Lazurnaya Bay Fm (upper part) - South Primorye: Olenekian, Russian Federation
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Cephalopoda
- Nautilida
- Grypoceratidae
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Gyronautilus praevolutum
(Kiparisova 1961)
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recombined as Gyronautilus praevolutus | |||||||
Cephalopoda
- Ceratitida
- Hedenstroemiidae
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Hedenstroemia sp.
Waagen 1895
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Cephalopoda
- Ceratitida
- Prionitidae
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Meekoceras subcristatum
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Meekoceras boreale
Diener 1895
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Rhynchonellata
- Rhynchonellida
- Rhynchonellidae
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Abrekia sulcata
Dagys 1974
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Lingulata
- Lingulida
- Lingulidae
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Lingula borealis
Bittner 1899
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recombined as Lingularia borealis | |||||||
see common names |
Geography
Country: | Russian Federation |
Coordinates: | 42.9° North, 132.3° East (view map) |
Paleocoordinates: | 43.6° North, 110.4° East |
Basis of coordinate: | estimated from map |
Geographic resolution: | local area |
Time
Period: | Triassic | Epoch: | Early/Lower Triassic |
Stage: | Olenekian | 10 m.y. bin: | Triassic 1 |
Key time interval: | Olenekian | ||
Age range of interval: | 251.20000 - 247.20000 m.y. ago |
Stratigraphy
Formation: | Lazurnaya Bay | ||||
Regional section: | Abrek Bay | ||||
Stratigraphic resolution: | formation | ||||
Stratigraphy comments: STRATIGRAPHIC RELATIONS: Lower Triassic strata in region are lithostratigraphically divided into the Lazurnaya Bay and Zhitkov Formations in an upward sequence. The Lazurnaya Bay Fm unconformably overlies the Permian Abrek Fm. THICKNESS: The Lazurnaya Bay Fm is 57.9 m thick in the Abrek Bay region. AGE: Contains an assemblage that suggest the lower Olenekian (lower part of the Hedenstroemia bisphorensis Zone) in the upper part of the formation, overlying upper Induan age sediments. The Induan/Olenekian boundary is located at 55 m above the base of the formation. |
Lithology and environment
Primary lithology: | fine,shelly/skeletal,gray lithified calcareous sandstone |
Includes fossils? | Y |
Lithology description: GENERAL LITHOLOGY: Gray, fine-grained, bedded sandstone, with lenses of coquinoid calcareous sandstone. LITHIFICATION: Lithified, based on observation of figured specimens. | |
Environment: | coastal indet. |
Geology comments: ENVIRONMENT: No environmental data reported. Assigned to Siliciclastic coastal indet. on the basis of facies. TECTONIC SETTING: No tectonic data reported in text. SEQUENCE STRATIGRAPHY: No sequence stratigraphic data reported in text. |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Preservation of anatomical detail: | poor |
Collection methods and comments
Collection methods: | field collection |
Reason for describing collection: | taxonomic analysis |
Collection method comments: COLLECTOR: Collection is a composite based on several workers, none of which are named. REPOSITORY: NSM (National Science Museum, Tokyo); CGM ? | |
Taxonomic list comments:COMPLETENESS: Not exhaustive (as compiled from previous workers first hand accounts), but fairly complete. NOMENCLATURE: Authoritative text, modern nomenclature. Presumably nomenclature of taxa listed from older collections has been revised. |
Metadata
Database number: | 61959 | ||
Authorizer: | A. Hendy | Enterer: | A. Hendy |
Modifier: | A. Hendy | Research group: | marine invertebrate |
Created: | 2006-07-08 19:45:56 | Last modified: | 2013-11-25 13:37:23 |
Access level: | the public | Released: | 2006-07-08 19:45:56 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
17926. | Y.D. Zakharov and Y. Shigeta. 2000. Gyronautilus, a new genus of Triassic Nautilida from South Primorye, Russia. Paleontological Research 4(4):231-234 [A. Miller/A. Hendy] |