Arundel Formation

The Arundel Formation, also known as the Arundel Clay, is a clay-rich sedimentary rock formation, within the Potomac Group, found in Maryland[2] of the United States of America. It is of Aptian age (Lower Cretaceous). This rock unit had been economically important as a source of iron ore, but is now more notable for its dinosaur fossils. It consists of clay lenses within depressions in the upper part of the Patuxent Formation that may represent oxbow swamp facies.[3] It is named for Anne Arundel County, Maryland.[4]

Arundel Formation
Stratigraphic range: Aptian
Outdoor excavation on an exposed portion of the Arundel clays at Dinosaur Park at Laurel, Maryland, USA
TypeGeological Formation
Unit ofPotomac Group
UnderliesPatapsco Formation (Unconformity)
OverliesPatuxent Formation
Thicknessup to 125 feet (40 m)[1]
Lithology
PrimaryClay
OtherSiderite nodules
Location
Region Maryland, Washington D. C.
CountryUnited States
Type section
Named forAnne Arundel County, Maryland
Named byW. B. Clark, 1897[1]

Vertebrate paleofauna

Dinosaurs

Dinosaurs present include cf. Acrocanthosaurus,[5][6] the possible ornithischian Magulodon,[5] the poorly known theropods "Allosaurus" medius, "Creosaurus" potens, and "Coelurus" gracilis, the ornithomimosaurian "Dryosaurus" grandis,[7] as well as another indeterminate ornithomimosaurian (though it most likely is Nedcolbertia),[8] the sauropod Astrodon, the nodosaurid Priconodon,[9] a possible basal ceratopsian,[10] and potentially the ornithopod Tenontosaurus.[3] Other vertebrates are not as well known from the formation, but include a freshwater shark, a lungfish,[11] at least three genera of turtles, and at least one crocodilian.[3]

Color key
TaxonReclassified taxonTaxon falsely reported as presentDubious taxon or junior synonymIchnotaxonOotaxonMorphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
Dinosaurs reported from the Arundel Formation
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
Acrocanthosaurus[5][12]A. cf. atokensis[12]"Teeth",[5] "incomplete skeleton"[12]A large carcharodontosaurid theropod. Presence long suspected but uncertain, but confirmed in 2024 following the discovery of more complete remains.[12]
Acrocanthosaurus

Allosaurus[13]

"A." medius[13]

"Tooth."[14]

An indeterminate theropod tooth.

Astrodon
Deinonychus
Tenontosaurus

Astrodon[15]

A. johnstoni[15]

"Tooth."[17]

"Capitalsaurus"[18]

"C." potens

"Vertebra."[14]

A neotheropod possibly synonymous with Acrocanthosaurus.[19]

Coelurus[13]

"C." gracilis

"Manual ungual and teeth."[14]

A dromaeosaurid synonymous with Deinonychus.[19]

Creosaurus[13]

"C." potens[13]

Reclassified as "Capitalsaurus" potens

cf. Deinonychus[13]

Indeterminate[13]

A dromaeosaurid

Dryosaurus

"D." grandis

"Limb elements."[20]

An indeterminate member of Ornithomimosauria.

Magulodon[21]

M. muirkirkensis[21]

"Tooth"[21]

Likely an ornithischian, this genus is a nomen nudum that has not been formally published.

Neoceratopsia indet.[10]Indeterminate[10]"Teeth"[10]An indeterminate member of Neoceratopsia. Initially believed to have belonged to an indeterminate member of Dryosauridae or the genus Tenontosaurus.

Ornithomimus

"O." affinis

Junior synonym of "Dryosaurus" grandis

Pleurocoelus[13]

P. altus[13]

"Tibia [and] fibula."[22]

Possibly synonymous with Astrodon.

P. nanus[13]

Possibly synonymous with Astrodon.

Priconodon[13]

P. crassus[13]

"Teeth, tibia."[23]

A large nodosaurid.

cf. Tenontosaurus[24]

Indeterminate[24]

Pterosaurs

Unassigned pteradactyloid tracks.[25]

Color key
TaxonReclassified taxonTaxon falsely reported as presentDubious taxon or junior synonymIchnotaxonOotaxonMorphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
Pterosaurs of the Arundel Formation
GenusSpeciesLocationStratigraphic positionAbundanceNotesImages

Pteraichnus[25]

[25]

Other fossils

William Bullock Clark (1897) described lignitized trunks of trees often found in upright positions with their roots still intact.[1]

G. J. Brenner (1963) described spores and pollen within the formation.[26]

See also

Footnotes

References

  • Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.

39°3′N 76°38′W / 39.050°N 76.633°W / 39.050; -76.633