Gravel Point Formation

Last updated
Gravel Point Formation
Stratigraphic range: Middle Devonian (Givetian) [1]
O
S
D
C
P
T
J
K
Pg
N
Fossiliferous limestone (Gravel Point Formation, Middle Devonian; near South Point, west of Charlevoix, Michigan, USA) 8.jpg
Fossiliferous limestone from the Gravel Point Formation
Type Geological formation
Unit of Traverse Group
Lithology
Primary Limestone
Location
RegionFlag of Michigan.svg  Michigan
CountryFlag of the United States.svg  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]

Contents

Description

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]

Fossil content

Vertebrates

Acanthodians

Acanthodians of the Gravel Point Formation
GenusSpeciesPresenceMaterialNotesImages
Gyracanthus G. sp.South Point (Gravel Point), Little Traverse Bay, Charlevoix County. [2] A single specimen (UMMP 1329). [2] A gyracanthid.
Gyracanthus NT small.jpg

Bony fish

Bony fish of the Gravel Point Formation
GenusSpeciesPresenceMaterialNotesImages
?Onychodus ?O. sp.South Point (Gravel Point), Little Traverse Bay, Charlevoix County. [2] A single specimen (UMMP 14370). [2] An onychodontiform.
OnychodusDB15.jpg

Placoderms

Placoderms of the Gravel Point Formation
GenusSpeciesPresenceMaterialNotesImages
Holonemiid South Point (Gravel Point), Little Traverse Bay, Charlevoix County. [2] A single specimen (UMMP 3129). [2]

Invertebrates

Several species of ostracods, an unidentified arthropod 'hook', crinoid columnals and several species of polychaetes and scolecodonts are known from the formation. [1]

Brachiopods

Brachiopods of the Gravel Point Formation
GenusSpeciesPresenceMaterialNotesImages
Atrypa A. corrugata [1]
Douvillina D. sp.Lower part of the formation. [3] 2 specimens. [3]
Heteralosia H. sp. B2 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. aftonensisGorbut Member. [3]
P. alpenensis [3] Also found in the Alpena Limestone and Four Mile Dam Formation.
P. sp. DA 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. fissicostaUpper 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

Bryozoans of the Gravel Point Formation
GenusSpeciesPresenceMaterialNotesImages
Fenestellapolypore F. magnifica [1] A fenestellid.

Cnidarians

Cnidarians of the Gravel Point Formation
GenusSpeciesPresenceMaterialNotesImages
Aulocystis A. alectiformis [5] Also found in the Alpena Limestone.
A. fenestrata6 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. socialisUpper 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

Sponges of the Gravel Point Formation
GenusSpeciesPresenceMaterialNotesImages
Parallelopora P. winchelli [1] A stromatoporoid.

Tentaculitans

Tentaculitans of the Gravel Point Formation
GenusSpeciesPresenceMaterialNotesImages
Tentaculites T. sp. [1] A tentaculitid.
TentaculitidDevonian.jpg

Trilobites

Color key
Taxon Reclassified taxonTaxon falsely reported as presentDubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
Trilobites of the Gravel Point Formation
GenusSpeciesPresenceMaterialNotesImages
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.
Phacops rana.jpg
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.

Flora

Algal colonies are known from the formation. [1]

Acritarchs

Acritarchs of the Gravel Point Formation
GenusSpeciesPresenceMaterialNotesImages
Lophosphaeridium L. sp. [1]
Tasmanites T. sp. [1]

Plants

Plants of the Gravel Point Formation
GenusSpeciesPresenceMaterialNotesImages
Ancyrospora A. sp. Miospores. [1]

See also

Related Research Articles

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.

<span class="mw-page-title-main">Paleontology in Oklahoma</span> Paleontological research in the U.S. state of Oklahoma

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.

<span class="mw-page-title-main">Four Mile Dam Formation</span> Geological feature in Michigan USA

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.

<span class="mw-page-title-main">Norway Point Formation</span>

The Norway Point Formation is a geologic formation in Michigan. It preserves fossils dating back to the middle Devonian period.

<span class="mw-page-title-main">Thunder Bay Limestone</span> Geological Formations

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.

<span class="mw-page-title-main">Ash Hollow Formation</span> Geologic formation in Nebraska

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.

<span class="mw-page-title-main">Lueders Formation</span> Geologic formation in Texas, United States

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.

<span class="mw-page-title-main">Rockport Quarry Limestone</span>

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.

References

  1. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 Mohan, Joseph (November 2013). "A Paleoenvironmental Analysis of the Middle Devonian Gravel Point Formation, Western Michigan". The Professional Geologist. 50 (6): 12–16.
  2. 1 2 3 4 5 6 Stack, Jack; Sallan, Lauren (2018-09-20). "An examination of the Devonian fishes of Michigan". PeerJ. 6 (2): e5636. doi: 10.7717/peerj.5636 . PMC   6151260 . PMID   30258725. S2CID   52843222.
  3. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 Imbrie, John (1959). "Brachiopods of the Traverse group (Devonian) of Michigan. Part 1, Dalmanellacea, Pentameracea, Strophomenacea, Orthotetacea, Chonetacea, and Productacea. Bulletin of the AMNH ; v. 116, article 4". hdl:2246/1258.{{cite journal}}: Cite journal requires |journal= (help)
  4. Rogers, Frederick S.; Pitrat, Charles W. (May 1987). "Distribution of Tylothyris (Brachiopoda) and its occurrence in the Traverse Group (Middle Devonian) of Michigan". Journal of Paleontology. 61 (3): 494–507. doi:10.1017/S0022336000028651. ISSN   0022-3360. S2CID   130922140.
  5. 1 2 3 4 5 6 Watkins, J. Lloyd (1959). "Middle Devonian Auloporid Corals from the Traverse Group of Michigan". Journal of Paleontology. 33 (5): 793–808. ISSN   0022-3360. JSTOR   1300915.
  6. 1 2 3 4 5 6 7 Stumm, Erwin (1953). "Trilobites of the Devonian Traverse Group of Michigan" (PDF). University of Michigan Press - Museum of Paleontology.