Vagrania-Leptathyris Comm., Early Emsian, Nanning Area, S. Guangxi: Early/Lower Emsian, China

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Rhynchonellata - Pentamerida - Clorindidae
Pentamerella sp.
Rhynchonellata - Pentamerida - Gypidulidae
? Gypidula sp. Hall 1867
fine ribbed
Rhynchonellata - Rhynchonellida
Rhynchonellida indet. Kuhn 1949
bilobate
Rhynchonellata - Rhynchonellida - Uncinulidae
Uncinulus sp. Bayle 1878
Rhynchonellata - Rhynchonellida - Trigonirhynchiidae
Nymphorhynchia sp. Rzhonsnitskaya 1956
Rhynchonellata - Spiriferida - Xenomartiniidae
? Quadrithyris sp. Havlicek 1957
Rhynchonellata - Spiriferida - Adolfiidae
? Brevispirifer sp.
Rhynchonellata - Atrypida - Atrypidae
Anatrypa sp.
? Desquamatia sp. Alekseeva 1960
Spinatrypa sp. Stainbrook 1951
Atrypa sp. Dalman 1828
Atrypa 1
Atrypa sp. Dalman 1828
Atrypa 2
Rhynchonellata - Atrypida - Karpinskiidae
Vagrania sp.
Rhynchonellata - Atrypida - Carinatinidae
Carinatina sp.
Rhynchonellata - Athyridida - Athyrididae
Leptathyris sp.
Rhynchonellata - Orthida - Schizophoriidae
? Schizophoria sp. King 1850
Strophomenata - Strophomenida - Chonetidae
Chonetidae indet. Bronn 1862
see common names

Geography
Country:China State/province:Guangxi
Coordinates: 22.8° North, 108.3° East (view map)
Paleocoordinates:4.1° North, 126.3° East
Basis of coordinate:based on political unit
Geographic resolution:small collection
Time
Period:Devonian Epoch:Early/Lower Devonian
Stage:Emsian 10 m.y. bin:Devonian 2
*International age/stage:Early/Lower Emsian
Key time interval:Early/Lower Emsian
Age range of interval:407.60000 - 398.30000 m.y. ago
* legacy (obsolete) database fields
Stratigraphy
Stratigraphy comments: "from an unnamed formation in South China"
Lithology and environment
Primary lithology: cherty/siliceous siltstone
Includes fossils?Y
Lithology description: "fossils occur largely as articulated valves in a siliceous siltstone matrix indicating relatively quiet water"
Environment:marine indet.
Geology comments: "Although the community is not well located environmentally in South China, except that it is near the outer limits of the shelly facies-Nandan facies, it may be compared with similar units elsewhere [details follow]....This community belongs in about the BA 3-4 position."
Taphonomy
Collection methods and comments
Reason for describing collection:paleoecologic analysis
Collection method comments: "currently known in South China from only a single small collection"
Metadata
Database number:25866
Authorizer:M. Foote Enterer:M. Foote
Modifier:M. Foote Research group:marine invertebrate
Created:2002-09-26 13:20:44 Last modified:2006-09-15 15:14:05
Access level:the public Released:2002-09-26 13:20:44
Creative Commons license:CC BY
Reference information

Primary reference:

7183. Y. Wang, A. J. Boucot, J.Y. Rong and X.C. Yang. 1987. Community paleoecology as a geologic tool: the Chinese Ashgillian-Eifelian (latest Ordovician through early Middle Devonian) as an example. Geological Society of America Special Paper 211:1-100 [M. Foote/M. Foote/M. Foote]