Thaerodonta recedens-Iowacystis sagittaria Comm., Elgin Member, Maquoketa Fm.: Maysvillian, Iowa
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Trilobita
- Phacopida
- Cheiruridae
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Ceraurus sp.
Green 1832
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Trilobita
- Phacopida
- Calymenidae
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Flexicalymene sp.
Shirley 1936
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Trilobita
- Asaphida
- Asaphidae
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Isotelus sp.
Dekay 1824
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Anataphrus sp.
Whittington 1954
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Cephalopoda
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Nautiloidea indet.
Agassiz 1847
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Bivalvia
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Pelecypoda indet.
Goldfuss 1820
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synonym of Bivalvia | |||||||
Rhynchonellata
- Orthida
- Plaesiomyidae
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Plaesiomys subquadrata
(Hall 1847)
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recombined as Plaesiomys subquadratus | |||||||
Rhynchonellata
- Orthida
- Dalmanellidae
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Paucicrura corpulenta
(Sardeson 1892)
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Strophomenata
- Strophomenida
- Furcitellidae
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Megamyonia unicostata
(Meek and Worthen 1868)
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Strophomenata
- Strophomenida
- Sowerbyellidae
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Thaerodonta recedens
(Sardeson 1892)
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unclassified
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Bryozoa indet.
Ehrenberg 1831
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Soluta
- Syringocrinida
- Iowacystidae
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Iowacystis sagittaria
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Myeinocystites sp.
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Crinoidea
- Cupulocrinidae
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Cupulocrinus sp.
d'Orbigny 1849
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Crinoidea
- Porocrinida
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Porocrinus fayettensis
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Carabocrinus slocomi
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Rhombifera
- Pleurocystitidae
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Pleurocystites sp.
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Anthozoa
- Stauriida
- Streptelasmatidae
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Grewingkia sp.
Dybowski 1873
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see common names |
Geography
Country: | United States | State/province: | Iowa |
Coordinates: | 43.1° North, 91.8° West (view map) | ||
Paleocoordinates: | 19.6° South, 61.8° West | ||
Basis of coordinate: | based on political unit | ||
Geographic resolution: | local area |
Time
Period: | Ordovician | Epoch: | Late/Upper Ordovician |
Stage: | Katian | 10 m.y. bin: | Ordovician 5 | *Epoch: | Ashgill | *Local age/stage: | Maysvillian |
Key time interval: | Maysvillian | Graptolite zone: | Amplexograptus manitoulinensis |
Age range of interval: | 450.40000 - 449.80000 m.y. ago | ||
* legacy (obsolete) database fields |
Stratigraphy
Geological group: | Maquoketa | Formation: | Scales Shale | Member: | Elgin |
Stratigraphic resolution: | member | ||||
Stratigraphy comments: "Late Ordovician (Edenian, Upper Caradocian) according to Sloan, 1987: but more likely Maysvillian (Ashgillian) because of the occurrence of Amorphognathus ordovicius." |
Lithology and environment
Primary lithology: | argillaceous wackestone | ||
Includes fossils? | Y | ||
Includes fossils? | Y | ||
Lithology description: "The dominant lithology is moderately fossiliferous thin, wavy-bedded shaley limestones (wackestones to rare grainstone textures) with thin, fossiliferous shale interbeds." | |||
Environment: | deep subtidal ramp | Tectonic setting: | cratonic basin |
Geology comments: Interpreted by authors as shoal margin, BA 4, subject to episodic, strong disturbance (based on numerous compositional and taphonomic features). |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Collection methods and comments
Reason for describing collection: | paleoecologic analysis |
Collection method comments: Some overlap with PBDB collections 23409 and 23521, but not a duplicate entry. |
Metadata
Database number: | 26683 | ||
Authorizer: | M. Foote | Enterer: | M. Foote |
Modifier: | P. Wagner | Research group: | marine invertebrate |
Created: | 2002-10-24 04:44:57 | Last modified: | 2018-03-08 17:15:38 |
Access level: | the public | Released: | 2002-10-24 04:44:57 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
4379. | T. J. Frest, C. E. Brett, and B. J. Witzke. 1999. Caradocian-Gedinnian echinoderm associations of Central and Eastern North America. Paleocommunities--a case study from the Silurian and Lower Devonian 638-783 [M. Foote/K. Koverman/P. Wagner] |