Hercynella gigantea Community, Early Emsian, Polar Urals: Early/Lower Emsian, Russian Federation

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Anthozoa - Favositida - Favositidae
Squameofavosites sp. Chernyshev 1941
Favosites stellaris
Pachyfavosites sp. Sokolov 1952
Crinoidea - Cyathocrinida - Cupressocrinitidae
Cupressocrinites sp. Goldfuss 1831
includes crowns
Crinoidea
Cyclocyclicus sp. Yeltysheva 1955
Pentagonocyclicus sp. Yeltysheva and Shevchenko 1960
Gastropoda - Murchisoniina - Palaeozygopleuridae
Palaeozygopleura sp. HornĂ½ 1955
Bivalvia - Cyrtodontida - Antipleuridae
Hercynella gigantea
Hercynella polaris
Hercynella comiensis
Hercynella plana
Hercynella parvula
Hercynella sp. Kayser 1878
Cephalopoda - Orthocerida - Orthoceratidae
Orthoceratidae indet. M'Coy 1844
Cephalopoda - Pseudorthocerida - Pseudorthoceratidae
Pseudorthoceratidae indet. Flower and Caster 1935
Cephalopoda - Pseudorthocerida - Spyroceratidae
Spyroceras crotalum (Hall 1879)
Xiphosura - Xiphosurida - Belinuridae
Belinurus sp. Bronn 1839
see common names

Geography
Country:Russian Federation
Coordinates: 67.0° North, 65.0° East (view map)
Paleocoordinates:6.3° North, 6.3° East
Basis of coordinate:based on nearby landmark
Geographic resolution:local area
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
Stratigraphic resolution:bed
Stratigraphy comments: Late Early Emsian.
Lithology and environment
Primary lithology:shelly/skeletal "limestone"
Includes fossils?Y
Lithology description: "Occurs in a 3 m thick, algal-coral, organogenic and bioclastic crinoidal limestone patch directly overlying reef limestone belonging to the Fistulella-Ikella Community."
Environment:perireef or subreef
Geology comments: "[Occurrence] indicates that the H. Community formed after the cessation of reef activity, and is a level bottom rather than a reef community. The [specimens] form unevently distributed banks [0.3 to 0.5 m thick and 1-3 m long.] [Most specimens disarticulated.] Condition of ...shells suggests quiet water conditions near wave base, and an assignment to BA 4 is made. It is concluded that bioherm formation ceased, following which there was some basin deepening consequent with the establishement of the H. Community."
Taphonomy
Collection methods and comments
Reason for describing collection:paleoecologic analysis
Metadata
Also known as:Reef 2249
Database number:24775
Authorizer:M. Foote Enterer:M. Foote
Modifier:U. Merkel Research group:marine invertebrate
Created:2002-08-20 07:10:09 Last modified:2008-07-02 05:29:54
Access level:the public Released:2002-08-20 07:10:09
Creative Commons license:CC BY
Reference information

Primary reference:

6753. V. P. Sapelnikov, O. V. Bogoyavlenskaya, L. I. Mizens and V. P. Shuysky. 1999. Silurian and Early Devonian benthic communities of the Ural-Tien Shan region. In A. J. Boucot and J. D. Lawson (eds.), Paleocommunities--a case study from the Silurian and Lower Devonian 510-544 [M. Foote/M. Foote/M. Foote]