Norway Point Formation | |
---|---|
Stratigraphic range: | |
Type | Geological formation |
Unit of | Traverse Group [1] |
Overlies | Four Mile Dam Formation [1] |
Location | |
Region | Michigan |
Country | United States |
The Norway Point Formation is a geologic formation in Michigan. It preserves fossils dating back to the middle Devonian period.
Acanthodians | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Oracanthus | O. sp. | "Four Mile Dam, 6 kilometers northwest of Alpena, Alpena County, Michigan". [1] | "A single spine (UMMP 23495)". [1] | ||
Conodonts | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Acodina | A. formosa | [2] | Also found in the Detroit River, Traverse, Dundee, Bell, Alpena and Four Mile Dam formations. | ||
A. lanceolata | [2] | Also found in the Traverse Formation. | |||
Belodella | B. devonicus | [2] | Also found in the Detroit River, Traverse, Antrim, Alpena and Four Mile Dam formations. | ||
Hindeodella | H. germana | [2] | Also found in the Detroit River, Traverse and Antrim formations. | ||
Icriodus | I. cymbiformis | [2] | Also found in the Detroit River, Traverse, Antrim, Ferron Point, Genshaw, Alpena and Thunder Bay formations. | ||
I. expansus | [2] | Also found in the Detroit River, Traverse, Antrim, Lucas, Anderdon, Dundee, Bell, Ferron Point, Genshaw, Alpena, Potter Farm and Thunder Bay formations. | |||
I. latericrescens latericrescens | [2] | Also found in the Traverse, Bell, Ferron Point, Genshaw, Newton Creek, Alpena, Four Mile Dam, Potter Farm and Thunder Bay formations. | |||
Ligonodina | L. falciformis | [2] | Also found in the Traverse Formation and Alpena Limestone. | ||
Ozarkodina | O. willsi | [2] | Also found in the Detroit River, Traverse, Antrim, Dundee, Alpena and Four Mile Dam formations. | ||
Polygnathus | P. linguiformis linguiformis | [2] | Also found in the Detroit River, Traverse, Antrim, Dundee, Bell and Alpena formations. | ||
P. varcus | [2] | Also found in the Traverse, Antrim, Alpena, Four Mile Dam and Thunder Bay formations. | |||
Synprioniodina | S. regularis | [2] | Also found in the Detroit River, Traverse, Antrim, Dundee, Bell and Alpena formations. | ||
Color key
| Notes Uncertain or tentative taxa are in small text; |
Corals | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Aulocystis | A. commensalis | [5] | Also found in the Ipperwash Limestone and Wanakah Shale. | ||
A. stummi | Thunder Bay River below Four Mile Dam, Alpena County, Michigan. [5] | ||||
Ostracods | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Aechmina | A. choanobasota | 2 right valves. [6] | |||
A. sp. A | 2 right valves. [6] | ||||
A. sp. B | A carapace, No. 29828. [6] | ||||
Arcyzona | A. aperticarinata | [6] | |||
A. diademata | A carapace and right valve. [6] | ||||
A. sp. | 2 carapaces. [6] | ||||
Barychilina | B. embrithes | A left valve [6] | |||
B. labyrinthea | A carapace. [6] | ||||
B. sp. | A left valve. [6] | ||||
Birdsallella | B. delawarensis | [6] | |||
B. tumida | [6] | ||||
Bythocypris | B. devonica borealis | A carapace. [6] | |||
B. parsonia | A carapace. [6] | ||||
B. subquadrata | 2 carapaces. [6] | ||||
Coelonella | C. scapha | 2 carapaces. [6] | |||
Ctenoloculina | C. cicatricosa | [6] | |||
Dizygopleura | D. euglyphea | A left valve. [6] | |||
Euglyphella | E. compressa | A right valve. [6] | |||
E. sigmoidalis | [6] | ||||
E. simplex | [6] | ||||
Eukloedenella | E. doverensis | One female left valve and one male left valve. [6] | |||
Falsipollex | F. equipapillatus | [6] | |||
Glyptopleura | G. bipunctata | [6] | |||
Halliella | H. bellipuncta | 2 right valves. [6] | |||
Healdia | H. gibba | [6] | |||
H. sp. | A right valve. [6] | ||||
Hollinella | H. ampla | A left valve. [6] | |||
H. inclinisulcata | [6] | ||||
H. labrosa | 3 right valves. [6] | ||||
H. tendilobata | [6] | ||||
H. sp. A | "Two carapaces, Nos. 27352 and 27353". [6] | ||||
H. sp. B | "A male carapace, No. 27354". [6] | ||||
Hyphasmaphora | H. textiligera | 2 right valves. [6] | |||
Jenningsina | J. catenulata | [6] | |||
J. scalpta | A left valve. [6] | ||||
Lucasella | L. mundula | [6] | |||
Monoceratina | M. casei | "2 carapaces, Nos. 27374 and 27375". [6] | |||
Octonaria | O. crescentiformis | [6] | |||
O. quadricostata | [6] | ||||
Parabolbina | P. acinina | 2 male right valves. [6] | |||
Ponderodictya | P. punctulifera | [6] | |||
P. sp. | One specimen (No. 29891). [6] | May be an early instar of P. punctulifera. [6] | |||
Punctoprimitia | P. subaequalis | 1 right valve and 4 left valves. [6] | |||
Quasillites | Q. binodosus | [6] | |||
Q. jubatus | [6] | ||||
Q. lobatus | A right valve. [6] | ||||
Q. obliquus | A carapace. [6] | ||||
Q. cf. Q. ornatus | A carapace. [6] | ||||
Q. ornatus | 3 carapaces and a right valve. [6] | ||||
Reticestus | R. acclivitatus | [6] | |||
Ropolonellus | R. papillatus | A right valve. [6] | |||
R. plenus | A right valve. [6] | ||||
Ruptivelum | R. bacculatum | [6] | |||
Subligaculum | S. biorthogonium | [6] | |||
S. trullatum | 2 male left valves and a broken female right valve. [6] | ||||
Tetrasacculus | T. paeneloculatus | [6] | |||
Ulrichia | U. fragilis | 1 carapace and 2 left valves. [6] | |||
U. spinifera | 3 right valves. [6] |
Trilobites | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Dechenella | D. (Basidechenella) sp. A | "Nos. 25506, 28719, 28720, and 28721". [7] | |||
Dipleura | D. dekayi | "Shales just above the Spinocyrtia zone". [7] | Also found in the Thunder Bay Limestone. | ||
Eldredgeops | E. rana | [7] | Originally reported as Phacops rana. Also found in the Hamilton, Hungry Hollow, Widder, Plum Brook, Prout, Ten Mile Creek, Alpena, Four Mile Dam and Gravel Point formations. | ||
Greenops | G. aequituberculatus | [7] | Also found in the Gravel Point Formation and Dock Street clay of the Four Mile Dam Formation. | ||
Phacops | P. rana | [7] | Moved to the genus Eldredgeops . | ||
† Bembexia is a genus of fossil sea snails, marine gastropod mollusks. This genus is placed in the subfamily Eotomariinae, of the family Eotomariidae. The shell characters resemble those of Balbinipleura. These snails have been interpreted as herbivorous, probably grazing on algae.
The Marjum Formation is a Cambrian geological formation that overlies the Wheeler Shale in the House Range, Utah. It is named after its type locality, Marjum Pass, and was defined in 1908. The formation is known for its occasional preservation of soft-bodied tissue, and is slightly younger than the Burgess Shale, falling in the Ptychagnostus praecurrens trilobite zone.
Paleontology in Oklahoma refers to paleontological research occurring within or conducted by people from the U.S. state of Oklahoma. Oklahoma has a rich fossil record spanning all three eras of the Phanerozoic Eon. Oklahoma is the best source of Pennsylvanian fossils in the United States due to having an exceptionally complete geologic record of the epoch. From the Cambrian to the Devonian, all of Oklahoma was covered by a sea that would come to be home to creatures like brachiopods, bryozoans, graptolites and trilobites. During the Carboniferous, an expanse of coastal deltaic swamps formed in areas of the state where early tetrapods would leave behind footprints that would later fossilize. The sea withdrew altogether during the Permian period. Oklahoma was home a variety of insects as well as early amphibians and reptiles. Oklahoma stayed dry for most of the Mesozoic. During the Late Triassic, carnivorous dinosaurs left behind footprints that would later fossilize. During the Cretaceous, however, the state was mostly covered by the Western Interior Seaway, which was home to huge ammonites and other marine invertebrates. During the Cenozoic, Oklahoma became home to creatures like bison, camels, creodonts, and horses. During the Ice Age, the state was home to mammoths and mastodons. Local Native Americans are known to have used fossils for medicinal purposes. The Jurassic dinosaur Saurophaganax maximus is the Oklahoma state fossil.
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The Thunder Bay Limestone is a geologic formation in Michigan. It preserves fossils dating back to the Devonian period.
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The Johnson Spring Formation is a geologic formation in California. It preserves fossils dating back to the Ordovician period.
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