Horseshoe Canyon Formation

The Horseshoe Canyon Formation is a stratigraphic unit of the Western Canada Sedimentary Basin in southwestern Alberta. It takes its name from Horseshoe Canyon, an area of badlands near Drumheller.

The Horseshoe Canyon Formation is part of the Edmonton Group. In its type section (Red Deer River Valley at Drumheller), it is ~250 metres (820 ft) thick, but further west the formation is older and thicker, exceeding 500 metres (1,600 ft) near Calgary. It is of Late Cretaceous age, Campanian to early Maastrichtian stage (Edmontonian Land-Mammal Age), and is composed of mudstone, sandstone, carbonaceous shales, and coal seams. A variety of depositional environments are represented in the succession, including floodplains, estuarine channels, and coal swamps, which have yielded a diversity of fossil material. Tidally-influenced estuarine point bar deposits are easily recognizable as Inclined Heterolithic Stratification (IHS). Brackish-water trace fossil assemblages occur within these bar deposits and demonstrate periodic incursion of marine waters into the estuaries.

The Horseshoe Canyon Formation crops out extensively in the area around Drumheller, as well as farther north along the Red Deer River near Trochu and along the North Saskatchewan River in Edmonton. It is overlain by the Battle and Scollard formations. The Drumheller Coal Zone, located in the lower part of the Horseshoe Canyon Formation, was mined for sub-bituminous coal in the Drumheller area from 1911 to 1979, and the Atlas Coal Mine in Drumheller has been preserved as a National Historic Site. In more recent times, the Horseshoe Canyon Formation has become a major target for coalbed methane (CBM) production.

Dinosaurs found in the Horseshoe Canyon Formation include Albertavenator, Albertosaurus, Anchiceratops, Anodontosaurus, Arrhinoceratops, Atrociraptor, Epichirostenotes, Edmontonia, Edmontosaurus, Hypacrosaurus, Ornithomimus, Pachyrhinosaurus, Parksosaurus, Saurolophus, and Struthiomimus. Other finds have included mammals such as Didelphodon coyi, non-dinosaur reptiles, amphibians, fish, marine and terrestrial invertebrates and plant fossils. Reptiles such as turtles and crocodilians are rare in the Horseshoe Canyon Formation, and this was thought to reflect the relatively cool climate which prevailed at the time. A study by Quinney et al. (2013) however, showed that the decline in turtle diversity, which was previously attributed to climate, coincided instead with changes in soil drainage conditions, and was limited by aridity, landscape instability, and migratory barriers.

The Drumheller Coal Zone has been a primary coalbed methane target for industry. In the area between Bashaw and Rockyford, the Coal Zone lies at relatively shallow depths (about 300 metres) and is about 70 to 120 metres thick. It contains 10 to 20 metres of cumulative coal, in up to 20 or more individual thin seams interbedded with sandstone and shale, which combine to make an attractive multi-completion CBM drilling target. In total, it is estimated there are 14 trillion cubic metres (500 tcf) of gas in place in all the coal in Alberta.

The timeline below follows work by David A. Eberth and Sandra L. Kamo published in 2019.

Anodontosaurus

A. lambei

Horsethief, Morrin, and lowest Tolman

An ankylosaurine ankylosaurid also known from the middle Dinosaur Park Formation and closely related to Ankylosaurus.

Edmontonia

E. longiceps

Upper Horsethief

A panoplosaurin nodosaurid also known from the lower Dinosaur Park Formation and closely related Denversaurus.

Euoplocephalus

E. tutus

Walter Coombs (1971) synonymised Anodontosaurus lambei with E. tutus. However, recent studies suggest that Anodontosaurus is distinct enough from Euoplocephalus to be placed in its own genus and species. Furthermore, all Horseshoe Canyon Formation ankylosaurine specimens were suggested to be reassigned to Anodontosaurus.

Albertavenator

A. curriei

Horsethief

[Two] frontals.

A troodontid theropod that adds to the diversity of North American troodontids.

Albertonykus

A. borealis

Upper Tolman

Ulna, tibiae, metatarsals, manual ungual, pedal phalanxes and unidentified pedal phalanges.

An mononykin alvarezsaurid specialized for digging insect nests.

Apatoraptor

A. pennatus

Horsethief

A palatine, mandibles, ceratobranchials, axis, cervical vertebrae, dorsal vertebrae, pectoral girdles, sternal plate, forelimb, ilium, femur, tibia and fibula.

A caenagnathid oviraptorosaur recovered as sister taxon to Elmisaurus .

Atrociraptor

A. marshalli

Lower Horsethief

Premaxillae, maxilla, dentaries, teeth and numerous bone fragments.

A dromaeosaurid; teeth indicate it may have been present across all members.

Epichirostenotes

E. curriei

Horsethief, Morrin, and Tolman

A maxilla, probable palatine, partial braincase, cervical vertebrae, dorsal vertebrae, caudal vertebrae, synsacrum, an anterior and a posterior cervical rib, a mid-dorsal rib, fragments of ilia, ischium, both pubes, partial tibia, and unidentifiable bones.

A caenagnathid oviraptorosaur known from material previously assigned to Chirostenotes.

Anchiceratops

A. ornatus

Horsethief, Morrin, and Tolman; may have been present in Drumheller

[Two] nearly complete skulls and [seven] partial skulls.

A chasmosaurine ceratopsid contemporaneous and closely related to Arrhinoceratops.

Arrhinoceratops

A. brachyops

Horsethief

A nearly complete skull.

A chasmosaurine ceratopsid restricted to the holotype specimen as Farke (2007) assigned the referred specimen ROM 1439 to Torosaurus.

Eotriceratops

E. xerinsularis

Carbon

Premaxillae, maxillae, rostral, supraorbital horncore with lacrimal, prefrontal, frontal, postorbital, jugal, epijugal, quadratojugal, quadrate, partial parietal, squamosal frill, braincase, syncervical, cervical vertebrae, dorsal vertebrae, ribs and fragments of ossified ligaments.

A large chasmosaurine ceratopsid that may represent a senior synonym of Ojoceratops from the Ojo Alamo Formation.

Montanoceratops

M. cerorhynchus

Upper Tolman

An isolated braincase.

A leptoceratopsid ceratopsian also known from the St. Mary River Formation.

Pachyrhinosaurus

P. canadensis

Drumheller and Horsethief

[Two] partial skulls.

A centrosaurine ceratopsid also known from the St. Mary River Formation.

Sphaerotholus

S. edmontonense

Tolman

A frontoparietal.

A pachycephalosaurine pachycephalosaurid also known from the Hell Creek and Kirtland Formation.

Ornithomimus

O. currelli

Junior synonym of O. edmontonicus

O. edmontonicus

Drumheller, Horsethief, Morrin, and Tolman

Several specimens, type specimen

An ornithomimid

Struthiomimus

S. altus

Drumheller, Horsethief, and Morrin

An ornithomimid

Edmontosaurus

E. regalis

Horsethief; likely present in Drumheller.

Hypacrosaurus

H. altispinus

Morrin and Tolman.

"[Five to ten] articulated skulls, some associated with postcrania, isolated skull elements, isolated postcranial elements, many individuals, embryo to adult."

Parksosaurus

P. warreni

Tolman

Type specimen

Saurolophus

S. osborni

Upper Morrin and Tolman.

"Complete skull and skeleton, [two] complete skulls."

Albertosaurus

A. arctunguis

Junior synonym of A. sarcophagus

A. sarcophagus

Horsethief, Morrin, and Tolman; likely present in Drumheller and Carbon.

Several skeletons and partial skeletons, type specimen

A tyrannosaurid which was the most common large carnivore in the area.

Daspletosaurus

D. sp.

Suggested from the skeleton of an immature tyrannosaurid (CMN 11315), thorough analysis of this specimen supports a referral to A. sarcophagus. An isolated maxilla and teeth from an Edmontosaurus bonebed were also mistakenly referred to Daspletosaurus, however all the tyrannosaurid material in the bonebed was confirmed to belong to A. sarcophagus.

Didelphodon

D. coyi

a stagodontid metatherian

Stangerochampsa

S. mccabei

"a skull, partial lower jaws, and partial postcranial skeleton"

An alligatoroid

Champsosaurus

C. albertensis

"partial skeleton with partial skull"

a choristodere

Leurospondylus

L. ultimus

"a partial skeleton"

a plesiosaur of uncertain classification

Basilemys

B. morrinensis

"nearly complete shell"

a nanhsiungchelyid turtle

Horseshoeichthys

H. armaserratus

An ellimmichthyiform