This is an overview of the fossil flora and fauna of the Maastrichtian-Danian Hell Creek Formation.
Insects from the groups Diptera, Zygoptera, and possibly Hemiphlebiidae have been unearthed in Hell Creek in amber. [1] [2] Fossils found in the Hell Creek Formation and the Fort Union Formation of these insects went extinct during the K-T Event. [3] [4] [5]
Color key
| Notes Uncertain or tentative taxa are in small text; |
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
---|---|---|---|---|---|---|
Possible hispine beetle herbivory on Zingiberopsis attenuta | ||||||
Indeterminate | Possible Hemiphlebiid damselflies | |||||
Indeterminate | Undescribed brachyceran flies | |||||
Indeterminate | Undescribed nematoceran flies | |||||
Indeterminate | Indeterminate aeschnidiid dragonflies | |||||
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
---|---|---|---|---|---|---|
Plesielliptio | Freshwater Unionid river mussels | |||||
Freshwater Unionid river mussels | ||||||
Freshwater Unionid river mussels | ||||||
Rhabdotophorus | R. aldrichi | Freshwater mussel of family Unionidae. [7] | ||||
Pleurobema | P. cryptorhynchus | Freshwater mussel of family Unionidae. [7] | ||||
Plethobasus | P. aesopiformis | Freshwater mussel of family Unionidae. [7] | ||||
P. biesopoides | ||||||
Quadrula | Q. cylindricoides | Freshwater mussel of family Unionidae. [7] | ||||
Proparreysia | P. verrucosiformis | Freshwater mussel of family Unionidae. [7] | ||||
P. holmesiana | ||||||
P. barnumi | ||||||
P. percorrugata | ||||||
P. pyramidatoides | ||||||
P. letsoni | ||||||
P. retusoides | ||||||
P. corbiculoides | ||||||
P. paucinodosa | ||||||
?Obovaria | ?O. pyramidella | |||||
Corbicula | C. cf. subelliptica | |||||
C. sp | South Dakota | From a marine facies ("tongue"). Modern members of the genus live in fresh water | ||||
Sphaerium | S. beckmani | "Pill clam". "Nut clam". "Fingernail clam". "Pea clam". Family Sphaeriidae. | ||||
Pleiodon | Indeterminate | |||||
Campeloma | C. sp | Freshwater snail | ||||
Anomia | A. gryphorhyncha | Bivalve. Family Anomiidae. From a marine facies ("tongue") in South Dakota. | ||||
Crassostrea | C. subtrigonalis | Oyster. Family Ostreidae. Collected from a marine facies ("tongue") in South Dakota. | ||||
Granocardium | G. sp | Bivalve. Family Cardiidae (cockle). Collected from a marine facies ("tongue") in South Dakota. | ||||
?Hiatella | ?H. sp | Bivalve. Present members of this genus are rock borers. Collected from a marine facies ("tongue") in South Dakota. | ||||
Leptosolen | indeterminate | Bivalve. Family Cultellidae. Collected from a marine facies ("tongue") in South Dakota. | ||||
Sphenodiscus | S. lenticularis | Ammonite. From a marine facies ("tongue") in South Dakota. | ||||
Discoscaphites | D. rossi | Microconch of an ammonite. From a marine facies ("tongue") in South Dakota. | ||||
Scaphitidae | indeterminate | Ammonite. From a marine facies ("tongue") in South Dakota. Other attributes: specimen has hooks on its shell. | ||||
Color key
| Notes Uncertain or tentative taxa are in small text; |
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
---|---|---|---|---|---|---|
indeterminate [8] | Middle to upper Hell Creek Formation [10] | 3 unassigned specimens [11] | Anura indet. consists of material not currently assigned to any genus of frog. [8] | |||
Indeterminate [13] |
| |||||
Caudata (salamander) [8] | indeterminate [8] | Lower to uppermost Hell Creek Formation [10] | 149 unassigned specimens [11] | Material of Caudata indet. is not currently assigned to any genus. [8] | ||
Indeterminate [13] |
| |||||
Middle to upper Hell Creek Formation [10] | 6 specimens [11] | |||||
L. bairdi [13] |
| |||||
Lower to upper Hell Creek Formation [10] | 22 specimens [11] | Opisthotriton is classified as a Batrachosauroididae. [8] | ||||
P. garbanii [16] |
| |||||
P. cretacica [13] |
| |||||
P. copei [13] |
| |||||
Lower to upper Hell Creek Formation [10] | 144 specimens [11] | Scapherpeton is a scapherpetonid that is very common in the Hell Creek Formation. [8] | ||||
S. pustulosa [13] |
| A small frog |
Bony fishes | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images | |
Acipenser [8] [17] [18] | A. amnisinferos [18] | A sturgeon | |||||
A. eruciferus [17] |
| ||||||
A. praeparatorum [18] |
| ||||||
A. cf. A. amnisinferos [18] |
| ||||||
cf. A. sp. [8] | Lower to upper Hell Creek Formation [10] | 18 specimens are tentatively assigned to Acipenser sp. [11] | Acipenser sp. is tentatively referred to the genus. [8] | ||||
Anchiacipencer [20] | A. acanthaspis [20] |
| A sturgeon, originally considered as indeterminate material [20] | ||||
Belonostomus [8] [17] | B. longirostris [8] [17] | Lower to upper Hell Creek Formation [10] | 28 specimens [11] | A long-snouted slender fish classified as an aspidorhynchid. [8] | |||
Coriops [21] | C. amnicolus [21] |
| |||||
C. fragosus [17] | A small amiid fish (ubiquitous). Previously known as Amia fragosa or Kindleia fragosa. [23] 2610 specimens have been assigned to Kindleia, making it an extremely common genus. [11] | ||||||
" Lepisosteus " [8] [17] | "L. occidentalis" [8] [17] | Lower to uppermost Hell Creek Formation [10] | 938 specimens are assigned to Lepidosteus [11] | A lepidosteid that is very common in the Hell Creek Formation. [8] Nomen dubium . [24] | |||
Melvius [8] | M. thomasi [8] | Lower to upper Hell Creek Formation [10] | 6 specimens are assigned to Melvius [11] | A large amiid fish. [8] | |||
Phyllodus | P. paulkatoi | Fish with columnar teeth | |||||
Palaeolabrus [17] | P. montanensis [17] |
| |||||
Paleopsephurus [17] | P. wilsoni [17] |
| A paddlefish | ||||
Paralbula [25] | P. casei [25] |
| |||||
Parapsephurus [26] | P. willybemisi [26] |
| A paddlefish | ||||
Platacodon [21] | P. nanus [21] |
| Small teleost fish | ||||
Protamia [17] | Indeterminate [17] |
| |||||
Pachyrhizodontoidei | Indeterminate | Fish | |||||
Polyodontidae [27] | Indeterminate [27] |
| Paddlefish | ||||
Protoscaphirhynchus [17] | P. squamosus [17] |
| A sturgeon | ||||
Pugiopsephurus [26] | P. inundatus [26] |
| A paddlefish | ||||
Chondrichthyes reported from the Hell Creek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
C. sp. [28] | A member of Hemiscylliidae. [28] | |||||
G. nordquistae |
| Isolated teeth | ||||
L. selachos [30] | Lower to upper Hell Creek Formation [10] | 40 specimens [11] | A genus of prehistoric sharks in the family Hybodontidae. It makes up 0.4% of the remains of the vertebrates of the Hell Creek Formation. [8] | |||
M. pustulosus [28] | Lower to upper Hell Creek Formation. [10] | 1677 specimens [11] previously assigned to M. bipartitus. [28] | Is an anacoracid batoid [8] rajiform related to guitarfishes. [28] Described on the basis of teeth formerly assigned to the species M. bipartitus. [28] The material assigned to Myledaphus bipartitus and makes up 16.5% of the vertebrate remains. [8] | |||
P. estesi [28] | A member of Ginglymostomatidae. [28] Formerly assigned to the genus Brachaelurus . | |||||
R. americana [28] | Middle Hell Creek Formation [10] | 5 specimens previously assigned to Squatirhina [11] | A wobbegong-like shark. [28] Formerly assigned to Squatirhina. The remains consist of 0.05% of the vertebrates. [11] Also known from the Lance Formation. [28] | |||
Carcharhinidae indet. [29] | Indeterminate |
| An isolated tooth. | |||
.sp. |
| |||||
A paleo-population study is one of the most difficult of analyses to conduct in field paleontology. Here is the most recent estimate of the proportions of the eight most common dinosaurian families in the Hell Creek Formation, based on detailed field studies by White, Fastovsky and Sheehan. [33]
Outcrops sampled by the Hell Creek Project were divided into three sections: lower, middle and upper slices. The top and bottom sections were the focus of the PLoS One report, and within each portion many remains of Triceratops , Edmontosaurus , and Tyrannosaurus were found. Triceratops was the most common in each section, but, surprisingly, Tyrannosaurus was just as common, if not slightly more common, than the hadrosaur Edmontosaurus. In the upper Hell Creek section, for example, the census included twenty two Triceratops, five Tyrannosaurus, and five Edmontosaurus.
The dinosaurs Thescelosaurus , Ornithomimus , Pachycephalosaurus and Ankylosaurus were also included in the breakdown, but were relatively rare. Other dinosaurs, such as Sphaerotholus, Denversaurus, Torosaurus, Struthiomimus, Acheroraptor, Dakotaraptor, Pectinodon,Richardoestesia, Paronychodon, Anzu, Leptorhynchos and Troodon (more likely Pectinodon), were reported as being rare and are not included in the breakdown.
The dinosaur collections made over the past decade during the Hell Creek Project yielded new information from an improved genus-level collecting schema and robust data set that revealed relative dinosaur abundances that were unexpected, and ontogenetic age classes previously considered rare. We recognize a much higher percentage of Tyrannosaurus than previous surveys. Tyrannosaurus equals Edmontosaurus in U3 and in L3 comprises a greater percentage of the large dinosaur fauna as the second-most abundant taxon after Triceratops, followed by Edmontosaurus. This is surprisingly consistent in (1) the two major lag deposits (MOR loc. HC-530 and HC-312) in the Apex sandstone and Jen-rex sand where individual bones were counted and (2) in two thirds of the formation reflected in L3 and U3 records of dinosaur skeletons only.
Triceratops is by far the most common dinosaur at 40% (n = 72), Tyrannosaurus is second at 24% (n = 44), Edmontosaurus is third at 20% (n = 36), followed by Thescelosaurus at 8% (n = 15), Ornithomimus at 5% (n = 9), and Pachycephalosaurus and Ankylosaurus both at 1% (n = 2) are relatively rare.
Fossil footprints of dinosaurs from the Hell Creek Formation are very rare. As of 2017, there is only one find of a possible Tyrannosaurus rex footprint, dating from 2007 and described a year later. [34] A trackway made by mid-sized theropod, possibly a small tyrannosaurid individual, was discovered in South Dakota in 1997, and in 2014 these footprints were named Wakinyantanka styxi . [35]
Indeterminate nodosaur remains have been unearthed in the Hell Creek Formation and other nearby areas. [36] [37]
Ankylosauria reported from the Hell Creek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
A. magniventris [38] |
| Upper | A partial skull, teeth, cervical vertebrae, dorsal vertebrae, caudal vertebrae, right scapulocoracoid, otic capsule, maxilla fragment, right jugal, left jugal and quadratojugal, sacral centra, additional fragments of the cervical half rings and a partial tail club handle. | An ankylosaur. Also found in the Lance, Frenchman, Ferris and Scollard Formations. | ||
D. schlessmani [38] | Skull roof, pelvis and osteoderms. | A nodosaurid ankylosaur whose remains have been found in the Lance and Laramie Formation. [36] | ||||
An undescribed and unnamed pachycephalosaur is present in North Dakota. [40] Pachycephalosaur remains have been unearthed in Montana as in the case of Platytholus and the now invalid genus Stenotholus kohleri, which is now a junior synonym of Pachycephalosaurus. [41]
Pachycephalosaurs reported from the Hell Creek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
D. hogwartsia [42] |
|
| A pachycephalosaur, possibly synonymous with Pachycephalosaurus . | |||
P. wyomingensis [38] | A pachycephalosaur. Also found in the Lance Formation. | |||||
Platytholus [43] | P. clemensi [43] |
|
| A partial skull [43] | A medium-sized pachycephalosaurine closely related to Acrotholus and Prenocephale | |
S. buchholtzae [38] |
| "Skull material." [46] | A pachycephalosaur whose remains have also been found in the Frenchman Formation. Genus also known from the Kirtland Formation, Dinosaur Park Formation and the Horseshoe Canyon Formation. | |||
S. triregnum [45] |
|
| A left squamosal. [45] | A pachycephalosaur distinguished from S. buchholtzae by its more ornamented squamosal. [45] | ||
S. spinifer [38] |
| A pachycephalosaur, possibly synonymous with Pachycephalosaurus . Also found in the Ferris Formation and the Lance Formation. | ||||
Indeterminate ceratopsid teeth and some identifiable bones from Triceratops can be extremely common. [47] [48] [49] [50] [51] 8.31% of all vertebrate remains from the Hell Creek Formation are unassigned ceratopsids. [11] In 2012, a new unidentified species of chasmosaur ceratopsian with noticeable differences from Triceratops was unearthed in South Dakota by a fossil hunter named John Carter. [52] [53] [54]
Color key
| Notes Uncertain or tentative taxa are in small text; |
Ceratopsians reported from the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | Synonyms | State | Stratigraphic position | Material | Notes | Images |
L. gracilis [38] |
| A small primitive-looking ceratopsian. Fossils have also been found in the Lance Formation in Wyoming. [55] | |||||
T. sacrisonorum [56] |
| A controversial ceratopsian possibly synonymous with Triceratops [57] | |||||
Upper Hell Creek Formation [10] | A ceratopsian that was once proposed to be synonymous with Triceratops, [58] but is now regarded as a valid and distinct ceratopsian. [59] A rare ceratopsid. [10] Fossils have been in the Lance Formation, Javelina Formation, North Horn Formation, Laramie Formation, El Picacho Formation, Frenchman Formation and Scollard Formation. | ||||||
Lowermost to the middle Hell Creek Formation [61] | Four specimens are assigned to Triceratops horridus from the Hell Creek Formation. [11] Isolated, shed ceratopsid teeth are incredibly common in the Hell Creek and Lance Formations, being by most collectors, with some being nothing more than worn down fragments up to superb teeth containing complete, preserved roots. Because the teeth of different ceratopsians are so similar to one another, its hard to differentiate between genera/species, but based on the abundance of identifiable bones belonging to Triceratops in Lancian-aged North American formations, especially the Hell Creek, isolated ceratopsid teeth from the lower and middle Hell Creek Formation have a high likelihood of originating from T. horridus. | A ceratopsian. [8] Also found in the Evanston, Frenchman, Lance, Laramie, and Scollard Formations. | |||||
T. prorsus [38] |
| Upper 1/3 of the Hell Creek Formation [61] | Very common.[ citation needed ] Because the teeth of different ceratopsians are so similar to one another, its hard to differentiate between genera/species, but based on the abundance of identifiable bones belonging to Triceratops in Lancian-aged North American formations, especially the Hell Creek, isolated ceratopsid teeth from the upper 1/3 of the Hell Creek Formation have a high likelihood of originating from T. prorsus. | Also found in the Frenchman and Lance Formations. | |||
Indeterminate hadrosaurid remains are very common in the Hell Creek Formation. [8]
Ornithopods and Thescelosaurs reported from the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | Synonyms | State | Stratigraphic position | Material | Notes | Images |
E. annectens | Very common. | A hadrosaur. Also found in the Denver, Frenchman, Lance, Laramie, and Scollard Formations. [65] [66] Hatchlings have also been unearthed. [66] | |||||
| |||||||
Lower to upper Hell Creek Formation [10] | 50 specimens [11] | A small thescelosaurine. Also found in the Frenchman, Lance, Laramie, and Scollard Formations. [70] Two species are known from Hell Creek; T. neglectus and T. garbanii. [71] | |||||
Theropod tracks have been found in South Dakota. [39] A trackway from South Dakota, named Wakinyantanka, was made by a mid-sized theropod with three slender toes, possibly a small tyrannosaurid. [35] A second footprint that may have been made by a specimen of Tyrannosaurus was first reported in 2007 by British paleontologist Phil Manning, from the Hell Creek Formation of Montana. [72] This second track measures 72 centimeters (28 in) long, shorter than the track described by Lockley and Hunt. Whether or not the track was made by Tyrannosaurus is unclear, though Tyrannosaurus is the only large theropod known to have existed in the Hell Creek Formation, though in past albertosaurine remains have described here but its most likely that they are the remains of Tyrannosaurus rex. [73] [74] Theropod remains are very common in Hell Creek, some of which belong to indeterminate species on maniraptorans. [75]
Alvarezsaurs reported from the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | Synonyms | State | Stratigraphic position | Material | Notes | Images |
"Ornithomimus" | "O." minutus | ||||||
T. prairiensis [76] |
| upper Hell Creek Formation. | An alvarezsaur known from a partial post-cranial skeleton. [77] | ||||
Tyrannosaurids reported from the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | Synonyms | State | Stratigraphic position | Material | Notes | Images |
| Lower to upper Hell Creek Formation. | A tyrannosaur, known from several specimens including a juvenile nicknamed "Jane". [78] Also found in the Denver, Frenchman, Hill Creek South, Javelina, Lance, Ferris, Livingston, McRae, North Horn, Scollard, Willow Creek Formation, and also found in Lomas Coloradas Formations. Isolated teeth in the Hell Creek are common enough to be dug commercially by collectors, but rare enough that they are often sold for very high prices with fragmentary teeth usually beginning at least in the hundreds of USD, and complete teeth in the thousands of USD. Perhaps the best known iconic dinosaur. | |||||
|
| Lower to upper Hell Creek Formation. | A few specimens are known | Invalid genus, now recognised as juvenile T. rex. |
Ornithomimid remains are not uncommon in the Hell Creek Formation. [8] Fifteen specimens from the Hell Creek Formation are undetermined ornithomimids [11]
Color key
| Notes Uncertain or tentative taxa are in small text; |
Ornithomimids reported from the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images | |
unnamed |
| One partial skeleton. | An ornithomimid; nomen nudum . | ||||
S. sedens [80] |
|
| A large ornithomimid similar to Gallimimus in size. Also found in the Lance Formation. [80] | ||||
O. velox [80] |
| Fragmentary specimens | An ornithomimid which was also found in the Denver Formation. | ||||
Oviraptorosaur fossils have been found at the Hell Creek Formation for many years, most notably from isolated elements until the discovery of Anzu. In the past, oviraptorosaur fossils found were thought to have belonged to Caenagnathus , Chirostenotes , and Elmisaurus . [38] [81] [82] [83] [84] In 2016, an undescribed large-bodied caenagnathid was unearthed in Montana. [85]
Color key
| Notes Uncertain or tentative taxa are in small text; |
Oviraptorosaurs reported from the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images | |
A. wyliei [81] | Lower to upper Hell Creek Formation [11] | 12 well-preserved specimens [10] | One of the largest known oviraptorosaurs, and the largest known from North America. Material previously assigned to Caenagnathidae indet. is now placed in the genus Anzu. [81] | ||||
Indeterminate |
| Similar to Citipes and Elmisaurus. | |||||
Eoneophron | E. infernalis |
| A partial right hindlimb [86] | Closely related to Citipes and Elmisaurus. [86] | |||
Historically, numerous teeth have been attributed to various dromaeosaurid and troodontid taxa with known body fossils from only older formations, including Saurornithoides , Zapsalis , Dromaeosaurus , Saurornitholestes , and Troodon . However, in a 2013 study, Evans et al. concluded that there is little evidence for more than a single dromaeosaurid taxon, Acheroraptor , in the Hell Creek-Lance assemblages, which would render these taxa invalid for this formation. This was disproved in a 2015 study, DePalma et al., when they described the new genus Dakotaraptor , a large species of dromaeosaur. [87] Fossilized teeth of various troodontids and coelurosaurs are common throughout the Hell Creek Formation; the best known examples include Paronychodon , Pectinodon and Richardoestesia , respectively. Teeth belonging to possible intermediate species of Dromaeosaurus [88] and Saurornitholestes [89] have been unearthed at the Hell Creek Formation and the nearby Lance Formation.
Eumaniraptorans reported from the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images | |
A. temertyorum [87] | Lower? to upper Hell Creek Formation [8] | A velociraptorine dromaeosaurid. Teeth previously referred to various Campanian dromaeosaurids Saurornitholestes and Dromaeosaurus, frequently found throughout the formation, probably belong to this one species. Evans et al. conclude that there is little evidence for the former two taxa being present in the Hell Creek-Lance assemblages. [87] | |||||
| Middle Hell Creek Formation [10] |
| |||||
cf. A. archibaldi [90] |
| Uppermost Hell Creek Formation [90] |
| An avisaurid tentatively referred to A. archibaldi based on its size. [90] | |||
A. darwini [91] |
|
| |||||
A. sp. [92] |
|
| |||||
B. baileyi [93] |
|
| A primitive hesperornithiform. [93] | ||||
D. steini [94] |
| Upper Hell Creek Formation [94] | A large dromaeosaurid. [87] | ||||
Magnusavis [91] | M. ekalakaensis |
|
| A large enantiornithine closely related to avisaurids. | |||
P. caperatus [95] |
|
| A troodontid theropod who is known from fossil teeth. Fossils have also been found in the Lance Formation in Wyoming. | ||||
|
|
| |||||
Potamornis [93] | P. skutchi [97] |
|
| A hesperornithiform also found in the Lance Formation. [97] | |||
|
| A coelurosaur that is known from teeth and from two species Richardoestesia gilmorei and Richardestesia isosceles, which have also been unearthed in the Lance Formation in Wyoming. | |||||
"Styginetta" [100] | "S. lofgreni." |
| A Presbyornithid, it is notable for being one of the few birds known to have survived the Cretaceous–Paleogene extinction event. | ||||
"Unnamed enantiornithine B" [90] | Unnamed |
|
| An unnamed enantiornithean. [90] | |||
"Unnamed hesperornithiform A" [90] | Unnamed |
|
| A primitive hesperornithiform. [93] The Hell Creek specimen was referred to the same unnamed taxon as RSM P 2315.1 from the Canadian Frenchman Formation. [90] RSM P 2315.1 was later made the holotype of Brodavis americanus. [93] May be a synonym of Potamornis . [90] | |||
"Unnamed ornithurine B" [90] | Unnamed [101] |
|
| An ornithurine possibly similar to Cimolopteryx [90] [101] | |||
"Unnamed ornithurine C" [90] | Unnamed | An ornithurine, also present in the Lance Formation and Fort Union Formation, one of the few individual bird species known to have survived the Cretaceous–Paleogene extinction [90] | |||||
"Unnamed ornithurine D" [90] | Unnamed |
|
| An ichthyornithean also present in the Frenchman Formation [90] |
Undescribed pterosaur remains were reported from North Dakota. [103] A specimen of an azhdarchid pterosaur from Montana likely belongs to Quetzalcoatlus , though it is not diagnostic to the species level. [103]
Pterosaurs of the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Taxa | Species | State | Stratigraphic location | Material | Notes | Images | |
Indeterminate | Montana [103] | A single azhdarchid neck bone which may belong to the genus Quetzalcoatlus . [103] | |||||
Color key
| Notes Uncertain or tentative taxa are in small text; |
Crocodylomorphs reported from the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images | |
|
| Extinct genus of crocodylians that lived from the Late Cretaceous to the Eocene in North America. | |||||
|
| Extinct genus of alligatoroid. | |||||
|
| Extinct genus of gavialoid crocodilian which existed during the Late Cretaceous and early Paleocene. |
Color key
| Notes Uncertain or tentative taxa are in small text; |
Turtles reported from the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images | |
Indeterminate [105] |
| Extinct genus of aquatic turtles belonging to the family Adocidae. | |||||
A. infernalis [107] |
| A turtle belonging to the family Trionychidae. Its fossils from the Hell Creek Formation were formerly assigned to the late Campanian species Axestemys splendidus. [108] [107] | |||||
C. victa [105] |
| A relative of Dermatemydidae. | |||||
P. brinkman |
| A relative of Baenidae. | |||||
E. cretacea |
| A relative of chelydrids. [109] | |||||
E. cephalica [105] |
| ||||||
G. sonsalla |
| ||||||
P. cohen |
| A relative of extinct family of cryptodiran turtles. | |||||
C. putorius |
| A relative of Baenidae. | |||||
G. lancensis |
| Trionychidae related to the softshell turtle. | |||||
H. clark [109] |
| A kinosternoid related to the Central American river turtle. [109] | |||||
Hutchemys [110] | H. walkerorum [110] |
| A shell [110] | A Plastomeninae related to the softshell turtle. [110] | |||
P. sp | |||||||
B. sinuosa | Largest dermatemydid land tortoise. | ||||||
Indeterminate [105] |
| A genus of softshell turtles belonging to the family Trionychidae. | |||||
A. foveatus | |||||||
H. distincta | |||||||
J. backmani | Thin-shelled macrobaenid turtle. | ||||||
P. antiqua | |||||||
S. estesi | |||||||
N. eximius | |||||||
S. gilberti |
|
| A member of the family Baenidae. | ||||
T. insiliens | |||||||
Indeterminate | Chelydrids-like turtle. |
Color key
| Notes Uncertain or tentative taxa are in small text; |
Squamates reported from the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images | |
| A platynotan lizard of uncertain phylogenetic placement, also known from the Lance Formation. [112] | ||||||
| An alethinophidian snake of uncertain phylogenetic placement. [112] | ||||||
| A polyglyphanodontian lizard of uncertain phylogenetic placement. Also known from the Lance Formation. [112] | ||||||
P. aquilonius [112] |
| A chamopsiid polyglyphanodontian lizard. [112] | |||||
H. placodon | |||||||
L. denticulatus | |||||||
C. segnis | |||||||
C. sloani | |||||||
E. lancensis | |||||||
P. jepseni | |||||||
P. wyomingensis | Necrosaurid lizard. | ||||||
P. bogerti | |||||||
P. canadensis | A large Monstersauria lizard, closely related to today's varanid lizards. It was the largest lizard in the Hell Creek formation. | ||||||
Indeterminate | |||||||
Indeterminate | Indeterminate mosasaur remains have been unearthed in North Dakota; they may belong to a mosasaur measuring 11 m (36 ft) in length. [114] [115] | ||||||
Color key
| Notes Uncertain or tentative taxa are in small text; |
Choristoderans reported from the Hell Creek Formation | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images | |
C. sp. [104] |
| A champsosaur. |
Color key
| Notes Uncertain or tentative taxa are in small text; |
Multituberculates reported from the Hell Creek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
C. minor [116] |
| A multituberculate of uncertain phylogenetic placement. | ||||
C. nitidus |
| A cimolodontid multituberculate. | ||||
C. cf. nitidus [116] |
| A cimolodontid multituberculate. | ||||
C. sp. [116] |
| A cimolodontid multituberculate. | ||||
C. gracilis |
| A cimolomyid multituberculate. | ||||
|
| A cimolomyid multituberculate. | ||||
E. browni [116] |
| A cimolomyid multituberculate. | ||||
M. conquistus |
| A cimolomyid multituberculate. | ||||
M. robustus |
| A cimolomyid multituberculate. | ||||
M. cf. robustus |
| A cimolomyid multituberculate. | ||||
M. sp. |
| A cimolomyid multituberculate. | ||||
?M. sp. [116] |
| A cimolomyid multituberculate. | ||||
M. formosa |
| A neoplagiaulacid multituberculate. | ||||
M. cf. formosa |
| A neoplagiaulacid multituberculate. | ||||
M. hensleighi |
| A neoplagiaulacid multituberculate. | ||||
M. cf. hensleighi |
| A neoplagiaulacid multituberculate. | ||||
M. thompsoni |
| A neoplagiaulacid multituberculate. | ||||
M. cf. thompsoni |
| A neoplagiaulacid multituberculate. | ||||
M sp. [116] |
| A neoplagiaulacid multituberculate. | ||||
?M sp. [116] |
| A neoplagiaulacid multituberculate. | ||||
?N. burgessi [116] |
| A neoplagiaulacid multituberculate. | ||||
P. priscus [116] |
| A multituberculate of uncertain phylogenetic placement. | ||||
P. nelsoni [117] | A cimolomyid multituberculate. | |||||
S. kuszmauli |
| It was a member of the extinct order Multituberculata. | ||||
Color key
| Notes Uncertain or tentative taxa are in small text; |
Metatherians reported from the Hell Creek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
A. marshi |
| An alphadontid. genus of small, primitive mammal that was a member of the Metatheria, a group of mammals that includes modern-day marsupials. | ||||
A. cf. marshi |
| An alphadontid. | ||||
A. wilsoni |
| An alphadontid. | ||||
A. cf. wilsoni |
| An alphadontid. | ||||
A. sp. [116] |
| An alphadontid. | ||||
D. padanicus |
| A stagodontid. | ||||
D. vorax |
| A stagodontid. genus of Stagodontidae marsupials from the Late Cretaceous of North America. | ||||
D. cf. vorax |
| A stagodontid. | ||||
D. sp. |
| A stagodontid. | ||||
cf. D. sp. [116] |
| A stagodontid. | ||||
G. twitchelli |
| A glasbiid. | ||||
G. cf. twitchelli [116] |
| A glasbiid. | ||||
L. cooki |
| A pediomyid. | ||||
L. krejcii [118] |
| A pediomyid. | ||||
N. improvida [117] | ||||||
| ||||||
P. elegans [116] |
| A pediomyid. | ||||
P. foxi |
| An alphadontid. | ||||
P. lulli [116] |
| An alphadontid. | ||||
Protolambda [118] [120] |
| A pediomyid. | ||||
P. hatcheri [118] [120] |
| A pediomyid. | ||||
P. mcgilli [121] |
| A pediomyid. | ||||
T. rhaister [116] |
| An alphadontid. |
Color key
| Notes Uncertain or tentative taxa are in small text; |
Eutherians reported from the Hell Creek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | State | Stratigraphic position | Material | Notes | Images |
A. magnus |
| a possible creodont, formerly a species of Cimolestes [122] | ||||
A. saskatchewanensis [116] |
| A eutherian of uncertain phylogenetic placement. | ||||
A. cerberoides |
| A eutherian of uncertain classification, formally a species of Cimolestes | ||||
B. tenuis [116] |
| A cimolestid eutherian. | ||||
C. incisus |
| A cimolestid eutherian. | ||||
C. stirtoni [116] |
| A cimolestid eutherian. | ||||
G. hypoconus |
| A gypsonictopsid eutherian. | ||||
G. illuminatus |
| A gypsonictopsid eutherian. | ||||
G. cf. illuminatus |
| A gypsonictopsid eutherian. | ||||
G. sp. [116] |
| A gypsonictopsid eutherian. | ||||
cf. Paranyctoides [116] | cf. Paranyctoides sp. [116] |
| A nyctitheriid eutherian. | |||
P. coombsi [118] |
| A stem-placental. | ||||
P. ceratops |
| A genus with four species believed to be either stem-placentals or stem-primates. | ||||
S. propalaeoryctes |
| A eutherian of uncertain classification, formally a species of Cimolestes |
The Hell Creek Formation was a low floodplain at the time before the sea retreated, and in the wet ground of the dense woodland, the diversity of angiosperms and conifers were present. An endless diversity of herbaceous flowering plants, ferns and moss grew in the forest understory. On the exposed point bars of large river systems, there were shrubs and vines. The evidence of the forested environment is overwhelmingly supported by petrified wood, rooted gley paleosols, [123] and ubiquitous tree leaves. The presence of the simple and lobed leaves, combined with an extremely high dicot diversity, extinct cycadeoid Nilssoniocladus , Ginkgo , many types of monocots, and several types of conifers is different from any modern plant community. There are numerous types of leaves, seeds, flowers and other structures from Angiosperms, or flowering plants. The Hell Creek Formation of this layer contains over 300 tablets, of which angiosperms are by far the most diverse and dominant flora of the entire population, about 90 percent, followed by about 5% of conifers, 4% of ferns, and others. Compared to today Hell Creek's flora which is prairie, then Hell Creek's flora was hardwood forest mixed with deciduous and evergreen forest. In sharp contrast to the Great Plains today, the presence of many thermophilous taxa such as palm trees and gingers meant the climate was warmer and wetter then.
The plants of the Hell Creek Formation generally represent angiosperm-dominated riparian forests of variable diversity, depending on stratigraphic position and sedimentary environment. There appears to be floral transitions visible on a stratigraphic range from the lower to the upper Hell Creek Formation. For this reason, Kirk Johnson and Leo Hickey divided it into five zones and described them as HCIa, HCIb, HCIIa, HCIIb, and HCIII as a reflection of floral change through time. [124] For example, the HCIa zone is dominated by "Dryophyllum" subfalcatum , Leepierceia preartocarpoides, "Vitis" stantonii , and "Celastrus" taurenensis , and is located 55 to 105 meters below the K-Pg boundary layer. Although the HCIb zone is a very thin layer, about 5 meters of rock, it bears unusually high diversity of herbaceous and shrubby plants, including Urticaceae, Ranunculaceae, Rosaceae, and Cannabaceae. [125] [126]
There is evidence of transitional floras in the middle of the Hell Creek Formation as shown by HCII and HCIII zones. The HCII flora represents a transitional period where taxa from the lower Hell Creek are replaced by the HCIII flora. The diversity of the HCIII zone is very high, and its composition is more uniform than that of HCII, many of which were rare or absent from the zones below, and some others that used to be common below became rarer in the HCIII zone. These forms include Elatides longifolia , "Dryophyllum" tennessensis , Liriodendrites bradacii , and many members of the Laurales including Bisonia niemii , "Ficus" planicostata , and Marmarthia trivialis , while "Celastrus" taurenensis , Leepierceia preartocarpoides , and many cupressaceous conifers became rarer. This phenomenon suggests that the global temperature was warming during the last 300,000-500,000 years of the Cretaceous period. [125] [126] [127] [128]
Johnson claims that there are no grasses, oaks, maples, beeches, figs, or willows in the Hell Creek Formation. There is no evidence of fern prairie either. [129] However, there was an extremely high angiosperm diversity — common plane trees, "Dryophyllum" subfalcatum , Leepierceia preartocarpoides , and palm trees — along with extinct cycadeoid Nilssoniocladus , Ginkgo , araucariaceous, podocarpaceous, and cupressaceous conifers. This represents the mixed deciduous and evergreen broad-leaved forest as the Hell Creek landscape. The nature of these forests is uncertain because Johnson found that the majority of the angiosperm and conifer genera are now extinct. He also believes that, very roughly 80% of the terrestrial plant taxa died out in what is now Great Plains at the K-Pg boundary. On other hand, there is a great increase in the abundance of fossil fern spores in the two centimeters of rock that directly overlies the impact fallout layer (the famous K-Pg boundary layer). This increase in fern spore abundance is commonly referred as "the fern spike" (meaning that if the abundance of spores as a function of stratigraphic position were plotted out, the graph would show a spike just above the impact fallout layer).
Many of the modern plant affinities in the Hell Creek Formation (e.g., those with the prefix "aff." or with quotes around the genus name) may not in reality belong to these genera; instead they could be entirely different plants that resemble modern genera. Therefore, there is some question regarding whether the modern Ficus or Juglans , as two examples, actually lived in the Late Cretaceous.
Compared to the rich Hell Creek Formation fossil plant localities of the Dakotas, relatively few plant specimens have been collected from Montana. A few taxa were collected at Brownie Butte Montana by Shoemaker, but most plants were collected from North Dakota (Slope County) and from South Dakota. Among the localities, the Mud Buttes, located in Bowman County, North Dakota, is probably the richest megaflora assemblage known and the most diverse leaf quarry from the Hell Creek Formation. [126] "TYPE" after the binomial means that it is represented by a type specimen found in the Yale-Peabody Museum collections. "YPM" is the prefix for the Yale-Peabody Museum specimen number; "DMNH" is for the Denver Museum of Nature & Science; "USNM" is for Smithsonian National Museum of Natural History; and so on. The majority of Hell Creek megafloral specimens are collected at the Denver Museum of Nature & Science.
302 plant morphotypes based on leaf only, including:
Color key
| Notes Uncertain or tentative taxa are in small text; |
Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
---|---|---|---|---|---|---|
Only known liverwort in Hell Creek. | ||||||
Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
---|---|---|---|---|---|---|
E. sp | Rare in the Hell Creek Formation. | |||||
indeterminate | ||||||
S. sp | Floating aquatic plant. | |||||
Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
---|---|---|---|---|---|---|
Nilssoniocladus | N. comtula | Unlike N. yukonensis, its leaves are pinnatisect pinnules. Common. | ||||
N. yukonensis | The only Hell Creek Formation cycadophyte. A simple leaf. Common. | |||||
Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
---|---|---|---|---|---|---|
The only ginkgoalean in the Hell Creek Formation; uncommon | ||||||
Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
---|---|---|---|---|---|---|
indeterminate [126] | Casts of Monkey-puzzle leaves. | |||||
Casts of cupressaceae foliage. Uncommon | ||||||
D. sp | A conifer seed cone. It's likely to belong to Elatides longifolia. | |||||
A cupressaceous conifer closely related to Cupressinocladus . Common. | ||||||
Elatocladus sp, [126] | ||||||
Araucaria-like or Cunninghamia-like conifer. | ||||||
Glyptostrobus | Uncommon conifer. | |||||
M. occidentalis seed cones are known from the Hell Creek. | ||||||
Platyspiroxylon sp. [126] | A cupressaceaeous wood morphogenus | |||||
Podocarpoxylon sp. [126] | A possibly podocarpaceous wood morphogenus | |||||
Sequoiaxylon sp. [126] | A cupressaceaeous wood morphogenus | |||||
Taxodioxylon sp. [126] | A cupressaceaeous wood morphogenus | |||||
Related to today's bald cypress. | ||||||
Unidentified | Unidentified [126] | Unspecified cheirolepidiacous fossils [126] | ||||
Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
---|---|---|---|---|---|---|
"A." lessigiana | Abundant at Brownie Butte, Montana. | |||||
A?. robusta | Abundant at Brownie Butte, Montana. | |||||
Araliaephyllum | A. polevoi | A lobed leaf. Closely relating to Bisonia. Fairly common. | ||||
Averrhoites | cf. A. affinis | An uncommon taxon with compound leaves. | ||||
Bisonia | B. niemi | A broad leaf, probably in the Laurales. | ||||
Browniea | B. serrata | In the Nyssaceae, closely relating to extant Camptotheca. Less common. | ||||
Cannabaceae? | indeterminate | Incertae sedis. It's not likely in the Cannabaceae. [130] | ||||
Carpites | C. ulmiformis | Though this fossil fruit is abundant in the Early Paleocene, it's also found in Hell Creek. It may belong to Apiaceae. [131] | ||||
"C." taurenensis | Incertae sedis. It's common in the lowermost to the middle Hell Creek Formation, but less common in the upper 1/3 Hell Creek Formation. [126] | |||||
"C." lineafolia | Included in Ficus affinis by L. Hickey. | |||||
Cissites | cf. C. acerifolia | This morphotype was first described from the Cenomanian Dakota Group. [125] | ||||
C. insignis | This form represents of the group of Cenomanian leaves from Dakota Formation. [125] | |||||
C. lobata | A lobed leaf with half-naked basal lateral veins. Common in the upper 1/3 of the Hell Creek Formation. | |||||
C. puilasokensis | A palmately lobed leaf with 5 primary veins. Common in the upper 1/3 of the Hell Creek Formation. | |||||
C. corrugata | A prehistoric species of water lettuce, previously assigned to the genus Pistia . | |||||
C. hickeyi | Another Cobbania species from pond sediments known as "Licking Leaves." [132] | |||||
Cornophyllum | C. newberryi | The majority of leaves are entire-margined but some may develop a few teeth. [125] | ||||
"Cypercites" | "C." sp | A reed-type plant. | ||||
Dryophyllum | This taxon is extremely common in the Hell Creek Formation, but is rare in Paleocene sediments. | |||||
aff. "Dryophyllum" subfalcatum | see above. | |||||
"D." tenneseensis | This taxon is similar to D. subfalcatum]] but with extremely high L/W ratio and craspedodromous venation. [125] | |||||
Erlingdorfia | E. montana | Johnson, 1996. In the Platanaceae (related to today's Sycamore). A very common taxon. | ||||
" Ficus " | "F." planicostata | Despite the genus name, it's in Lauraceae. | ||||
G.saportana | Another generic Platanaceae. | |||||
H. hydrocotyloidea | Incertae sedis. May be related to lotus. An uncommon taxon. | |||||
aff. Humulus sp. | May be related to the extant genus Humulus . | |||||
H. pinnata | Floating aquatic fern | |||||
Limnobiophyllum | L. scutatum | Floating aquatic monocot, closely related to Pistia. | ||||
L. bradacii | Johnson, 1996. In the Magnoliidae: a common taxon. | |||||
"L." laramiense | Unlobed leaf. May be related to today's tulip tree (yellow poplar). An uncommon taxon. | |||||
L. sp | Four-lobed leaf. May be related to today's tulip tree (yellow poplar). An uncommon taxon. | |||||
L. preartocarpoides | Incertae sedis but possibly in Proteales. Johnson, 1996. | |||||
Laurophyllum | L. wardiana | Large leaves. Closely related to "Dryophyllum" subfalcatum. | ||||
"Magnolia" | M. pulchra | Occurs in southern the Wyoming flora, | ||||
Marmarthia | M. johnsonii | A new Marmarthia species described in Peppe et al. 2007. [134] | ||||
M. pearsonii | Johnson, 1996. In the Lauraceae: a very common taxon. | |||||
M. trivialis | Johnson, 1996. In the Lauraceae: a very common taxon. | |||||
" Myrica " | "Myrica" torreyi | Incertae sedis. Not actually a bayberry. | ||||
N. sp | One of the most common aquatic plants in Hell Creek. | |||||
Nelumbium | N. montanum | An aquatic angiosperm, closely related to lotus. Uncommon. | ||||
Nordenskioldia | N. borealis | A fossil fruit likely to belonging to Zizyphoides flabella. [135] | ||||
P. hastata | Despite the name, it's not related to extant genus Nymphaea. | |||||
Palaeoaster | P. porosia | A papaveraceous with fruits and seeds visually similar to Romneya though it's dubious.[ citation needed ] | ||||
P. cordatum | May be related to Sterculioideae. A common taxon. | |||||
P. marginata | Johnson, 1996. In the Platanaceae. A common taxon. | |||||
P. raynoldsii | An uncommon taxon. | |||||
P. verrucosa | A fossil fruit that may belong to Rutaceae. [136] | |||||
R. cleburnii | ||||||
S. sp | Coryphoid palm tree. Very common. | |||||
S. antiquus | A fruit seed that may belong to the palm family (Arecaceae), closely related to the genus Astrocaryum . [137] | |||||
T. angulata | A water caltrop look-alike. | |||||
T. arctica | A fossil fruit that may belong to Trochodendroides nebrascensis'. | |||||
T. ellipticum | A katsura look-alike. An uncommon taxon. | |||||
T. genetrix | A katsura look-alike. A common taxon. | |||||
T. nebrascensis | A very common taxon. | |||||
"Vitis" | "V." stantonii | Possibly a member of the Platanaceae rather than Vitaceae [126] [138] | ||||
"Ziziphus" | "Z." fibrillosus | A common taxon. | ||||
Z. attenuata | Related to today's ginger plant. Its closest living relative is the Asian genus Alpinia . | |||||
Z. magnifolia | Another Zinigberopsis species, previously assigned to Canna? magnifolia. | |||||
Z. flabella | An uncommon taxon. |
Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
---|---|---|---|---|---|---|
Abietineaepollenites | Montana | A conifer palynomorph | ||||
Montana | A conifer palynomorph | |||||
Montana | A conifer palynomorph | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Aquilapollenites | Aquilapollenites amplus [139] | Montana | ||||
Aquilapollenites attenuatus | ||||||
Aquilapollenites collaris | ||||||
Aquilapollenites conatus [139] | Montana | |||||
Aquilapollenites delicatus [139] | Montana | |||||
Aquilapollenites marmarthensis | ||||||
Aquilapollenites polaris [139] | Montana | |||||
Aquilapollenites pulvinus [139] | Montana | |||||
Aquilapollenites pyriformis [139] | Montana | |||||
Aquilapollenites quadricretaeus | ||||||
Aquilapollenites quadrilobus | ||||||
Aquilapollenites reductus [139] | Montana | |||||
Aquilapollenites reticulatus [139] | Montana | |||||
Aquilapollenites senonicus | ||||||
Aquilapollenites turbidus | ||||||
Aquilapollenites striatus | ||||||
Montana | A mosquito fern palynomorph | |||||
Balmeisporitessp. | ||||||
Montana | ||||||
Montana | ||||||
Cicatricosisporites | Montana | |||||
Montana | ||||||
Cingulatisporites | Montana | |||||
Montana | ||||||
Montana | ||||||
Concavisporites | Montana | |||||
Montana | ||||||
Converrucosisporites sp. [139] | Montana | |||||
Montana | A hazelnut palynomorph | |||||
Montana | ||||||
Cyathidites | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Ephedripites | Montana | |||||
Montana | ||||||
Montana | ||||||
Gleicheniidites | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Hymenophyllumsporites | Montana | A fern spore palynomorph | ||||
Montana | A fern spore palynomorph | |||||
Montana | ||||||
Interpollis cf. I. supplingensis | ||||||
Kurtzipites | Montana | |||||
Montana | ||||||
Laevigatosporites | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Liliacidites | Montana | |||||
Liliacidites sp. [139] | Montana | |||||
Montana | ||||||
Momipites | Montana | |||||
Montana | ||||||
Monosulcites | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Monosulcites sp. [139] | Montana | |||||
Myrtipites | Montana | |||||
Montana | ||||||
Nyssapollenites | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Phyllocladidites | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Proteacidites | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Schizosporis | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Stereisporites | Montana | |||||
Montana | ||||||
Montana | ||||||
Styx | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Tricolpites | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Tricolpopollenites | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Tricolpopollenites sp1, sp2 [139] | Montana | |||||
Tricolporopollenites | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Ulmipollenites | Montana | |||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Montana | ||||||
Tyrannosaurus is a genus of large theropod dinosaur. The type species Tyrannosaurus rex, often shortened to T. rex or colloquially T-Rex, is one of the best represented theropods. It lived throughout what is now western North America, on what was then an island continent known as Laramidia. Tyrannosaurus had a much wider range than other tyrannosaurids. Fossils are found in a variety of rock formations dating to the latest Campanian-Maastrichtian ages of the late Cretaceous period, 72.7 to 66 million years ago. It was the last known member of the tyrannosaurids and among the last non-avian dinosaurs to exist before the Cretaceous–Paleogene extinction event.
Triceratops is a genus of chasmosaurine ceratopsian dinosaur that lived during the late Maastrichtian age of the Late Cretaceous period, about 68 to 66 million years ago in what is now western North America. It was one of the last-known non-avian dinosaurs and lived until the Cretaceous–Paleogene extinction event 66 million years ago. The name Triceratops, which means 'three-horned face', is derived from the Greek words trí- meaning 'three', kéras meaning 'horn', and ṓps meaning 'face'.
Torosaurus is a genus of herbivorous chasmosaurine ceratopsian dinosaur that lived during the late Maastrichtian age of the Late Cretaceous period, between 68 and 66 million years ago, though it is possible that the species range might extend to as far back as 69 million years ago. Fossils have been discovered across the Western Interior of North America, from as far north as Saskatchewan to as far south as Texas.
Pachycephalosaurus is a genus of pachycephalosaurid ornithischian dinosaur. The type species, P. wyomingensis, is the only known species, but some researchers argue that Stygimoloch might be a second species, P. spinifer, or a juvenile specimen of P. wyomingensis. It lived during the Maastrichtian age of the Late Cretaceous period in what is now western North America. Remains have been excavated in Montana, South Dakota, Wyoming, and Alberta. The species is known mainly from a single skull, plus a few extremely thick skull roofs. More complete fossils would come to be found in the following years.
Thescelosaurus is an extinct genus of neornithischian dinosaur that lived during the Late Cretaceous period in North America. It was among the last of the non-avian dinosaurs to appear before the entire group went extinct during the Cretaceous–Paleogene extinction event around 66 million years ago. Adult Thescelosaurus would have measured roughly 3–4 metres (10–13 ft) long and probably weighed several hundred kilograms. The genus Thescelosaurus is the type genus and also the largest member of the eponymous Thescelosauridae, which includes similarly-sized bipedal herbivores from the Late Cretaceous of Asia and North America such as Orodromeus, Parksosaurus, and Haya.
Leptoceratops is a genus of ceratopsian dinosaur from the Late Cretaceous of North America. First found in Alberta in 1910, the type species Leptoceratops gracilis was named in 1914 by Barnum Brown for a partial skull and skeleton of two individuals found in the Scollard Formation of Alberta. Additional specimens found in the Scollard include one complete and two mostly complete skeletons together, uncovered in 1947 by Charles M. Sternberg. Specimens from Montana that were among the earliest referred to Leptoceratops have since been moved to their own genera Montanoceratops and Cerasinops, while new specimens of L. gracilis include bonebed remains from the Hell Creek Formation of Montana and a partial skeleton from the Lance Formation of Wyoming. Together with related taxa, Leptoceratops is the eponymous genus of the family Leptoceratopsidae. Leptoceratops is known from more than ten individuals, all from Maastrichtian deposits of Alberta, Montana and Wyoming, representing the entire skeleton.
The Hell Creek Formation is an intensively studied division of mostly Upper Cretaceous and some lower Paleocene rocks in North America, named for exposures studied along Hell Creek, near Jordan, Montana. The formation stretches over portions of Montana, North Dakota, South Dakota, and Wyoming. In Montana, the Hell Creek Formation overlies the Fox Hills Formation. The site of Pompeys Pillar National Monument is a small isolated section of the Hell Creek Formation. In 1966, the Hell Creek Fossil Area was designated as a National Natural Landmark by the National Park Service.
The Lance (Creek) Formation is a division of Late Cretaceous rocks in the western United States. Named after Lance Creek, Wyoming, the microvertebrate fossils and dinosaurs represent important components of the latest Mesozoic vertebrate faunas. The Lance Formation is Late Maastrichtian in age, and shares much fauna with the Hell Creek Formation of Montana and North Dakota, the Frenchman Formation of southwest Saskatchewan, and the lower part of the Scollard Formation of Alberta.
Centrosaurinae is a subfamily of ceratopsid, a group of large quadrupedal ornithischian dinosaur. Centrosaurine fossil remains are known primarily from the northern region of Laramidia but isolated taxa have been found in China and Utah as well.
Coriops is an extinct genus of freshwater osteoglossomorph fish, possibly a hiodontiform, with a single species known from the Late Cretaceous of western North America.
The North Horn Formation is a widespread non-marine sedimentary unit with extensive outcrops exposed in central and eastern Utah. The formation locally exceeds 3,600 feet (1,100 m) in thickness and is characterized by fluvial, lacustrine, and floodplain dominated systems, representing a terrestrial, high energy, depositional environment. The sediments date from Late Cretaceous (Maastrichtian) to early Paleocene in age and include the K-Pg extinction event boundary; however, this boundary is extremely difficult to locate and there is no strong stratigraphic evidence available that indicates a specific marker bed such as an iridium rich clay layer. Thus far, the only visible evidence is represented in the form of faunal turnover from dinosaur to mammal-dominated fossil assemblages. Taxa from the Cretaceous part of the formation include squamates, testudines, choristoderes, crocodyliforms, sharks, bony fishes, amphibians, mammals, dinosaurs, eggshell fragments, trace fossils, mollusks, plant macrofossils, such as wood fragments, and palynomorphs.
The McRae Group is a geological group exposed in southern New Mexico whose strata, including layers of the Hall Lake Formation and Jose Creek Formation, date to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from this unit.
The Javelina Formation is a geological formation in Texas. Dating has shown that the strata date to the Maastrichtian stage of the Late Cretaceous, approximately 70 to 66.5 million years old. The middle part of the formation has been dated to about 69 million years ago plus or minus 1 million years and the top situated near the Cretaceous–Paleogene boundary, dated to 66 Ma ago. Dinosaur remains are among the fossils that have been recovered from the formation.
Brachychampsa is an extinct genus of alligatorid, possibly a basal caiman. Specimens have been reported from New Mexico, Colorado, Wyoming, Montana, North and South Dakota, New Jersey, and Saskatchewan, though only those from Montana, Utah, and New Mexico are based on material sufficient to justify the referral. Some specimens have been reported from the Campanian-aged deposits of Central Asia, although the species status is indeterminate for these fossils. The genus first appeared during the late Campanian stage of the Late Cretaceous and became extinct during the late Maastrichtian stage of the Cretaceous. Brachychampsa is distinguished by an enlarged fifth maxillary tooth in the upper jaw.
Acheroraptor is an extinct genus of dromaeosaurid theropod dinosaur known from the latest Maastrichtian Hell Creek Formation of Montana, United States. It contains a single species, Acheroraptor temertyorum. A. temertyorum is one of the two geologically youngest known species of dromaeosaurids, the other being Dakotaraptor steini, which is also known from Hell Creek. A basal cousin of Velociraptor, Acheroraptor is known from upper and lower jaw material.
Leptorhynchos is an extinct genus of caenagnathid theropod from the Late Cretaceous of what is now the US state of Texas, although it has been suggested to also exist in Alberta and South Dakota. The type species is L. gaddisi, and it is currently the only widely accepted valid species. The generic name of Leptorhynchos comes from the Greek "leptos" meaning "small" and "rhynchos" meaning "beak". The specific epithet is in honor of the Gaddis family, who owned the land on which the holotype was discovered.
Trierarchuncus is a monotypic genus of alvarezsaurid theropod which includes a single species, Trierarchuncus prairiensis, which is known from fossils found in deposits of the Hell Creek Formation in Montana. It is the youngest known alvarezsaurid and one of the last non-avian dinosaurs, going extinct during the Cretaceous–Paleogene extinction event, which occurred approximately 66 million years ago.
Wakinyantanka is an ichnogenus of footprint produced by a large theropod dinosaur from the Late Cretaceous Hell Creek Formation of South Dakota. Wakinyantanka tracks are large with three long, slender toes with occasional impressions of a short hallux and narrow metatarsals. Wakinyantanka was the first dinosaur track to be discovered in the Hell Creek Formation, which remain rare in the preservational conditions of the rocks. The potential trackmakers may be a large oviraptorosaur or a small tyrannosaurid.