Port Colborne Quarry bioherm: Givetian, Canada

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
Echinodermata indet. Klein 1754
Cyanthophyllum robustum
Brachiopoda indet. Cuvier 1805
Bryozoa indet. Ehrenberg 1831
Gastropoda
Gastropoda indet. Cuvier 1795
tubinate and platyceratid gastropods
Trilobita - Proetida - Proetidae
Dechenella (Dechenella) delphinula (Hall and Clarke 1888)
Stumm 1953
synonym of Dechenella planimarginata
Trilobita - Phacopida - Phacopidae
Phacops cristata Hall 1861
Stumm 1954
recombined as Viaphacops cristatus
Phacops pipa Hall and Clarke 1888
Stumm 1954
recombined as Viaphacops pipa
Phacops canadensis Stumm 1954
Stumm 1954
recombined as Viaphacops canadensis
Anthozoa - Cystiphyllida - Cystiphyllidae
Cystiphyllum vesiculosum (Goldfuss 1826)
Anthozoa - Stauriida - Zaphrentidae
Zaphrentis sp. Haime 1850
synonym of Zaphrenthis
Heliophyllum halli Edwards and Haime 1851
Anthozoa - Stauriida - Halliidae
Blothrophyllum decorticatum
Anthozoa - Favositida - Micheliniidae
Pleurodictyum sp. Goldfuss 1829
Anthozoa - Favositida - Favositidae
Favosites emmonsia
Favosites basalticus (Goldfuss 1826)
Favosites canadensis (Billings 1858)
Stromatoporoidea - Stromatoporoidea
Stromatoporoidea indet. Nicholson and Murie 1878
see common names

Geography
Country:Canada State/province:Ontario
Coordinates: 42.9° North, 79.3° West (view map)
Paleocoordinates:36.3° South, 26.6° West
Basis of coordinate:based on political unit
Geographic resolution:outcrop
Time
Period:Devonian Epoch:Middle Devonian
Stage:Givetian 10 m.y. bin:Devonian 3
*Local age/stage:Erian
Key time interval:Givetian
Age range of interval:387.70000 - 382.70000 m.y. ago
* legacy (obsolete) database fields
Stratigraphy
Formation:Onondaga Member:Edgecliff
Stratigraphic resolution:member
Lithology and environment
Primary lithology:shelly/skeletal,gray calcareous packstone
Lithology description: biohermal complex with eight distinct facies ranging from crinoidal grainstones to fissile shales and including wackestones, packestones, and mudstone; corals predominantly from well bedded, light gray to blue, coral-rich, crinoidal packstones with distinct coral-rich fissile shale interbeds
Environment:reef, buildup or bioherm Tectonic setting:foreland basin
Taphonomy
Modes of preservation:body,original calcite,replaced with silica
Size of fossils:macrofossils
Collection methods and comments
Collection excludes:some macrofossils,difficult macrofossils
Collection methods:mechanical,field collection,observed (not collected)
Reason for describing collection:biostratigraphic analysis
Taxonomic list comments:corals were the most predominant fauna and thus identified to a generic level, other fauna listed in broad taxonomic categories
Metadata
Also known as:Reef 1485; was Port Colborne Quarry bioherm, Edgecliff Member, Onondaga Formation
Database number:9476
Authorizer:A. Miller, P. Wagner Enterer:K. Layou, P. Wagner
Modifier:P. Wagner Research group:marine invertebrate
Created:2000-11-15 10:59:17 Last modified:2020-09-12 11:42:19
Access level:the public Released:2000-11-15 10:59:17
Creative Commons license:CC BY
Reference information

Primary reference:

813. C. T. Johnston. 1990. Bioherm Development in the Edgecliff Member of the Onondaga Formation, Port Colburne, Ontario. 1-91 [A. Miller/K. Layou/M. Uhen]

Secondary references:

44940 B. S. Lieberman. 1994. Evolution of the trilobite subfamily Proetinae Salter, 1864, and the origin, diversification, evolutionary affinity, and extinction of the Middle Devonian proetid fauna of eastern North America. Bulletin of the American Museum of Natural History 223:1-176 [P. Wagner/P. Wagner]
71740 E. C. Stumm. 1953. Lower Middle Devonian proetid trilobites from Michigan, southwestern Ontario, and northern Ohio. Contributions from the Museum of Paleontology, University of Michigan 11:11-31 [P. Wagner/P. Wagner]
73823 E. C. Stumm. 1954. Lower Middle Devonian Phacopid Trilobites from Michigan, Southwestern Ontario, and the Ohio Valley. Contributions from the Museum of Paleontology University of Michigan 11(11):201-221 [P. Wagner/P. Wagner]