M Shell Bed: Middle Triassic - Anisian, China
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Rhynchonellata
- Spiriferinida
- Mentzeliidae
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Mentzelia mentzeli
(Dunker 1851)
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38 specimens | ||||||
Madoia sp.
Sun and Ye 1982
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73 specimens | ||||||
Rhynchonellata
- Spiriferinida
- Sinucostidae
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Sinucosta sp.
Dagys 1963
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38 specimens | ||||||
Rhynchonellata
- Spiriferinida
- Spiriferellinidae
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Pseudospiriferina multicostata
Yang and Xu 1966
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Rhynchonellata
- Rhynchonellida
- Cyclothyrididae
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Septaliphoria sinensis
Yang and Xu 1966
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23 specimens | ||||||
recombined as Costirhynchopsis sinensis | |||||||
Rhynchonellata
- Rhynchonellida
- Norellidae
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Diholkorhynchia sinensis
(Koken 1910)
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11 specimens | ||||||
Nudirostralina minima
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Costinorella sp.
Dagys 1974
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Rhynchonellata
- Rhynchonellida
- Erymnariidae
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Crurirhynchia subssicostata
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9 specimens | ||||||
Rhynchonellata
- Terebratulida
- Zeilleriidae
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Aulacothyris angustaeformis
Yang and Xu 1966
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35 specimens | ||||||
recombined as Sacothyris angustaeformis | |||||||
Rhynchonellata
- Terebratulida
- Angustothyrididae
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Rhaetina angustaeformis
(Boekh 1872)
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55 specimens | ||||||
recombined as Angustothyris angustaeformis | |||||||
see common names |
Geography
Country: | China | State/province: | Guizhou |
Coordinates: | 26.3° North, 106.7° East (view map) | ||
Paleocoordinates: | 13.3° North, 95.1° East | ||
Basis of coordinate: | stated in text | ||
Geographic resolution: | small collection |
Time
Period: | Triassic | Epoch: | Middle Triassic |
10 m.y. bin: | Triassic 2 | ||
Key time interval: | Middle Triassic - Anisian | ||
Age range of interval: | 247.20000 - 237.00000 m.y. ago |
Stratigraphy
Formation: | Qingyan | Member: | Yingshangpo | ||
Stratigraphic resolution: | group of beds | ||||
Stratigraphy comments: The Middle Triassic succession at Qingyan is lithologically divided into the Qingyan and Guiyang Formations. The Qingyan Formation is an 890 m-thick succession composed of five members: Xiaoshan, Mafengpo, Yingshangpo, Leidapo and Yuqing Members in ascending order. The Xiaoshan Member is dominated by grey medium- bedded limestone; the Mafengpo Member consists of dark mudstone; the Yingshangpo Member is composed of grey medium-bedded bioclastic limestone interbedded with black shale; and the Leidapo Member is characterized by black mudstone in the lower part and calcareous mudstone in the upper part. |
Lithology and environment
Primary lithology: | gray lithified wackestone |
Secondary lithology: | black lithified packstone |
Includes fossils? | Y |
Lithology description: the Yingshangpo Member is composed of grey medium-bedded bioclastic limestone interbedded with black shale. Brachiopod skeletal packstone-wackestone. | |
Environment: | intrashelf/intraplatform reef |
Geology comments: Qingyan was situated on a shallow carbonate bank, the junction between the carbonate platform in the north and west and a deep basin in the south and east during the Early and Middle Triassic times |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Temporal resolution: | snapshot |
Collection methods and comments
Collection excludes: | some macrofossils |
Collection methods: | surface (in situ),mechanical,field collection |
Collection size: | 400 specimens |
Reason for describing collection: | paleoecologic analysis |
Collection method comments: Brachiopod specimens statistically studied in this paper were obtained from one shell slab, 45 cm x 25 cm x 10 cm, of the Yingshangpo Member and another shell slab, 60 cm x 30 cm x 5 cm, of the Leidapo Member at the Qingyan section. |
Metadata
Database number: | 111833 | ||
Authorizer: | N. Bonuso | Enterer: | N. Bonuso |
Modifier: | N. Bonuso | Research group: | marine invertebrate |
Created: | 2011-06-29 04:38:45 | Last modified: | 2011-06-28 15:02:49 |
Access level: | the public | Released: | 2011-06-29 04:38:45 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
36557. | J. Chen, Z. Chen, and J. Tong. 2010. Palaeoecology and taphonomy of two brachiopod shell beds from the Anisian (Middle Triassic) of Guizhou, Southwest China: Recovery of benthic communities from the end-Permian. Global and Planetary Change 73:149-160 [N. Bonuso/N. Bonuso] |