Gravel Point Formation | |
---|---|
Stratigraphic range: | |
Type | Geological formation |
Unit of | Traverse Group |
Lithology | |
Primary | Limestone |
Location | |
Region | Michigan |
Country | United States |
The Gravel Point Formation is a geologic formation in western Michigan. It preserves fossils dating back to the middle Devonian period and correlates with the Long Lake Limestone and Alpena Limestone. [1]
The Michigan Basin was a shallow marine shelf during the middle Devonian, located between 30º South and 20º North latitude in central Laurasia. According to stratigraphic and paleontological examination, the sediments of the Gravel Point Formation were deposited in a shallow lagoonal reef environment. [1]
Acanthodians of the Gravel Point Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Gyracanthus | G. sp. | South Point (Gravel Point), Little Traverse Bay, Charlevoix County. [2] | A single specimen (UMMP 1329). [2] | A gyracanthid. | |
Bony fish of the Gravel Point Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
?Onychodus | ?O. sp. | South Point (Gravel Point), Little Traverse Bay, Charlevoix County. [2] | A single specimen (UMMP 14370). [2] | An onychodontiform. | |
Placoderms of the Gravel Point Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Holonemiid | South Point (Gravel Point), Little Traverse Bay, Charlevoix County. [2] | A single specimen (UMMP 3129). [2] | |||
Several species of ostracods, an unidentified arthropod 'hook', crinoid columnals and several species of polychaetes and scolecodonts are known from the formation. [1]
Brachiopods of the Gravel Point Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Atrypa | A. corrugata | [1] | |||
Douvillina | D. sp. | Lower part of the formation. [3] | 2 specimens. [3] | ||
Heteralosia | H. sp. B | 2 pedicle valves. [3] | |||
Leptalosia | L. radicans | [3] | Also found in the Norway Point, Alpena, Four Mile Dam, Genshaw, Arkona and Hungry Hollow formations. | ||
Longispina | L. emmetensis | [3] | Also found in the Alpena Limestone and Four Mile Dam Formation. | ||
Mucrospirifer | M. latus | [1] | A spiriferid. | ||
M. sp. | [1] | A spiriferid. | |||
Oligorhachis | O. oligorhachis | [3] | Also found in the Four Mile Dam Formation. | ||
Orthopleura | O. sp. A | "Large Atrypa zone". [3] | One specimen (U.S.N.M. no. 124258). [3] | ||
O. sp. B | "Upper Blue shale". [3] | One specimen (U.S.N.M. no. 124280). [3] | |||
Pentamerella | P. aftonensis | Gorbut Member. [3] | |||
P. alpenensis | [3] | Also found in the Alpena Limestone and Four Mile Dam Formation. | |||
P. sp. D | A small collection of large shells (the largest being 38 millimeters). [3] | ||||
Pholidostrophia | P. geniculata | [3] | Also found in the Alpena, Widder and Hungry Hollow formations. | ||
Pseudoatrypa | P. keslingi | [1] | |||
Schuchertella | S. anomala | [3] | Possibly also found in the Four Mile Dam Formation. | ||
Strophodonta | S. costata | [1] | A strophomenid. | ||
S. cf. S. erotica | [1] | A strophomenid. | |||
S. erratica | [3] | Also found in the Alpena Limestone and Four Mile Dam Formation. | |||
S. fissicosta | Upper part of the formation. [3] | Also found in the Four Mile Dam Formation. | |||
S. nanus | [3] | Also found in the Alpena Limestone and Four Mile Dam Formation. | |||
S. titan titan | [3] | Also known from the Alpena Limestone. | |||
Truncalosia | T. gibbosa | [3] | Also found in the Alpena, Genshaw, Norway Point, Petoskey and Potter Farm formations, the Arkona Shale and the Hamilton Group. | ||
Tylothyris | T. subvaricosa | [4] | Also found in the Cedar Valley, Milwaukee, Mineola, Bell, Rockport Quarry, Ferron Point, Genshaw, Alpena, Norway Point and Potter Farm formations. |
Bryozoans of the Gravel Point Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Fenestellapolypore | F. magnifica | [1] | A fenestellid. | ||
Cnidarians of the Gravel Point Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Aulocystis | A. alectiformis | [5] | Also found in the Alpena Limestone. | ||
A. fenestrata | 6 specimens. [5] | Also found in the Alpena Limestone. | |||
Aulopora | A. conferta | [5] | Also found in the Bell, Ferron Point, Genshaw, Alpena, Four Mile Dam, Potter Farm, Petoskey and Hungry Hollow formations. | ||
A. socialis | Upper part of the formation. [5] | ||||
Favosites | F. mammilatus | [1] | A tabulate coral. | ||
Pachyphragma | P. concentricum | [5] | Also found in the Ferron Point, Four Mile Dam and Alpena formations. | ||
P. erectum | [5] | Also found in the Potter Farm and Petoskey formations. | |||
Sponges of the Gravel Point Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Parallelopora | P. winchelli | [1] | A stromatoporoid. | ||
Tentaculitans of the Gravel Point Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Tentaculites | T. sp. | [1] | A tentaculitid. | ||
Color key
| Notes Uncertain or tentative taxa are in small text; |
Trilobites of the Gravel Point Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Ancyropyge | A. romingeri | "Longispina emmetensis zone". [6] | |||
Dechenella | D. (Basidechenella) pulchra | [6] | Also found in the Alpena Limestone and Dock Street clay of the Four Mile Dam Formation. | ||
Eldredgeops | E. rana alpenensis | [6] | Originally reported as Phacops rana alpenensis. Also found in the Alpena Limestone. | ||
Greenops | G. aequituberculatus | [6] | Also found in the Norway Point and Four Mile Dam formations. | ||
G. traversensis | [6] | Also found in the Dock Street clay of the Four Mile Dam Formation. | |||
Phacops | P. rana alpenensis | [6] | Reassigned to the genus Eldredgeops . | ||
Proetus | P. (Crassiproetus) traversensis | [6] | Also found in the Four Mile Dam Formation. | ||
Algal colonies are known from the formation. [1]
Acritarchs of the Gravel Point Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Lophosphaeridium | L. sp. | [1] | |||
Tasmanites | T. sp. | [1] | |||
Plants of the Gravel Point Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Material | Notes | Images |
Ancyrospora | A. sp. | Miospores. [1] | |||
† 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.
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.
The Traverse Group is a geologic group in Michigan, Indiana and Ohio comprising middle Devonian limestones with calcareous shale components. Its marine fossils notably include Michigan's state stone, the Petoskey stone, among other corals and records of ancient marine life. A range of trilobites has also been found in the Traverse Group.
The Four Mile Dam Formation, also called the Four Mile Dam Limestone, is a geologic formation in Michigan. It preserves fossils dating back to the middle Devonian period.
The Norway Point Formation is a geologic formation in Michigan. It preserves fossils dating back to the middle Devonian period.
The Thunder Bay Limestone is a geologic formation in Michigan. It preserves fossils dating back to the Devonian period.
The Georgian Bay Formation is a geologic formation in Michigan and Ontario. It preserves fossils dating back to the Ordovician period. The type locality of the formation is on East Meaford Creek, south shore of Nottawasaga Bay, Georgian Bay.
The Piney Point Formation is a geologic formation in Virginia. It preserves fossils dating back to the Lutetian Stage of the Eocene Epoch of the Paleogene period.
The Ash Hollow Formation of the Ogallala Group is a geological formation found in Nebraska and South Dakota. It preserves fossils dating back to the Neogene period. It was named after Ash Hollow, Nebraska and can be seen in Ash Hollow State Historical Park. Ashfall Fossil Beds State Historical Park is within this formation.
The Sharps Formation is a geologic formation in South Dakota. It preserves fossils dating back to the Paleogene.
The Lueders Formation is a geologic formation in Texas. It is the top formation of the Albany Group and preserves fossils dating back to the Permian period.
The Luning Formation is a geologic formation in Nevada. It preserves fossils dating back to the Triassic period.
The Attawapiskat Formation is a geologic formation in Ontario. It preserves fossils dating back to the Silurian period.
The Escuminac Formation is a geologic formation in Quebec. It preserves fossils dating back to the Frasnian, in the Devonian period.
The Merrimack Formation is a geologic formation in Quebec. It preserves fossils dating back to the Silurian period.
The Jupiter Formation is a geologic formation in Quebec, well-exposed in the southern third of Anticosti Island and lying in the St Lawrence River Valley. It preserves fossils dating back to the Silurian period.
The Campbellton Formation is a geologic formation in New Brunswick. It preserves fossils dating back to the latest Pragian and Emsian of the Devonian period.
The Bird Fiord Formation is a geologic formation in Nunavut. It preserves fossils dating back to the Devonian period.
The Rockport Quarry Limestone is a geologic formation in Michigan. It preserves fossils dating back to the middle Devonian period.
The Bertie Group or Bertie Limestone, also referred to as the Bertie Dolomite and the Bertie Formation, is an upper Silurian geologic group and Lagerstätte in southern Ontario, Canada, and western New York State, United States. Details of the type locality and of stratigraphic nomenclature for this unit as used by the U.S. Geological Survey are available on-line at the National Geologic Map Database. The formation comprises dolomites, limestones and shales and reaches a thickness of 495 feet (151 m) in the subsurface, while in outcrop the group can be 60 feet (18 m) thick.
{{cite journal}}
: Cite journal requires |journal=
(help)