Cloverly Formation | |
---|---|
Stratigraphic range: | |
![]() Brightly colored strata of the Himes Member of the Cloverly Formation near Shell, Wyoming | |
Type | Geological formation |
Sub-units | Pryor Conglomerate, Little Sheep Member, Himes Member |
Underlies | Thermopolis Shale |
Overlies | Morrison Formation |
Thickness | 150–400 ft (46–122 m) |
Lithology | |
Primary | Mudstone |
Other | Conglomerate, sandstone |
Location | |
Region | ![]() ![]() ![]() |
Country | ![]() |
Type section | |
Named for | Cloverly post office, Wyoming |
Named by | Nelson Horatio Darton, 1904 [1] |
The Cloverly Formation is a geological formation of Early and Late Cretaceous age (Valanginian to Cenomanian stage) that is present in parts of Montana, Wyoming, Colorado and Utah in the western United States. It was named for a post office on the eastern side of the Bighorn Basin in Wyoming by N.H. Darton in 1904. [1] [2] The sedimentary rocks of formation were deposited in floodplain environments and contain vertebrate fossils, including a diverse assemblage of dinosaur remains. In 1973, the Cloverly Formation Site was designated as a National Natural Landmark by the National Park Service. [3]
The Cloverly Formation rests disconformably on the Morrison Formation and is conformably overlain by the Thermopolis Shale. It is subdivided into a variety of members, depending on the location. [2] [4] In the Bighorn Basin along the Montana-Wyoming border, Moberly (1960) divided the Cloverly into the following three members:
In contrast, Ostrom (1970) divided the formation into four units, which he named Units IV-VII:
A stratigraphic revision of the Cloverly Formation using new uranium lead dates reinterpret the formation as spanning the Valanginian-Cenomanian stages of the Cretaceous period. The individual ages of the members are listed below: [6]
The sediments of the Cloverly Formation were deposited in alluvial and floodplain environments. The basal conglomerates probably represent braided river deposits, while the sandstones were deposited in fluvial channels. The mudstones that contain most of the fossils represent overbank, lacustrine, and pedogenic deposits. [2] [4] [7]
Animals recovered include the dinosaurs Deinonychus , Microvenator , Tenontosaurus , Zephyrosaurus and Sauropelta as well as fragmentary remains of Titanosaurs, Ankylosaurs and Ornithomimids. As well, two genera of turtle Naomichelys and Glyptops and the lungfish Ceratodus . [8] Dinosaur eggs have been found in Montana. [9]
References for data: Ostrom 1970; Cifelli et al. 1998; Cifelli 1999; Nydam and Cifelli 2002. Possible goniopholidid remains are known from the formation.
Ankylosaurs reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
S. edwardsorum [10] | Known from "several articulated skeletons" and common armor plates. [10] Only one partial skull is known. [11] | Articulated skeletons are often encased in carbonate caliche deposits that require acid to be removed safely. [10] | ![]() | |||
Tatankacephalus [12] | T. cooneyorum [12] |
| Cloverly VII [12] | Partial cranium, rib fragments, and osteoderms. [12] | Originally described as an ankylosaurid but has since been reclassified as a nodosaurid. [13] | |
Ceratopsians reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
A. americanus |
| Cloverly VII; Himes Member [14] | A basal neoceratopsian. | ![]() | ||
Ornithopods reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
T. tilleti [10] | Its remains are the most common of any dinosaur of the formation. [10] | Juvenile remains are sometimes found together, suggesting that young Tenontosaurus lived in sibling groups. Deinonychus teeth are sometimes associated with Tenontosaurus, suggesting a predator-prey relationship between the two. [10] | ![]() ![]() | |||
Z. schaffi [10] |
| Himes Member | Its remains are "very rare." [10] | An orodromine ornithopod. | ||
Theropod eggshell fragments are known from the formation. Unidentifiable ornithomimid remains are present and most commonly represented by toe bones. [10] Indeterminate allosauroid remains are known from the formation. Remains identified by John Ostrom as Ornithomimus are suspected by Jack Horner to be of a new ornithomimid genus. [10] Possible remains of a microraptorian, a troodontid, and a basal tyrannosauroid similar to Moros have also been found here as well.
Color key
| Notes Uncertain or tentative taxa are in small text; |
Sauropods reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
R. cooneyi [16] |
| Cloverly VII; Himes Member [16] | ![]() | |||
Sauroposeidon [17] | S. proteles |
| Cloverly VII; Himes Member [18] |
Theropods reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
Acrocanthosaurus [18] | A. atokensis [18] |
| Cloverly VII; Himes Member [18] | A carcharodontosaurid. | ![]() ![]() ![]() | |
D. antirrhopus [10] | Its remains are "very rare." [10] | A dromaeosaur. Tenontosaurus remains have been recovered in association with Deinonychus teeth, suggesting a predator-prey relationship between the two. [10] | ||||
M. celer [10] | Himes Member | Its remains are "extremely rare." [10] Known only from a "[p]artial skeleton with partial skull." [19] The specimen lacks feet and is catalogued as AMNH 3041. [20] | The type specimen AMNH 3041 [10] was recovered by Barnum Brown from Cloverly strata in Montana in 1933. | |||
O. velox [21] | Later found to be indeterminate ornithomimid remains. [21] | |||||
Mammals reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
A. sp. [22] | Previously referred as "Cloverly triconodont" | ![]() | ||||
cf. Atokatheridium | Indeterminate | |||||
B. sp. | ||||||
C. montanensis | ||||||
G. ostromi | ||||||
J. sp. | ||||||
M. keeblerorum | ||||||
cf. Oklatheridium | Indeterminate | |||||
cf. Paracimexomys | Indeterminate | |||||
Spalacotheriidae | Indeterminate | |||||
Crocodyliforms reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | |
cf. Atoposauridae | Indeterminate | |||||
cf. Bernissartidae | Indeterminate | |||||
cf. Goniopholididae | Indeterminate| | |||||
cf. Pholidosauridae | Indeterminate |
Turtles reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | |
Indeterminate | ||||||
"G". pervicax [10] | ||||||
N. speciosa [10] | ||||||
Indeterminate | ||||||
Lepidosaurs reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | |
P. keebleri | ||||||
Indeterminate | ||||||
P. wilsoni | Also known from the Antlers Formation | |||||
Indeterminate |
Amphibians reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
A. ektopistikon [23] | ![]() | |||||
Anura | Indeterminate | |||||
Batrachosauroididae | Indeterminate | |||||
Indeterminate | ||||||
cf. Scotiophryne | Indeterminate | |||||
Osteichthyes reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
C. frazieri [10] | ![]() | |||||
C. nirumbee [24] | ||||||
aff. Lepidotes | Indeterminate | |||||
aff. Pycnodontidae | Indeterminate | |||||
Indeterminate | ||||||
Chondrichthyes reported from the Cloverly Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | |
E. sp. | ||||||
H. parvidens | ||||||
L. sp. | ||||||
P. sp. | ||||||
P. sp. |
Year designated: 1973