Lynna River valley, A. raniceps zone: Kunda, Russian Federation
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
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Porambonites costata
Pander 1830
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Lingulata
- Lingulida
- Pseudolingulidae
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Pseudolingula sp.
Mickwitz 1909
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Strophomenata
- Billingsellida
- Gonambonitidae
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Gonambonites sp.
Pander 1830
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Strophomenata
- Billingsellida
- Clitambonitidae
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Hemipronites imbricata
(Opik 1934)
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Strophomenata
- Billingsellida
- Polytoechiidae
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Antigonambonites planus
(Pander 1830)
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Gonambonites plana | |||||||
Strophomenata
- Strophomenida
- Taffiidae
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Ukoa ornata
Öpik 1932
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Pedersen and Rasmussen 2019 | ||||||
Strophomenata
- Strophomenida
- Plectambonitidae
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Ingria sp.
Öpik 1930
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Rhynchonellata
- Orthida
- Paurorthidae
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Paurorthis parva
(Pander 1830)
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Orthambonites parva | |||||||
Rhynchonellata
- Orthida
- Lycophoriidae
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Lycophoria sp.
Lahusen 1885
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Rhynchonellata
- Orthida
- Orthidae
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Orthambonites sp.
Pander 1830
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Orthambonites cf. majuscula
Rubel 1961
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Orthambonites calligramme
(Dalman 1828)
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Rhynchonellata
- Pentamerida
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Syntrophiidina indet.
Ulrich and Cooper 1936
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see common names |
Geography
Country: | Russian Federation | State/province: | St. Petersburg |
Coordinates: | 60.0° North, 32.6° East (view map) | ||
Paleocoordinates: | 35.6° South, 1.9° East | ||
Basis of coordinate: | stated in text | ||
Geographic resolution: | outcrop |
Time
Period: | Ordovician | Epoch: | Middle Ordovician |
10 m.y. bin: | Ordovician 2-3 | ||
Key time interval: | Kunda | Trilobite zone: | Asaphus raniceps |
Age range of interval: | 467.10000 - 462.90000 m.y. ago |
Stratigraphy
Formation: | Sillaoru | Member: | Lopukhinka | ||
Regional section: | Bed | Regional bed: | Bed 0- -II | ||
Regional order: | bottom to top | ||||
Stratigraphic resolution: | group of beds | ||||
Stratigraphy comments: Boundary Marl. |
Lithology and environment
Primary lithology: | gray,red claystone |
Secondary lithology: | glauconitic,ooidal,gray argillaceous "limestone" |
Lithology description: "The Sillaoru Formation is here probably only represented by the Lopukhinka Member (Dronov, 1997), some 50 cm thick. The lower 10 cm is a red to grey clay bed with almost no iron ooliths. Above this follows a light grey argillaceous limestone with some glauconite and iron ooliths.", in Rasmussen & Harper (2008) | |
Environment: | marine indet. |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils,mesofossils |
Collection methods and comments
Collection methods: | field collection |
Reason for describing collection: | taxonomic analysis |
Metadata
Database number: | 191361 | ||
Authorizer: | B. Kröger, P. Wagner | Enterer: | B. Kröger, P. Wagner |
Modifier: | P. Wagner | ||
Created: | 2018-01-23 12:41:23 | Last modified: | 2019-08-13 11:09:59 |
Access level: | the public | Released: | 2018-01-23 12:41:23 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
64540. | C. M. O. Rasmussen and D. A. T. Harper. 2008. Resolving early Mid-Ordovician (Kundan) bioevents in the East Baltic based on brachiopods. Geobios 41:533-542 [B. Kröger/B. Kröger] |
Secondary references:
69737 | M. Pedersen and C. M. Ø Rasmussen. 2019. The glacially induced Middle Ordovician rise of the Plectambonitoidea (Brachiopoda) and the phylogenetic placement of the Baltic genus Ukoa. Palaeogeography, Palaeoclimatology, Palaeoecology 534 [P. Wagner/P. Wagner/M. Uhen] |