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Dinosaur Park Formation
Uppermost member of the Belly River Group geologic unit in Alberta, Canada From Wikipedia, the free encyclopedia
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The Dinosaur Park Formation is the uppermost member of the Belly River Group (also known as the Judith River Group), a major geologic unit in southern Alberta. It was deposited during the Campanian stage of the Late Cretaceous, between about 76.5 and 74.4 million years ago.[3] It was deposited in alluvial and coastal plain environments, and it is bounded by the nonmarine Oldman Formation below it and the marine Bearpaw Formation above it.[4]
The Dinosaur Park Formation contains dense concentrations of dinosaur skeletons, both articulated and disarticulated, which are often found with preserved remains of soft tissues. Remains of other animals such as fish, turtles, and crocodilians, as well as plant remains, are also abundant.[5] The formation has been named after Dinosaur Provincial Park, a UNESCO World Heritage Site where the formation is well exposed in the badlands that flank the Red Deer River.[2]
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Research history
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The Dinosaur Park Formation has been a significant source of terrestrial vertebrate fossils for over a century. The first recorded account of fossils was in 1871 by the priest Jean-Baptiste L’Heureux who was shown bones of the "grandfather of the buffalo" by the Blackfoot Confederacy he was living with, though these notes were never published. Official reports of dinosaur bones in western Canada were reported by George Mercer Dawson in 1874 from southern Saskatchewan and Alberta along the Milk River. Further discoveries by Dawson and his colleagues of the Geological Survey of Canada continued in the 1880s, including the 1884 discovery by Joseph Burr Tyrrell of the skull of a theropod identified as Laelaps by American palaeontologist Edward Drinker Cope but named in 1905 as Albertosaurus by American palaeontologist Henry Fairfield Osborn. In 1889 rich fossil beds in the areas of Deadlodge Canyon[a] and Berry Creek[b] were found by Thomas Chesmer Weston along the Red Deer River. The areas along the Red Deer River would be more completely surveyed by Canadian palaeontologist Lawrence Lambe from 1897 until 1901, when he, along with Osborn, described the fossils found in what was then considered to be the Belly River Formation of mid-Cretaceous age.[6]
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Geological setting
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The Dinosaur Park Formation is composed of sediments that were derived from the erosion of the mountains to the west. It was deposited on an alluvial to coastal plain by river systems that flowed eastward and southeastward to the Bearpaw Sea, a large inland sea that was part of the Western Interior Seaway. That sea gradually inundated the adjacent coastal plain, depositing the marine shales of the Bearpaw Formation on top of the Dinosaur Park Formation.[4]
The Dinosaur Park Formation is about 70 metres (230 ft) thick at Dinosaur Park. The lower portion of the formation was laid down in fluvial channel environments and consists primarily of fine- to medium-grained, crossbedded sandstones. The upper portion, which was deposited in overbank and floodplain environments, consists primarily of massive to laminated, organic-rich mudstones with abundant root traces, and thin beds of bentonite. The Lethbridge Coal Zone, which consists of several seams of low-rank coal interbedded with mudstones and siltstones, marks the top of the formation.[4]
The sediments of the Dinosaur Park Formation are similar to those of the underlying Oldman Formation and they were originally included in that formation. The two formations are separated by a regional disconformity, however, and are distinguished by petrographic and sedimentologic differences. In addition, articulated skeletal remains and bonebeds are rare in the Oldman Formation but abundant in the Dinosaur Park Formation.[2][4]
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Biostratigraphy
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The Dinosaur Park Formation can be divided into at least two distinct faunas. The lower part of the formation is characterized by the abundance of Corythosaurus and Centrosaurus. This group of species is replaced higher in the formation by a different ornithischian fauna characterized by the presence of Lambeosaurus and Styracosaurus.[7] The appearance of several new, rare species of ornithischian at the very top of the formation may indicate that a third distinct fauna had replaced the second during the transition into younger, non-Dinosaur Park sediments, at the same time an inland sea transgresses onto land, but there are fewer remains here. An unnamed pachyrhinosaur, Vagaceratops irvinensis, and Lambeosaurus magnicristatus may be more common in this third fauna.[8][9]
Biostratigraphy of the megaherbivores of the Dinosaur Park Formation with ranges, assemblage zones, and radiometric dating after Mallon (2019) and Eberth and colleagues (2023):[10][11]


*The taxonomy of Euoplocephalus tutus is disputed, with Penalski (2018) separating the taxon into: Scolosaurus cutleri (~0m), Platypelta coombsi (~3-8m), Euoplocephalus tutus (~16-30m), Anodontosaurus inceptus (~27-31m), and Scolosaurus thronus (~40m)[12]
Fossil content
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Amphibians
Remains of the following amphibians have been found in the formation:[13]
Albanerpetontidae (extinct, salamander-like amphibians)
- Habrosaurus prodilatus
- Lisserpeton
- Opisthotriton kayi
- Scapherpeton tectum
- unnamed caudatan
- Two indeterminate caudatans
Dinosaurs
Color key
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Notes Uncertain or tentative taxa are in small text; |

Remains of the following dinosaurs have been found in the formation:[16][17]
Ornithischians
Remains of the following ornithischians have been found in the formation:[18]
Ankylosaurs
Numerous specimens that cannot be definitively assigned to ankylosaurs are known from the formation, including fragmentary cranial, dental, postcranial, and armour material.[19] As all ankylosaurids from the Campanian of Alberta and Montana were historically referred to Euoplocephalus sensu lato, the taxonomy is variable between studies and ranges from one to seven valid genera between the Dinosaur Park, Judith River, Two Medicine, and Horseshoe Canyon Formations.[12]
Ceratopsians
An unnamed Pachyrhinosaurus-like taxon has been recovered from the formation.[22]
Ornithopods
At least one indeterminate thescelosaurid specimen has been recovered from the formation.
In a 2001 review of hadrosaur eggshell and hatchling material from the Dinosaur Park Formation, Darren H. Tanke and M. K. Brett-Surman concluded that hadrosaurs nested in both the ancient upland and lowlands of the formation's depositional environment.[32] The upland nesting grounds may have been preferred by the less common hadrosaurs, like Brachylophosaurus or Parasaurolophus. However, the authors were unable to determine what specific factors shaped nesting ground choice in the formation's hadrosaurs. They suggested that behavior, diet, soil condition, and competition between dinosaur species all potentially influenced where hadrosaurs nested.[33]
Sub-centimeter fragments of pebbly-textured hadrosaur eggshell have been reported from the Dinosaur Park Formation. This eggshell is similar to the hadrosaur eggshell of Devil's Coulee in southern Alberta as well as that of the Two Medicine and Judith River Formations in Montana, United States.[34] While present, dinosaur eggshell is very rare in the Dinosaur Park Formation and is only found in two different microfossil sites.[32] These sites are distinguished by large numbers of pisidiid clams and other less common shelled invertebrates like unionid clams and snails. This association is not a coincidence as the invertebrate shells would have slowly dissolved and released enough basic calcium carbonate to protect the eggshells from naturally occurring acids that otherwise would have dissolved them and prevented fossilization.[34]
In contrast with eggshell fossils, the remains of very young hadrosaurs are actually somewhat common. Darren Tanke has observed that an experienced collector could actually discover multiple juvenile hadrosaur specimens in a single day. The most common remains of young hadrosaurs in the Dinosaur Park Formation are dentaries, bones from limbs and feet, as well as vertebral centra. The material showed little or none of the abrasion that would have resulted from transport, meaning the fossils were buried near their point of origin.[35] Bonebeds 23, 28, 47, and 50 are productive sources of young hadrosaur remains in the formation, especially bonebed 50. The bones of juvenile hadrosaurs and fossil eggshell fragments are not known to have preserved in association with each other, despite both being present in the formation.[36]
Pachycephalosaurs
Theropods
In the Dinosaur Park Formation, small theropods are rare due to the tendency of their thin-walled bones to be broken or poorly preserved.[43] Small bones of small theropods that were preyed upon by larger ones may have been swallowed whole and digested.[44] In this context, the discovery of a small theropod dinosaur with preserved tooth marks was especially valuable.[43] Possible indeterminate avimimid remains are known from the formation.
Ornithomimids
Oviraptorosaurs
Paravians
A new taxon of troodontid based solely on teeth is known from the upper part of the formation.[51]
Tyrannosaurs
Other reptiles
Color key
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Notes Uncertain or tentative taxa are in small text; |
Choristoderes
Choristoderes, or champsosaurs, were aquatic reptiles. Small examples looked like lizards, while larger types were superficially similar to crocodilians. Remains of the following Choristoderes have been found in the formation:[60]
- Champsosaurus (at least 3 species)
- Cteniogenys sp. cf. antiquus (possibly another genus)
Crocodylians
Remains of the following Crocodylians have been found in the formation:[61]
- Albertochampsa
- Leidyosuchus
- at least 1 unnamed taxon
Lizards
Remains of the following lizards have been found in the formation:[62]
Plesiosaurs
Remains of the following Plesiosaurs have been found in the formation:[63]
- Fluvionectes
- indeterminate polycotylids (shorter-necked)
Pterosaurs
Remains of the following pterosaurs have been found in the formation:[64]
- Cryodrakon [65] (known from small and large specimens)
- 1 unnamed non-azhdarchid pterosaur
Turtles
Remains of the following turtles have been found in the formation:[66]
- Adocus
- "Apalone"
- Aspideretoides (3 species)
- Basilemys
- Boremys
- Judithemys
- Neurankylus
- Plesiobaena
- 2 indeterminate taxa
Mammals

Remains of the following mammals have been found in the formation:[67]
- Multituberculata
- Cimexomys sp.
- Cimolodon spp.
- Cimolomys clarki
- Meniscoessus major
- Mesodma primaeva
- unnamed multituberculates
- Metatherians
- Alphadon halleyi
- Eodelphis browni
- E. cutleri
- 5 species of "Pediomys"
- Turgidodon russelli
- T. praesagus
- Eutherians
- Cimolestes sp. (uncertain taxonomy)
- Gypsonictops lewisi
- Paranyctoides sternbergi
- Unknown therians: at least 1 species
Fish
Remains of the following fish have been found in the formation:[68]
- Chondrichthyans
- Cretorectolobus olsoni (a carpet shark)
- Eucrossorhinus microcuspidatus (a carpet shark)
- Ischyrhiza mira (a sclerorhynchid)[69]
- Meristodonoides montanensis (a shark)
- Myledaphus bipartitus (a ray)
- Protoplatyrhina renae (a guitarfish)
- indeterminate orectolobid
- Acipenseriformes (sturgeons)
- Holostean fish
- Lepisosteus occidentalis (the gar)
- unnamed bowfin
- at least 2 other holosteans
- Teleost fish
- Archaeosiilik sp. (a pike)[71]
- Belonostomus longirostris
- Cretophareodus alberticus (an osteoglossomorph)
- Coriops amnicolus
- Estesesox foxi (a pike)
- Horseshoeichthys armaserratus (an ellimmichthyiform)[71]
- Nunikuluk gracilis (a pike)[71]
- Oldmanesox canadensis (a pike)
- Paralbula (including Phyllodus)
- Paratarpon apogerontus (an elopomorph, like the tarpon)
- Primuluchara laramidensis (a characin)[72][73]
- Sivulliusalmo sp. (a salmonid)[71]
- at least 8 other teleosts
Invertebrates
Remains of the following invertebrates have been found in the formation:[74]
- Freshwater bivalves
- Freshwater gastropods
- Campeloma (2 species)
- Elimia
- Goniobasis (3 species)
- Hydrobia
- Lioplacodes (2 species)
Flora
Plant body fossils
The following plant body fossils have been found in the formation:[75]
- various ferns
- Equisetum (Equisetaceae)
- Gymnosperms
- Platyspiroxylon (Cupressaceae)
- Podocarpoxylon (Podocarpaceae)
- Elatocladus (Taxodiaceae)
- Sequoia (Taxodiaceae)
- Sequoiaxylon (Taxodiaceae)
- Taxodioxylon (Taxodiaceae)
- Ginkgos
- Angiosperms
- Artocarpus (Moraceae)
- Cercidiphyllum (Cercidiphyllaceae)
- Dombeyopsis (Sterculiaceae)
- Menispermites (Menispermaceae)
- Pistia (Araceae)
- Platanus (Platanaceae)
- Vitis (Vitaceae)
- Trapa (Trapaceae)
Palynomorphs
Palynomorphs are organic-walled microfossils, like spores, pollen, and algae. The following palynomorphs have been found in the formation:[76]
- Unknown producers
- at least 8 species
- Fungi
- at least 35 taxa
- Chlorophyta (green algae and blue-green algae)
- at least 12 species
- Pyrrhophyta (dinoflagellates, a type of marine algae)
- unassigned cysts
- Bryophytes (mosses, liverworts, and hornworts)
- Anthocerotophyta (hornworts)
- at least 5 species
- Marchantiophyta (liverworts)
- at least 14 species
- Bryophyta (mosses)
- at least 5 species
- Anthocerotophyta (hornworts)
- Lycopodiophyta
- Lycopodiaceae (club mosses)
- at least 11 species
- Selaginellaceae (small club mosses)
- at least 6 species
- Isoetaceae (quillworts)
- at least 1 species
- Lycopodiaceae (club mosses)
- Polypodiophyta
- Osmundaceae (cinnamon ferns)
- at least 6 species
- Schizaeaceae (climbing ferns)
- at least 20 species
- Gleicheniaceae (Gleichenia and allies; coral ferns)
- at least 5 species
- Cyatheaceae (Cyathea and allies)
- at least 4 species
- Dicksoniaceae (Dicksonia and allies)
- at least 3 species
- Polypodiaceae (ferns)
- at least 4 species
- Matoniaceae
- at least 1 species
- Marsileaceae
- at least 1 species
- Osmundaceae (cinnamon ferns)
- Pinophyta (gymnosperms)
- Cycadaceae (cycads)
- at least 3 species
- Caytoniaceae
- at least 1 species
- Pinaceae (pines)
- at least 4 species
- Cupressaceae (cypresses)
- at least 3 species
- Podocarpaceae (Podocarpus and allies)
- at least 4 species
- Cheirolepidiaceae
- at least 2 species
- Ephedraceae (Mormon teas)
- at least 6 species
- Unknown gymnosperms: at least 3 species
- Cycadaceae (cycads)
- Magnoliophyta (angiosperms)
- Magnoliopsida (dicots)
- Buxaceae (boxwood)
- at least 1 species
- Gunneraceae (gunneras)
- at least 1 species
- Salicaceae (willows, cottonwood, quaking aspen)
- at least 1 species
- Droseraceae (sundews)
- at least 1 species
- Olacaceae (tallowwood)
- at least 2 species
- Loranthaceae (showy mistletoes)
- at least 1 species
- Sapindaceae (soapberry)
- at least 1 species
- Aceraceae (maples)
- at least 1 species
- Proteaceae (proteas)
- at least 9 species
- Compositae (sunflowers)
- at least 1 species
- Fagaceae (beeches, oaks, chestnuts)
- at least 2 species
- Betulaceae (birches, alders)
- at least 1 species
- Ulmaceae (elms)
- at least 1 species
- Chenopodiaceae (goosefoots)
- at least 1 species
- Buxaceae (boxwood)
- Liliopsida (monocots)
- Liliaceae (lilies)
- at least 6 species
- Cyperaceae (sedges)
- at least 1 species
- Sparganiaceae (bur-reeds)
- possibly 1 species
- Unknown angiosperms: at least 88 species
- Liliaceae (lilies)
- Magnoliopsida (dicots)
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See also
Footnotes
- "Deadlodge Canyon". Canadian Geographical Names Database. Government of Canada. Retrieved 2 February 2025.
- "Berry Creek". Canadian Geographical Names Database. Government of Canada. Retrieved 2 February 2025.
References
References
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