Karadon Formation: Carboniferous, Turkey
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
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Lonchopteridium karvinese
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Paripteris linguaefolia
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Sphenopteridae
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Sphenopteris artemisiaefolioides
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Polypodiopsida
- Equisetales
- Calamitaceae
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Asterophyllites sp.
Brongniart 1828
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Calamites sp.
Suckow 1784
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Polypodiopsida
- Equisetales
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Annularia jongmansi
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Polypodiopsida
- Hymenophyllales
- Hymenophyllaceae
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Eusphenopteris cf. obtusiloba
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Eusphenopteris schumannii
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Eusphenopteris sauveuri
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Pteridopsida
- Filicales
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Palmatopteris sturi
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Pteropsida
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Alethopteris davreuxi
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spelled with current rank as Pecopteris (Alethopteris) | |||||||
unclassified
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? Karinopteris andraeana
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Medullosaceae
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Mariopteris muricata
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Neuropteris obliqua
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Equisetopsida
- Sphenophyllales
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Sphenophyllum emarginatum
(Brongniart 1822)
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Sphenophyllostachys sp.
Seward 1896
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unclassified
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Alloiopteris sp.
Potonie 1897
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Alloiopteris similis
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see common names |
Geography
Country: | Turkey |
Coordinates: | 41.0° North, 31.0° East (view map) |
Paleocoordinates: | 41.0° North, 31.0° East |
Basis of coordinate: | based on nearby landmark |
Time
Period: | Carboniferous |
10 m.y. bin: | Carboniferous 1-5 |
*Period: | Middle Carboniferous - Late/Upper Carboniferous |
Key time interval: | Carboniferous |
Age range of interval: | 358.90000 - 298.90000 m.y. ago |
* legacy (obsolete) database fields |
Stratigraphy
Lithology and environment
Primary lithology: | sandstone |
Lithology description: Dominated by coarse, grey to buff sandstones and conglomerates with coals and subordinate siltstones and mudstones, including some thick clays. Most coals are found in the lower part of the formation. | |
Geology comments: Sequence represents interfingering of coarse sandy braided streams and humid alluvial fans. |
Taphonomy
Modes of preservation: | mold/impression |
Collection methods and comments
Reason for describing collection: | taphonomic analysis |
Collection method comments: The entire formation is a dominantly sandy succession with subordinate shales, pebbly units, and thick coals. Basal part of the formation i s characterized by lacustrine depostis, while the upper parts comprises sequences formed by meandering low sinuosity streams. The coals closely resembles those of the later Westphalian coals of northwestern Europe. |
Metadata
Database number: | 28300 | ||
Authorizer: | R. Gastaldo | Enterer: | J. Allen |
Modifier: | J. Allen | Research group: | paleobotany |
Created: | 2003-02-05 16:00:53 | Last modified: | 2003-07-18 18:05:03 |
Access level: | database members | Released: | 2003-02-05 16:00:53 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
7641. | I.E. Kerey, G. Kelling, and R.H. Wagner. 1985. An outline stratigraphy and palaeobotanical records from the middle Carboniferous rocks of northwestern Turkey. Extrait des Annales de la Societe Geologique du Nord 203-216 [R. Gastaldo/J. Allen/J. Allen] |