stems of fossil giant horsetails. The genus has been established for the pith casts, the natural infillings of the hollow central parts of the stem. The stems are articulated and have nodes and internodes. Calamites shows characteristic ribs which normally alternate at the nodes. The pithcasts only give an idea about the diameter of the internal cavity of the stem, not about the diameter of the stem itself ! Outer stem surfaces are rare. The generic name is also used for permineralized stems, e.g. in coal balls. Many species have been described. However, the taxonomy is rather confusing. | ||||
Calamites carinatus | Plant fossils from the Northen Anthracite Field |
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Calamites cistii | Plant fossils from the Northen Anthracite Field |
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Calamites cistii | M. Hieb's Plant Fossils of West Virginia |
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Calamites cistii | M. Hieb's Plant Fossils of West Virginia |
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Calamites cistii | M. Hieb's Plant Fossils of West Virginia | branching axes |
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Calamites | M. Hieb's Plant Fossils of West Virginia | outer surface with branch scars |
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Calamites sp. | Mazon Creek Exhibit, Illinois State Museum |
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Calamites sp. | Kansas Fossils, Geology Museum, Emporia State University | |||
Calamites | Collection Jens-Wilhelm Janzen |
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Calamites | Kathleen Pigg's "Plant Fossils and Evolution" |
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C alamites | R.A. Spicer, The Open University, Milton Keynes |
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Calamites | Manny's Fossil Gallery |
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Calamites | Manny's Fossil Gallery |
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Calamites | Botanical Society of America: Online Image Collection | coal ball: longitudinal section |
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Calamites | Botanical Society of America: Online Image Collection | as above; high resolution image |
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Calamites | Botanical Society of America: Online Image Collection | coal ball: cross section |
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Calamites | Botanical Society of America: Online Image Collection | as above; high resolution image |
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Calamites | Botanical Society of America: Online Image Collection | coal ball: cross section |
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Calamites | Botanical Society of America: Online Image Collection | as above; high resolution image |
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Calamites | Botanical Society of America: Online Image Collection | coal ball: cross section |
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Calamites | Botanical Society of America: Online Image Collection | as above; high resolution image |
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Annularia is a genus for calamitalean foliage. The narrow lancet-like Annularia leaves are placed in whorls, positioned at the nodes. All leaves lie in one plane and the whorls are circular to oval in outline. Several dozens of species are distinguished, some of them being valuable index fossils. | ||||
Annularia radiata | M. Hieb's Plant Fossils of West Virginia |
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Annularia radiata | M. Hieb's Plant Fossils of West Virginia |
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Annularia mucronata | Plant fossils from the Northen Anthracite Field |
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Annularia stellata | Plant fossils from the Northen Anthracite Field |
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Annularia sp. | Mazon Creek Exhibit, Illinois State Museum |
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Annularia sp. | Kansas Fossils, Geology Museum, Emporia State University | |||
Annularia | Collection Jens-Wilhelm Janzen |
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Annularia sphenophylloides | Kathleen Pigg's "Plant Fossils and Evolution" |
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Asterophyllites is another type of calamitalean foliage. The narrow needle-shaped leaves are also positioned in whorl inserted at the nodes but all leaves are directed towards the apex of the shoot. The leaf whorls are laterally compressed. Some of the Asterophyllites species are valuable index fossils. | ||||
Asterophyllites equisetiformis | Mazon Creek Exhibit, Illinois State Museum |
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Asterophyllites charaeformis | M. Hieb's Plant Fossils of West Virginia |
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Asterophyllites equisiteformis | M. Hieb's Plant Fossils of West Virginia |
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Asterophyllites equisetiformis | Natural History Museum, Maastricht, The Netherlands |
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Asterophyllites equisetiformis | Kathleen Pigg's "Plant Fossils and Evolution" |
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Asterophyllites | Collection Jens-Wilhelm Janzen |
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Asterophyllites | Botanical Society of America: Online Image Collection | coal ball material |
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Asterophyllites | Botanical Society of America: Online Image Collection | coal ball material |
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Calamostachys is a genus that has been defined for one of the fructification types of Calamitaleans. The stobilus axes are articulated like all the other axial parts of the plant and bear bracts at the nodes. The sporophylls holding the sporangia are inserted in between on the internodes. The exact mode of attachment of the sporophylls is often difficult to recognise in compression material. | ||||
Calamostachys sp. | M. Hieb's Plant Fossils of West Virginia |
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Calamostachys | M. Hieb's Plant Fossils of West Virginia |
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Calamostachys | Collection Jens-Wilhelm Janzen |
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Calamostachy binneyana | Botanical Society of America: Online Image Collection | coal ball: cross section |
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Calamostachys binneyana | Botanical Society of America: Online Image Collection | as above; high resolution image |
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Calamostachy binneyana | Botanical Society of America: Online Image Collection | coal ball: longitudinal section |
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Calamostachs binneyana | Botanical Society of America: Online Image Collection | as above; high resolution image |
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Sphenophyllum is a genus of spore plants with articulated axes and wedge-shaped leaves which are positioned in whorls, inserted at the nodes. Leaf whorls usually hold six leaves. The genus Sphenophyllum was originally established for leaf compressions but is now also used for permineralised axes. In crsoss section the axes show a typical triarch xylem with secondary growth. Sphenophylls were herbaceous plants, at least several species had a scrambling growth habit. The various Sphenophyllum foliage species are valuable index fossils for the Upper Carboniferous and Lower Permian. | ||||
Sphenophyllum cuneifolium | M. Hieb's Plant Fossils of West Virginia |
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Sphenophyllum cuneifolium | M. Hieb's Plant Fossils of West Virginia |
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Sphenophyllum emarginatum | Plant fossils from the Northen Anthracite Field |
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M. Hieb's Plant Fossils of West Virginia |
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Sphenophyllum | M. Hieb's Plant Fossils of West Virginia |
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Sphenophyllum | M. Hieb's Plant Fossils of West Virginia |
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Sphenophyllum | M. Hieb's Plant Fossils of West Virginia |
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Sphenophyllum | Collection Jens-Wilhelm Janzen |
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Sphenophyllum | Kathleen Pigg's "Plant Fossils and Evolution" | coal ball material: cross section |
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Sphenophyllum plurifoliatum | Botanical Society of America: Online Image Collection | coal ball material: cross section |
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Sphenophyllum plurifoliatum | Botanical Society of America: Online Image Collection | as above; high resolution image |
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Sphenophyllum | Botanical Society of America: Online Image Collection | coal ball material: cross section |
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Sphenophyllum | Botanical Society of America: Online Image Collection | as above; high resolution image |
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Only a single genus of sphenophytes has survived up the present day, Equisetum. All species are herbaceous. The following site gives some information on extant sphenophytes. | ||||
Modern sphenophytes | University of California Museum of Paleontology, Berkeley |
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= excellent ! | = very good |
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The last check of the list of links was done on 25 October
1999. 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 |
October 1999
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