Hell Creek Formation (original) (raw)

Geological formation in the United States

Hell Creek Formation
Stratigraphic range: Late Cretaceous to Early Paleogene, Maastrichtian–Danian (Lancian)~68–66 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓
Exposure in the badlands near Fort Peck Reservoir
Type Geological formation
Unit of Montana Group
Sub-units Breien, Little Beaver Creek, Middle Sandstone & Pretty Butte Members
Underlies Fort Union Formation
Overlies Fox Hills Formation
Thickness 50–100 m (160–330 ft)
Lithology
Primary Claystone, mudstone
Other Sandstone, siltstone, conglomerate, amber
Location
Coordinates 46°54′N 101°30′W / 46.9°N 101.5°W / 46.9; -101.5
Approximate paleocoordinates 52°36′N 74°24′W / 52.6°N 74.4°W / 52.6; -74.4
Region Montana, North Dakota, South Dakota, Wyoming
Country United States
Extent Williston Basin
Type section
Named for Hell Creek, Jordan, Montana
Named by Barnum Brown
Year defined 1907
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Paleontological camp of Museum of the Rockies in eastern Montana – Hell Creek Formation (summer dig season 2009)

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.[1] 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.

It is a series of fresh and brackish-water clays, mudstones, and sandstones deposited during the Maastrichtian and Danian (respectively, the end of the Cretaceous period and the beginning of the Paleogene) by fluvial activity in fluctuating river channels and deltas and very occasional peaty swamp deposits along the low-lying eastern continental margin fronting the late Cretaceous Western Interior Seaway.[2] The climate was mild; the presence of crocodilians along with palm trees suggests a subtropical and temperate climate with no prolonged annual cold. The famous iridium-enriched Cretaceous–Paleogene boundary, which separates the Cretaceous from the Cenozoic, occurs as a discontinuous but distinct thin marker bedding above and occasionally within the formation, near its boundary with the overlying Fort Union Formation.

The world's largest collection of Hell Creek fossils is housed and exhibited at the Museum of the Rockies in Bozeman, Montana.[3] The specimens displayed are the result of the museum's Hell Creek Project, a joint effort between the museum; Montana State University; the University of Washington;[4] the University of California, Berkeley; the University of North Dakota; and the University of North Carolina which began in 1998.

The Hell Creek Formation is an intensively studied geological formation of mostly Upper Cretaceous and some Early 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.

Dinosaurs and pterosaurs of Hell Creek Formation

In 1966, the Hell Creek Fossil Area was designated as a National Natural Landmark by the National Park Service.[5]

Map of the Hell Creek and Lance Formations in western North America

The Hell Creek Formation in Montana overlies the Fox Hills Formation and underlies the Fort Union Formation, and the boundary with the latter occurs near the Cretaceous–Paleogene boundary (K–Pg), which defines the end of the Cretaceous period and has been dated to 66 ± 0.07 Ma old.[6] The 90-metre (300 ft) thickness of the formation is estimated to have been deposited in about 2 million years.[[[Wikipedia:Citing%5Fsources|page needed]]]-7" title="null">[7] Lancian fauna characteristic of Hell Creek are found as high as a few meters below the boundary.[8]

The K–Pg boundary is generally situated near the contact between the upper Hell Creek and the lower Ludlow member of the Fort Union Formation, though in some areas (e.g. in North Dakota) the boundary is well within the Ludlow member, 3 metres (9.8 ft) above the boundary with the Hell Creek.[8] On the other hand, in some small regions of Montana, the Hell Creek Formation contains the K–Pg boundary, and extends slightly into the Paleogene.[9]

The Tanis site in North Dakota contains possible evidence of the Chicxulub meteorite impact—such as the chaotic mixing of fossil carcasses and a layer of glass tektites with associated impact impressions—deposited minutes to hours after the impact.[10][11][12]

Hell Creek fauna

The remains of many animals including dinosaurs were found in the Hell Creek Formation. Its location at the changing conjunction of the eastern coast of Laramidia and the adjacent western shallows of the Western Interior Seaway led to the preservation of fossils of both marine and terrestrial creatures.[13] Vertebrates include dinosaurs, pterosaurs, crocodiles, champsosaurs, lizards, snakes, turtles, frogs and salamanders. Remains of fishes and mammals have also been found in the Hell Creek Formation. The formation has produced impressive assemblages of invertebrates (including ammonites), plants, mammals, fish, reptiles (including the lizard Obamadon), marine reptiles (including the marine reptiles like mosasaurs, plesiosaurs and sea turtles), and amphibians. Notable dinosaur finds include Tyrannosaurus and Triceratops, ornithomimids as well, caenagnathids like Anzu, a variety of small theropods, pachycephalosaurs, ankylosaurs, crocodylomorphs and squamates, including various animal fossils unearthed in the Hell Creek Formation. The most complete hadrosaurid dinosaur ever found, an Edmontosaurus, was retrieved in 2000 from the Hell Creek Formation and widely publicized in a National Geographic documentary aired in December 2007. A few bird, mammal, and pterosaur fossils have also been found. The teeth of sharks and rays are sometimes found in the riverine Hell Creek Formation, suggesting that some of these taxa were then, as now, tolerant of fresh water. The "Lancian" fauna is more similar overall phylogenetically to East Asian and Canadian/Alaskan faunas than most Campanian North American faunas. Fossil insects from inclusions found within amber are known.[14]

View of Hell Creek State Park, the "heart" of Hell Creek Formation

Depositional environment

[edit]

The dominant plants of the Hell Creek Formation are mainly flowering plants

It is a series of fresh and brackish-water clays, mudstones, and sandstones deposited during the Maastrichtian and Danian (respectively, the end of the Cretaceous period and the beginning of the Paleogene) by fluvial activity in fluctuating channels and deltas and very occasional peaty swamp deposits along the low-lying eastern continental margin fronting the late Cretaceous Western Interior Seaway. The Hell Creek Formation, as typified by exposures in the Fort Peck area of Montana, has been interpreted as a flat, forested floodplain with a relatively subtropical climate that supported a variety of plants ranging from angiosperm trees to gymnosperms such as the conifers, cycadeoids and ginkgos to ferns and moss. The Hell Creek Formation was laid down by streams, on a coastal plain along the edge of the Western Interior Seaway. The presence of crocodylians suggests climate was subtropical; there was no cold season and probably ample precipitation.

The Hell Creek Formation, Lance Formation and Scollard Formation represent different sections of the western shore of the shallow sea that divided western and eastern North America during the Cretaceous. Swampy lowlands were the habitat of various animals, including dinosaurs. A broad coastal plain extended westward from the seaway to the newly formed Rocky Mountains. These formations are composed largely of sandstone and mudstone which have been attributed to floodplain, fluvial, lacustrine, swamp, estuarine and coastal plain environments.[15][16][17] Hell Creek is the best studied of these ancient environments. At the time, this region had a subtropical, warm and moist climate. The climate was humid, with flowering plants, conifers, palm trees, and ferns in the swamps, and conifers, canopy, understory plants, high diversity of angiosperm trees and shrubs in the forests. In northwestern South Dakota, strips of black layers deposited in the wetland environment are rich in coal, and a bright band-like layer of sand and mud from the river floodplain accumulated. Many plant species were supported, primarily angiosperms, and less commonly conifers, ferns and cycadeoids. An abundance of fossil leaves are found at dozens of different sites indicating that the area was largely forested by small- to medium-sized trees.

Pie chart of the time averaged census for large-bodied dinosaurs from the entire Hell Creek Formation in the study area

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 Horner, Goodwin, and Myhrvold (2011)[18]

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 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, a possible Parasaurolophus walkeri, 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.[19] The largest Triceratops skull ever discovered, nicknamed 'Dragon King', was found in Glendive, Montana, which is in the Hell Creek Formation.[20][21]

Historically, numerous teeth have been attributed to various Dromaeosaurid and Troodontid taxa with known body fossils from only older formations, including 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.[22] Fossilized teeth of various troodontids and coelurosaurs are common throughout the Hell Creek Formation; the best known examples include Paronychodon, Pectinodon and Richardoestesia, respectively.

Detail of Hell Creek diorama at Milwaukee Public Museum is represented by angiosperm-dominated riparian forest.

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. A great 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,[23] 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.

Fossil fruits from the Hell Creek Formation of Spinifructus antiquus of the palm family (Arecaceae), closely related to the genus Astrocaryum.

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.[24] For example, the HCIa zone is dominated by ["Dryophyllum" subfalcatum](/w/index.php?title=%22Dryophyllum%22%5Fsubfalcatum&action=edit&redlink=1 ""Dryophyllum" subfalcatum (page does not exist)"), Leepierceia preartocarpoides, ["Vitis" stantonii](/w/index.php?title=%22Vitis%22%5Fstantonii&action=edit&redlink=1 ""Vitis" stantonii (page does not exist)"), and ["Celastrus" taurenensis](/w/index.php?title=%22Celastrus%22%5Ftaurenensis&action=edit&redlink=1 ""Celastrus" taurenensis (page does not exist)"), 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.[[[Wikipedia:Citing%5Fsources|page needed]]]-25" title="null">[25][26]

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](/w/index.php?title=%22Dryophyllum%22%5Ftennessensis&action=edit&redlink=1 ""Dryophyllum" tennessensis (page does not exist)"), Liriodendrites bradacii, and many members of the Laurales including Bisonia niemii, ["Ficus" planicostata](/w/index.php?title=%22Ficus%22%5Fplanicostata&action=edit&redlink=1 ""Ficus" planicostata (page does not exist)"), and Marmarthia trivialis, while ["Celastrus" taurenensis](/w/index.php?title=%22Celastrus%22%5Ftaurenensis&action=edit&redlink=1 ""Celastrus" taurenensis (page does not exist)"), 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.[[[Wikipedia:Citing%5Fsources|page needed]]]-25" title="null">[25][26][27][28]

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.[29] However, there was an extremely high angiosperm diversity—common plane trees, ["Dryophyllum" subfalcatum](/w/index.php?title=%22Dryophyllum%22%5Fsubfalcatum&action=edit&redlink=1 ""Dryophyllum" subfalcatum (page does not exist)"), 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 the 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. 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.[26] "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.

Overview (from Johnson, 2002): 302 plant morphotypes based on leaf only, including:

Plants of the Hell Creek Formation

Gymnosperms

Ginkgos

Angiosperms

  1. ^ White, Paul D.; Fastovsky, David E.; Sheehan, Peter M. (February 1998). "Taphonomy and Suggested Structure of the Dinosaurian Assemblage of the Hell Creek Formation (Maastrichtian), Eastern Montana and Western North Dakota". PALAIOS. 13 (1). SEPM Society for Sedimentary Geology: 41–51. Bibcode:1998Palai..13...41W. doi:10.2307/3515280. JSTOR 3515280. Retrieved 13 November 2020.
  2. ^ Fowler, Denver (5 November 2020). "The Hell Creek Formation, Montana: A Stratigraphic Review and Revision Based on a Sequence Stratigraphic Approach". Geosciences. 10 (11): 435. Bibcode:2020Geosc..10..435F. doi:10.3390/geosciences10110435. ISSN 2076-3263.
  3. ^ Boswell, Evelyn. "Paradise in Hell Creek". Montana State University. Retrieved 2 April 2007.
  4. ^ Wilson Lab
  5. ^ U.S. National Park Service, 1966
  6. ^ Husson et al. 2011.
  7. [[[Wikipedia:Citing%5Fsources|page needed]]]%5F7-0" title="null">^ LeCain 2010, p. [_page needed_].
  8. ^ a b Pearson et al. 2002.
  9. ^ Johnson et al., 2002
  10. ^ DePalma et al. 2019.
  11. ^ Broad, 2019
  12. ^ Preston, 2019
  13. ^ Richardson, T (2008). "Spatial arrangements of fossil species at the Hell Creek formation: Perspectives and conclusions". International Journal of Paleogeology. 12 (24).
  14. ^ DePalma 2010.
  15. ^ Lofgren, 1997
  16. ^ Breithaupt, 1997
  17. ^ Eberth, 1997
  18. ^ Horner, John R; Goodwin, Mark B; Myhrvold, Nathan (2011). "Dinosaur Census Reveals Abundant Tyrannosaurus and Rare Ontogenetic Stages in the Upper Cretaceous Hell Creek Formation (Maastrichtian), Montana, USA". PLOS ONE. 6 (2): e16574. Bibcode:2011PLoSO...616574H. doi:10.1371/journal.pone.0016574. PMC 3036655. PMID 21347420.
  19. ^ Manning, Ott & Falkingham 2008.
  20. ^ "How a $1.8 million dinosaur skull went from Montana to Hong Kong". 23 April 2015.
  21. ^ "Yours for US$1.8m or more: 'world's biggest dinosaur' skull on sale in Hong Kong". 25 April 2015.
  22. ^ Evans, 2013
  23. ^ Fastovsky, David E.; McSweeney, Kevin (1987). "Paleosols spanning the Cretaceous-Paleogene transition, eastern Montana and western North Dakota". Geological Society of America Bulletin. 99 (1): 66. Bibcode:1987GSAB...99...66F. doi:10.1130/0016-7606(1987)99<66:PSTCTE>2.0.CO;2.
  24. ^ Johnson, Kirk R.; Hickey, Leo J. (1990). "Megafloral change across the Cretaceous/Tertiary boundary in the northern Great Plains and Rocky Mountains, U.S.A.". Global Catastrophes in Earth History; an Interdisciplinary Conference on Impacts, Volcanism, and Mass Mortality. Geological Society of America Special Papers. Vol. 247. pp. 433–444. doi:10.1130/SPE247-p433. ISBN 0-8137-2247-0.
  25. ^ [[[Wikipedia:Citing%5Fsources|page needed]]]%5F25-0" title="null">a [[[Wikipedia:Citing%5Fsources|page needed]]]%5F25-1" title="null">b Johnson 1989, p. [_page needed_].
  26. ^ a b c Johnson, Kirk R. (2002). "Megaflora of the Hell Creek and lower Fort Union Formations in the western Dakotas: Vegetational response to climate change, the Cretaceous-Tertiary boundary event, and rapid marine transgression". The Hell Creek Formation and the Cretaceous-Tertiary boundary in the northern Great Plains: An Integrated continental record of the end of the Cretaceous. doi:10.1130/0-8137-2361-2.329. ISBN 978-0-8137-2361-7.
  27. ^ Johnson, Kirk R.; Nichols, Douglas J.; Attrep, Moses; Orth, Charles J. (August 1989). "High-resolution leaf-fossil record spanning the Cretaceous/Tertiary boundary". Nature. 340 (6236): 708–711. Bibcode:1989Natur.340..708J. doi:10.1038/340708a0. S2CID 4302433.
  28. ^ Barnet, James S.K.; Littler, Kate; Kroon, Dick; Leng, Melanie J.; Westerhold, Thomas; Röhl, Ursula; Zachos, James C. (February 2018). "A new high-resolution chronology for the late Maastrichtian warming event: Establishing robust temporal links with the onset of Deccan volcanism". Geology. 46 (2): 147–150. Bibcode:2018Geo....46..147B. doi:10.1130/G39771.1. hdl:10871/30937.
  29. ^ Retallack, Gregory J. (November 1994). "A pedotype approach to latest Cretaceous and earliest Tertiary paleosols in eastern Montana". Geological Society of America Bulletin. 106 (11): 1377–1397. Bibcode:1994GSAB..106.1377R. doi:10.1130/0016-7606(1994)106<1377:APATLC>2.3.CO;2.

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