Gull River Formation | |
---|---|
Stratigraphic range: Caradoc ~ | |
Type | Formation |
Unit of | |
Underlies | |
Overlies | Shadow Lake Formation |
Lithology | |
Primary | Limestone, dolomite |
Other | Shale, sandstone |
Location | |
Region | Ontario New York Pennsylvania |
Country | Canada United States |
Type section | |
Named for | Gull River |
Named by | V. J. Okulitch |
Year defined | 1939 |
The Gull River Formation is a geological formation of Middle Ordovician age (Caradoc Stage), which outcrops in Ontario, Canada.[1] Lithologically, the formation is dominated by light grey to brown limestones and greenish gray dolomites with thin shale and sandstone interlayers.[2][3]
Chelicerates reported from the Gull River Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Lunataspis | L. borealis | Upper Member, Kingston, Ontario.[4] | 3 specimens (1 adult & 2 juveniles or subadults).[4] | A horseshoe crab. |
Acritarchs reported from the Gull River Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Dicommopalla | D. rissae | Southern Ontario.[5] | Also found in the Bobcaygeon Formation. |