Upper Upper Kaochaitien Fm, Luoshuichong, Mairang, Wudang, Guiyang, Guizhou Prv.: Sheinwoodian, China
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Bivalvia
- Cyrtodontida
- Cyrtodontidae
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Cyrtodonta sp.
Billings 1858
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Bivalvia
- Modiomorphida
- Modiomorphidae
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Modiomorpha sp.
Hall and Whitfield 1869
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Bivalvia
- Solemyida
- Ctenodontidae
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Ctenodonta sp.
Salter 1852
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Rhynchonellata
- Spiriferida
- Cyrtiidae
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Eospirifer sp.
Schuchert 1913
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Eospirifer cf. radiatus
(Sowerby 1834)
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see common names |
Geography
Country: | China | State/province: | Guizhou | County: | Wudang |
Coordinates: | 26.6° North, 106.8° East (view map) | ||||
Paleocoordinates: | 8.0° North, 127.0° East | ||||
Basis of coordinate: | based on nearby landmark | ||||
Geographic resolution: | local area |
Time
Period: | Silurian | Epoch: | Wenlock |
Stage: | Sheinwoodian | 10 m.y. bin: | Silurian 2 |
Key time interval: | Sheinwoodian | ||
Age range of interval: | 433.40000 - 430.50000 m.y. ago |
Stratigraphy
Formation: | Upper Kaochaitien | ||||
Stratigraphic resolution: | member | ||||
Stratigraphy comments: Except where otherwise stated, ref. 7624 uses Lower Silurian as equivalent to Llandovery, Middle Silurian as equivalent to Wenlock, and Upper Silurian as equivalent to Ludlow plus Pridoli. Upper K. Fm. divided into three parts, and as a whole spans the Late Llandovery to Early Wenlock, according to correlation chart. "The fossils from the middle part correlate with those of the Xiushan Formation. Therefore, the lower part of this formation is correlated with the Rongxi Formation [which is herein regarded as middle Late Llandovery], and the upper part is missing in many areas, but may be correlated with the Huixingshao Formation red beds [which are thought herein to be Wenlock, although with some uncertainty]. These formations are close to the Llandovery-Wenlock boundary, but the fossils do not permit precise zonation." This discussion suggests that a lower part is Late Llandovery, middle part is Llandovery to Wenlock, and upper part is Wenlock. |
Lithology and environment
Primary lithology: | gray,green,red or brown "shale" |
Secondary lithology: | sandstone |
Includes fossils? | Y |
Lithology description: "The upper part consists of gray-green and purplish-red, thin-bedded shale with intercalated fine-grained sandstone, containing [fossils]..." | |
Environment: | marine indet. |
Geology comments: Correlation chart shows shelly-based BA1. |
Taphonomy
Collection methods and comments
Reason for describing collection: | biostratigraphic analysis |
Metadata
Database number: | 27787 | ||
Authorizer: | M. Foote | Enterer: | M. Foote |
Modifier: | M. Foote | Research group: | marine invertebrate |
Created: | 2003-01-09 08:33:47 | Last modified: | 2006-09-13 14:01:03 |
Access level: | the public | Released: | 2003-01-09 08:33:47 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
7624. | E.-z. Mu, A. J. Boucot, X. Chen and J.-y. Rong. 1986. Correlation of the Silurian rocks of China. In A. J. Boucot and W. B. N. Berry (eds.), Geological Society of America Special Paper 202:1-80 [M. Foote/M. Foote/P. Wagner] |