Prince Creek Formation | |
---|---|
Stratigraphic range: Latest Campanian ~73 ma | |
![]() General location of the Prince Creek Formation, in red | |
Type | Geological formation |
Unit of | Colville Group |
Sub-units | Kikak-Tegoseak Quarry, Kogosukruk Tongue, Ocean Point, Coleville River Bluff |
Underlies | Sagavanirktok Formation |
Overlies | Schrader Bluff Formation |
Lithology | |
Primary | Sandstone, mudstone[1] |
Other | siltstone, carbonaceous shale, ash-fall[1] |
Location | |
Coordinates | 70°00′N 151°30′W / 70.0°N 151.5°W |
Approximate paleocoordinates | 80°N 115°W / 80°N 115°W |
Region | Alaska |
Country | United States |
The Prince Creek Formation is a geological formation in Alaska with strata dating to the Late Campanian stage of the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.[2]
Age
[edit]The PCF ranges from Late Cretaceous (Campanian) to Paleogene in age. Due to a slight structural dip, the unit becomes progressively younger downriver (northward). Biostratigraphic analyses from the upper, vertebrate-bearing portion of the unit near Ocean Point indicate a temporal range from as old as late Campanian to as young as late Maastrichtian. Although previous radiometric dating suggested an early Maastrichtian age, more recent work indicates the fossiliferous beds near Ocean Point to be late Campanian in age (Druckenmiller et al. 2023).[3]
Habitat
[edit]
During the time when the Prince Creek Formation was deposited, Earth was going through a global cooling phase.[4] The Prince Creek Formation depositional environment includes tidally influenced meandering rivers, anastomosed distributary channels, crevasse splays, levees, lakes, ponds, and mires.[5] Large amounts of plants material are represented by peridonoid dinocysts, algae, fungal hyphae, fern and moss spores, projectates, Wodehouseia edmontonicola, bisaccate pollen, taxodiaceous pollen, and pollen from trees, shrubs, and herbs. Preserved woody trunks show trees did not exceed 20cm in diameter and canopy heights were estimated to have been around 5-6 meters tall. Frequent false rings observed in the dendrochronology of the stumps were deduced to have been caused by sudden drops in temperature during the growing season to between 6–10 °C (43–50 °F) suggestive of more sub-arctic summer conditions. These trees were compared to the modern Picea mariana which is common throughout the modern North American Taiga. Another similarity to modern boreal forests is the presence of charcoal indicating frequent forest fires in the depositional environment.[6] Emerging methodologies using oxygen-18 isotope values from fossil vertebrate remains to estimate average meteoric water temperature have yielded highly accurate results. When applied to the Prince Creek Formation it estimated a mean annual temperature around 0 °C (32 °F).[7] Mean annual precipitation was around 1,300 millimetres (51 in).[8] The paleolatitude of the formation at the time of deposition was around 80°N, high in the Arctic Circle, and would have likely experienced 120 days of winter darkness.[9][10]
Vertebrate paleofauna
[edit]Dinosaurs
[edit]Theropods
[edit]Indeterminate tyrannosaurid remains are present, mostly in the form of teeth. The teeth are from the Kikak-Tegoseak Quarry, Liscomb Quarry, and Byers Bed, totaling 8 teeth.[11] Fossils of crown or near-crown birds as well as members of Hesperornithes and Ichthyornithes have been reported in 2025, providing the oldest evidence of birds nesting at polar latitudes reported to date.[12]
Color key
|
Notes Uncertain or tentative taxa are in small text; |
Theropods of the Prince Creek Formation | |||||
---|---|---|---|---|---|
Genus | Species | Location | Abundance | Notes | Images |
Liscomb Quarry[11] Kikak-Tegoseak Quarry[11] Byers Bed[11] |
Fossilized teeth[11] |
A dromaeosaur. | |||
Ornithomimosauria indet.[14] | Indeterminate[14] | Old Bone Beach | Distal metatarsal IV | Possibly an ornithomimid. | |
Saurornitholestinae indet.[15] |
Indeterminate |
Pediomys Point - Liscomb Quarry[15] |
Small dentary tip from a juvenile.[15] |
A new species of dromaeosaurid closely related to Saurornitholestes.[15] |
|
N. hoglundi[16] |
Kikak-Tegoseak Quarry[16] |
One partial skull including a bone near the front of the maxilla and the front of the lower jaw.[16] |
Nanuqsaurus is a tyrannosaurid closely related to Lythronax, Tyrannosaurus, and Tarbosaurus.[16] |
||
Old Bone Beach[11] |
Teeth[11] |
A dromaeosaur. | |||
Kikak-Tegoseak Quarry[16] Liscomb Quarry[11] Byers Bed[11] Magical Mystery Bar[17] |
Dental remains,[16] including teeth.[11] Braincases have also been found.[17] |
Remains of T. sp. are approximately 50% larger than specimens from Alberta and Montana.[16] Remains were previously assigned to T. formosus.[13] The most abundant theropod.[17] As of 2011, a dubious genus.[18] |
Ornithischians
[edit]Color key
|
Notes Uncertain or tentative taxa are in small text; |
Ornithischians of the Prince Creek Formation | |||||
---|---|---|---|---|---|
Genus | Species | Location | Abundance | Notes | Images |
A. gangloffi[19] |
Kogosukruk Tongue[20] |
A squamosal, and the back of the dome.[21] |
The first pachycephalosaurine from Alaska discovered.[21] |
||
Kikak-Tegoseak Quarry[22] |
An abundance of skeletal remains,[22] including an immature juvenile.[23] |
The youngest of the Pachyrhinosaurus species, found in one of the highest latitudes of centrosaurine discoveries.[22] A discovery in the Kikak-Tegoseak Quarry was identified in 2013 as a juvenile of Pachyrhinosaurus perotorum. This discovery shows that the crest started to develop in the front of the snout, then extending farther back until it reaches the eye.[23] |
|||
Thescelosaurinae indet.[24] |
Indeterminate |
Teeth[24] |
Remains previously attributed to Thescelosaurus.[24] |
||
Leptoceratopsidae[9] | Indeterminate | Remains of adult and juvenile individuals[9] | |||
E. cf. regalis[26] |
Disassociated parts from multiple juveniles |
Originally identified as a distinct genus (Ugrunaaluk), recent studies have found it ontogenetically indistinguishable from Edmontosaurus.[25][26] |
|||
Lambeosaurinae indet.[27] | Indeterminate | Liscomb Bonebed | A supraoccipital | The first confirmed lambeosaurine in the Prince Creek Formation. | |
Ornithopoda indet.[24] |
Indeterminate[24] |
One tooth[24] |
A single "hypsilophodontid" cheek tooth not attributable to Parksosaurus or Thescelosaurus.[24] |
Mammals
[edit]Mammals of the Prince Creek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
Cimolodon[28] | C. cf. nitidus | Lower Maastrichtian | Isolated teeth | A small multituberculate. | ||
Gypsonictops[28] | G. sp. | Lower Maastrichtian | Isolated teeth | A small eutherian. | ||
Multituberculata indet.[28] | Indeterminate | Lower Maastrichtian | Isolated teeth | |||
Marsupialia indet.[28] | Indeterminate | Lower Maastrichtian | Most common in the Prince Creek Formation | |||
Sikuomys[29] | S. mikros | Lower Colville River. | Upper Campanian | A tiny eutherian. | ||
Unnuakomys[30] | U. hutchisoni | Pediomys Point | Lower Maastrichtian | Over 60 specimens | A small metatherian. |
Cartilaginous fish
[edit]Cartilaginous fishes of the Prince Creek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
Squatina | S. sp. | An angelshark.[31] | ![]() |
Ray-finned fish
[edit]Ray-finned fishes of the Prince Creek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
Acipenseridae indet. | A sturgeon.[31] | |||||
Archaeosiilik[31] | A. gilmulli | A esocid salmoniform | ||||
?Beryciformes indet. | Acanthomorph remains reminiscent of beryciforms.[31] | |||||
Cypriniformes indet.[31] | A cypriniform, the oldest record of this order.[31] | |||||
Horseshoeichthys | H. armaserratus | An armigatid ellimmichthyiform.[31] | ||||
Neopterygii indet. | A potential basal neopterygian, known from a scale similar to Belonostomus.[31] | |||||
Nunikuluk[31] | N. gracilis | A esocid salmoniform | ||||
Oldmanesox | O. canadensis | An esocid salmoniform.[31] | ||||
Polyodontidae indet. | A paddlefish, potentially represented by two distinct forms.[31] | |||||
Sivulliusalmo[31] | S. alaskensis | A salmonid salmoniform, the oldest record of this family. |
Plants
[edit]A Reinvestigation of the Parataxodium-type flora has revealed the assemblage was far more diverse than previously thought. However, this sedimentary block’s stratigraphic origins are uncertain. No other in situ limestone blocks comparable to the Parataxodium-type flora have been located along the Colville River. Rivers upstream from the point of discovery cut through Upper Cretaceous deposits that range in age from Late Albian to Cenomanian. The diversity of flora present is more consistent with the Tuluvak Formation, which is dated to the Turonian-Coniacian.[32]
Color key
|
Notes Uncertain or tentative taxa are in small text; |
Plants of the Prince Creek Formation[33] | |||||
---|---|---|---|---|---|
Genus | Species | Location | Abundance | Notes | Images |
P. wigginsii[20] |
Kogosukruk Tongue?[20] |
Previously thought to represent a single taxon, now shown to have included many distinct conifer morphotypes.[20][32] |
|||
Oncophoraceae indet. | Kogosukruk Tongue?[32] | A Dicranalean moss.[32] | |||
Osmundastrum[32] | O. cinnamomeum[32] | Kogosukruk Tongue?[32] | |||
Ginkgo[32] | G. adiantoides[32] | Kogosukruk Tongue?[32] | |||
Pityophyllum[32] | P. nordenskioldii[32] | Kogosukruk Tongue?[32] | Pinaceous needles.[32] | ||
Sequioideae indet. | Kogosukruk Tongue?[32] | Previously included in Parataxodium.[32] | |||
Taiwanioideae indet. | Kogosukruk Tongue?[32] | Previously included in Parataxodium.[32] | |||
Cryptomerioideae indet. | Kogosukruk Tongue?[32] | Previously included in Parataxodium.[32] | |||
Athrotaxoideae indet. | Kogosukruk Tongue?[32] | Previously included in Parataxodium.[32] | |||
Archeampelos[32] | A. sp. | Kogosukruk Tongue?[32] | |||
Cf. Cercidiphyllum | cf. C. sp. | Kogosukruk Tongue?[32] | |||
Dicotyledon indet. | Morphotype 2 | Kogosukruk Tongue?[32] | |||
Morphotype 3 | Kogosukruk Tongue?[32] | ||||
Morphotype 4 | Kogosukruk Tongue?[32] | ||||
Monocotyledon indet. | Kogosukruk Tongue?[32] | ||||
H. quercifolia[20] |
Kogosukruk Tongue?[20] |
Leaves[20] |
An angiosperm, known from leaves.[20] |
||
Q. angulata[20] |
Kogosukruk Tongue?[20] |
An aquatic angiosperm.[20] |
|||
E. sp.[20] |
Kogosukruk Tongue?[20] |
||||
P. krempii |
Coleville River Bluff |
Pollen spores |
Also found in the Schrader Bluff Formation. |
||
cf. Proteacidites |
cf. P. sp. |
Coleville River Bluff |
Pollen spores |
Also found in the Schrader Bluff Formation. |
|
cf. P. reduncus |
Coleville River Bluff |
Pollen spores |
Also found in the Schrader Bluff Formation. |
||
P. sp. |
Coleville River Bluff |
Pollen spores |
Also found in the Schrader Bluff Formation. |
||
O.? sp. |
Coleville River Bluff |
Pollen spores |
Also found in the Schrader Bluff Formation. |
||
O. sp. |
Coleville River Bluff |
Pollen spores |
Also found in the Schrader Bluff Formation. |
||
O. parvus |
Coleville River Bluff |
Pollen spores |
Also found in the Schrader Bluff Formation. |
||
O. arcticus |
Coleville River Bluff |
Pollen spores |
Also found in the Schrader Bluff Formation. |
||
O. wellmanii |
Coleville River Bluff |
Pollen remains |
Common in the Early Maastrichtian. Also found in the Schrader Bluff Formation. |
||
M. sp. indet. |
Coleville River Bluff |
Pollen remains |
Also found in the Schrader Bluff Formation. |
||
M. pseudosenonicus |
Coleville River Bluff |
Pollen remains |
Also found in the Schrader Bluff Formation. |
||
L. sp. |
Coleville River Bluff |
Pollen remains |
Also found in the Schrader Bluff Formation. |
||
L. dissolutum |
Coleville River Bluff |
Pollen remains |
Also found in the Schrader Bluff Formation. |
||
Indeterminate |
Coleville River Bluff |
Septate fungal hypha. |
Also found in the Schrader Bluff Formation. |
||
L."stellata" |
Coleville River Bluff |
Pollen remains |
Common in the Early Maastrichtian. Also found in the Schrader Bluff Formation. |
||
L. magnus |
Coleville River Bluff |
Pollen remains |
Also found in the Schrader Bluff Formation. |
||
L. sp. |
Coleville River Bluff |
Pollen remains |
Indeterminate remains are abundant in the Early Maastrichtian and still numerous in the Late Maastrichtian. Also found in the Schrader Bluff Formation. |
||
L. sp. |
Coleville River Bluff |
Pollen remains |
Also found in the Schrader Bluff Formation. |
||
K. trispissatus |
Coleville River Bluff |
Pollen remains |
Also found in the Schrader Bluff Formation. |
||
I. sp. |
Coleville River Bluff |
Pollen remains |
Also found in the Schrader Bluff Formation. |
||
I. sp. |
Coleville River Bluff |
Pollen remains |
Also found in the Schrader Bluff Formation. |
||
I. tappaniae |
Coleville River Bluff |
Samples of distinct pollen |
Also found in the Schrader Bluff Formation. |
||
I. marylandensis |
Coleville River Bluff |
Samples of distinct pollen |
Also found in the Schrader Bluff Formation. |
||
H. scollardensis |
Coleville River Bluff |
Samples of distinct pollen |
Also found in the Schrader Bluff Formation. |
||
H. amplus |
Coleville River Bluff |
Samples of distinct pollen |
Also found in the Schrader Bluff Formation. |
||
G. senonicus |
Coleville River Bluff |
Samples of distinct pollen |
Also found in the Schrader Bluff Formation. |
||
F sp. |
Coleville River Bluff |
Samples of distinct pollen |
Also found in the Schrader Bluff Formation. |
||
F. undulosus |
Coleville River Bluff |
Samples of distinct pollen |
Also found in the Schrader Bluff Formation. |
||
F. scabratus |
Coleville River Bluff |
Samples of distinct pollen |
Also found in the Schrader Bluff Formation. |
||
cf. E. accuratus |
Coleville River Bluff |
Samples of distinct pollen |
Also found in the Schrader Bluff Formation. |
||
E. procumbentformis |
Coleville River Bluff |
Pollen spores |
Also found in the Schrader Bluff Formation. |
||
D. sp. |
Coleville River Bluff |
Pollen remains |
Also found in the Schrader Bluff Formation. |
||
D. sp. |
Coleville River Bluff |
Preserved pollen samples |
Very abundant in the early Maastrichtian and Indeterminate level of the formation, becoming rarer until the Middle/Late Maastrichtian. Also found in the Schrader Bluff Formation. |
||
C. fragilis |
Coleville River Bluff |
Samples of distinct pollen |
Also found in the Schrader Bluff Formation. |
||
cf. C. apisulacea |
Coleville River Bluff |
Pollen samples |
Also found in the Schrader Bluff Formation. |
||
cf. C. sp. |
Coleville River Bluff |
Specimens of preserved pollen spores |
Also found in the Schrader Bluff Formation. |
||
C. sp. |
Coleville River Bluff |
Preserved pollen samples |
Also found in the Schrader Bluff Formation. |
||
C. sp. |
Coleville River Bluff |
Pollen samples |
Also found in the Schrader Bluff Formation. |
||
cf. C. congruens |
Coleville River Bluff |
Pollen remains |
Also found in the Schrader Bluff Formation. |
||
C. bialatus |
Coleville River Bluff |
Pollen samples |
Also found in the Schrader Bluff Formation. |
||
C. sp. 1 |
Coleville River Bluff |
Distinct pollen remains |
Also found in the Schrader Bluff Formation. |
||
C. sp. 2 |
Coleville River Bluff |
Preserved pollen |
Also found in the Schrader Bluff Formation. |
||
cf. C. dorogensis |
Coleville River Bluff |
Fossilized pollen spores |
Also found in the Schrader Bluff Formation. |
||
C. sp. |
Coleville Bluff Formation |
Pollen spores |
Also found in the Schrader Bluff Formation. |
||
C. ambigens |
Coleville River Bluff |
Pollen specimens |
Also found in the Schrader Bluff Formation. |
||
Coleville River Bluff |
Pollen |
Also found in the Schrader Bluff Formation. |
|||
Indeterminate |
Coleville River Bluff |
Bissacate gymnosperm pollen |
Also found in the Schrader Bluff Formation. |
||
B. sp. |
Coleville River Bluff |
Pollen spore remains |
Also found in the Schrader Bluff Formation. |
||
cf. A. cribrata |
Coleville River Bluff |
Carbonized pollen |
Also found in the Schrader Bluff Formation. |
||
A. trialatus |
Coleville River Bluff |
Pollen |
Also found in the Schrader Bluff Formation. |
||
A. sp. 2 |
Coleville River Bluff |
Pollen |
Also found in the Schrader Bluff Formation. |
||
A. sp. 3 |
Coleville River Bluff |
Pollen |
Also found in the Schrader Bluff Formation. |
||
cf. A. dentatus |
Coleville River Bluff |
Pollen |
Also found in the Schrader Bluff Formation. |
||
A. amygdaloides |
Coleville River Bluff |
Pollen |
Numerous in the Late Campanian, becoming abundant in the Maastrichtian. Also found in the Schrader Bluff Formation. |
||
A. sp. |
Coleville River Bluff |
Pollen |
Also found in the Schrader Bluff Formation. |
||
A. sp. 1 |
Coleville River Bluff |
Pollen |
Also found in the Schrader Bluff Formation. |
||
A. sp. 2 |
Coleville River Bluff |
Pollen |
Also found in the Schrader Bluff Formation. |
||
A. clavate |
Coleville River Formation |
Pollen |
Also found in the Schrader Bluff Formation. |
||
cf. A. spinulosus |
Coleville River Bluff |
Pollen |
Also found in the Schrader Bluff Formation. |
||
A. sp. |
Coleville River Bluff |
Pollen |
Also found in the Schrader Bluff Formation. |
See also
[edit]References
[edit]- ^ a b Flaig, P.P.; McCarthy, P.J.; Fiorillo, A.R. (2013). "Anatomy, Evolution, and Paleoenvironmental Interpretation of an Ancient Arctic Coastal Plain: Integrated Paleopedology and Palynology from the Upper Cretaceous (Maastrichtian) Prince Creek Formation, North Slope, Alaska, USA". In Driese, S.G.; Nordt, L.C. (eds.). New Frontiers in Paleopedology and Terrestrial Paleoclimatology: Paleosols and Soil Surface Analog Systems. Vol. 104. pp. 179–230. doi:10.2110/sepmsp.104.14. ISBN 9781565763227.
{{cite book}}
:|journal=
ignored (help) - ^ Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, North America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 574-588. ISBN 0-520-24209-2.
- ^ Brinkman, D. B.; López, J. A.; Erickson, G. M.; Eberle, J. J.; Muñoz, X.; Wilson, L. N.; Perry, Z. R.; Murray, A. M.; Van Loon, L.; Banerjee, N. R.; Druckenmiller, P. S. (2025). "Fishes from the Upper Cretaceous Prince Creek Formation, North Slope of Alaska, and their palaeobiogeographical significance". Papers in Palaeontology. 11 (3). e70014. doi:10.1002/spp2.70014.
- ^ Linnert, C.; A. Robinson, S.; A. Lees, J.; Pérez-Rodríguez, I.; C. Jenkyns, H.; Rose Petrizzo, M.; A. Arz, J.; R. Bown, P.; Falzoni, F. (2017-06-07). "Did Late Cretaceous cooling trigger the Campanian–Maastrichtian Boundary Event?". Newsletters on Stratigraphy. ISSN 0078-0421.
- ^ "Depositional environments of the Late Cretaceous (Maastrichtian) dinosaur-bearing Prince Creek Formation: Colville River region, North Slope, Alaska - ProQuest". www.proquest.com. Retrieved 2025-06-11.
- ^ Spicer, Robert I.; Herman, Alexei B.; Amiot, Romain; Spicer, Teresa E. V. (2016). "Environmental adaptations and constraints on latest Cretaceous Arctic dinosaurs". Global Geology. 19 (4): 241–254. doi:10.3969/j.issn.1673-9736.2016.04.05.
- ^ Amiot, Romain; Lécuyer, Christophe; Buffetaut, Eric; Fluteau, Frédéric; Legendre, Serge; Martineau, François (2004-09-30). "Latitudinal temperature gradient during the Cretaceous Upper Campanian–Middle Maastrichtian: δ18O record of continental vertebrates". Earth and Planetary Science Letters. 226 (1): 255–272. doi:10.1016/j.epsl.2004.07.015. ISSN 0012-821X.
- ^ Salazar-Jaramillo, Susana; McCarthy, Paul J.; Ochoa, Andrés; Fowell, Sarah J.; Longstaffe, Fred J. (2019-10-15). "Paleoclimate reconstruction of the Prince Creek Formation, Arctic Alaska, during Maastrichtian global warming". Palaeogeography, Palaeoclimatology, Palaeoecology. 532: 109265. doi:10.1016/j.palaeo.2019.109265. ISSN 0031-0182.
- ^ a b c Druckenmiller, Patrick S.; Erickson, Gregory M.; Brinkman, Donald; Brown, Caleb M.; Eberle, Jaelyn J. (June 2021). "Nesting at extreme polar latitudes by non-avian dinosaurs". Current Biology. 31 (16): 3469–3478.e5. Bibcode:2021CBio...31E3469D. doi:10.1016/j.cub.2021.05.041. ISSN 0960-9822. PMID 34171301.
- ^ Clennett, Edward J.; Sigloch, Karin; Mihalynuk, Mitchell G.; Seton, Maria; Henderson, Martha A.; Hosseini, Kasra; Mohammadzaheri, Afsaneh; Johnston, Stephen T.; Müller, R. Dietmar (2020). "A Quantitative Tomotectonic Plate Reconstruction of Western North America and the Eastern Pacific Basin". Geochemistry, Geophysics, Geosystems. 21 (8): e2020GC009117. doi:10.1029/2020GC009117. ISSN 1525-2027.
- ^ a b c d e f g h i j k l m n Fiorillo, A.R.; Gangloff, R.A. (2000). "Theropod Teeth from the Prince Creek Formation (Cretaceous) of Northern Alaska, with Speculations on Arctic Dinosaur Paleoecology". Journal of Vertebrate Paleontology. 20 (4): 675–682. doi:10.1671/0272-4634(2000)020[0675:ttftpc]2.0.co;2. S2CID 130766946.
- ^ Wilson, L. N.; Ksepka, D. T.; Wilson, J. P.; Gardner, J. D.; Erickson, G. M.; Brinkman, D.; Brown, C. M.; Eberle, J. J.; Organ, C. L.; Druckenmiller, P. S. (2025). "Arctic bird nesting traces back to the Cretaceous". Science. 388 (6750): 974–978. doi:10.1126/science.adt5189. PMID 40440391.
- ^ a b c d e "3.33 Alaska, United States; 3. Prince Creek Formation," in Weishampel, et al. (2004). Page 587.
- ^ a b Watanabe, Akinobu; Erickson, Gregory M.; Druckenmiller, Patrick S. (2013-09-01). "An ornithomimosaurian from the Upper Cretaceous Prince Creek Formation of Alaska". Journal of Vertebrate Paleontology. 33 (5): 1169–1175. Bibcode:2013JVPal..33.1169W. doi:10.1080/02724634.2013.770750. ISSN 0272-4634. S2CID 130049294.
- ^ a b c d Chiarenza, A. A.; Fiorillo, A. R.; Tykoski, R. S.; McCarthy, P. J.; Flaig, P. P.; Contreras, D. L. (2020). "The first juvenile dromaeosaurid (Dinosauria: Theropoda) from Arctic Alaska". PLOS ONE. 15 (7): e0235078. Bibcode:2020PLoSO..1535078C. doi:10.1371/journal.pone.0235078. PMC 7343144. PMID 32639990.
- ^ a b c d e f g h i j Fiorillo, A. R.; Tykoski, R. S. (2014). Dodson, Peter (ed.). "A Diminutive New Tyrannosaur from the Top of the World". PLoS ONE. 9 (3): e91287. Bibcode:2014PLoSO...991287F. doi:10.1371/journal.pone.0091287. PMC 3951350. PMID 24621577.
- ^ a b c Fiorillo, A.R.; Tykoski, R.S.; Currie, P.J.; Mccarthy, P.J.; Flaig, P. (2009). "Description of two partial Troodon braincases from the Prince Creek Formation (Upper Cretaceous), North Slope Alaska". Journal of Vertebrate Paleontology. 29 (1): 178–187. Bibcode:2009JVPal..29..178F. doi:10.1080/02724634.2009.10010370. S2CID 197535475.
- ^ Zanno, Lindsay E.; Varricchio, David J.; O'Connor, Patrick M.; Titus, Alan L.; Knell, Michael J. (2011-09-19). "A New Troodontid Theropod, Talos sampsoni gen. et sp. nov., from the Upper Cretaceous Western Interior Basin of North America". PLOS ONE. 6 (9): e24487. Bibcode:2011PLoSO...624487Z. doi:10.1371/journal.pone.0024487. ISSN 1932-6203. PMC 3176273. PMID 21949721.
- ^ a b Sullivan, R.M. (2006). "A taxonomic review of the Pachycephalosauridae (Dinosauria: Ornithischia)". New Mexico Museum of Natural History and Science Bulletin. 35: 347–365.
- ^ a b c d e f g h i j k l m n o p q r Spicer, R.A.; Parrish, J.T. (1987). "Plant Megafossils, Vertebrate Remains, and Paleoclimate of the Kogosukruk Tongue (Late Cretaceous), North Slope, Alaska". In Hamilton, Thomas D.; Galloway, John P. (eds.). Geologic Studies in Alaska. pp. 47–48.
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ignored (help) - ^ a b Gangloff, R.A.; Fiorillo, A.R.; Norton, D.W. (2005). "The First Pachycephalosaurine (Dinosauria) from the Paleo-Arctic of Alaska and its Paleogeographic Implications". Journal of Paleontology. 79 (5): 997–1001. doi:10.1666/0022-3360(2005)079[0997:tfpdft]2.0.co;2. S2CID 130669713.
- ^ a b c d e f Fiorillo, A.R.; Tykoski, R.S.T. (2012). "A new species of the centrosaurine ceratopsid Pachyrhinosaurus from the North Slope (Prince Creek Formation: Maastrichtian) of Alaska". Acta Palaeontologica Polonica. 57 (3): 561–573. doi:10.4202/app.2011.0033.
- ^ a b c d Fiorillo, A.R.; Tykoski, R.S. (2013). Farke, Andrew A. (ed.). "An Immature Pachyrhinosaurus perotorum (Dinosauria: Ceratopsidae) Nasal Reveals Unexpected Complexity of Craniofacial Ontogeny and Integument in Pachyrhinosaurus". PLoS ONE. 8 (6): e65802. Bibcode:2013PLoSO...865802F. doi:10.1371/journal.pone.0065802. PMC 3686821. PMID 23840371.
- ^ a b c d e f g Brown, C.M.; Druckenmiller, P. (2011). "Basal ornithopod (Dinosauria: Ornithischia) teeth from the Prince Creek Formation (early Maastrichtian) of Alaska". Canadian Journal of Earth Sciences. 48 (9): 1342–1354. Bibcode:2011CaJES..48.1342B. doi:10.1139/e11-017.
- ^ a b c Re-examination of the cranial osteology of the Arctic Alaskan hadrosaurine with implications for its taxonomic status Ryuji Takasaki, Anthony R. Fiorillo, Ronald S. Tykoski, Yoshitsugu Kobayashi.
- ^ a b Sharpe, Henry S.; Powers, Mark J.; Dyer, Aaron D.; Rhodes, Matthew M.; McIntosh, Annie P.; Garros, Christiana W.; Currie, Philip J.; Funston, Gregory F. (2024-04-16). "Craniomandibular anatomy of a juvenile specimen of Edmontosaurus regalis Lambe, 1917 clarifies issues in ontogeny and biogeography". Journal of Vertebrate Paleontology. 43 (5). doi:10.1080/02724634.2024.2326644. ISSN 0272-4634.
- ^ McCarthy, Paul J.; Tykoski, Ronald S.; Kobayashi, Yoshitsugu; Fiorillo, Anthony R.; Takasaki, Ryuji (2019-03-29). "The First Definite Lambeosaurine Bone From the Liscomb Bonebed of the Upper Cretaceous Prince Creek Formation, Alaska, United States". Scientific Reports. 9 (1): 5384. Bibcode:2019NatSR...9.5384T. doi:10.1038/s41598-019-41325-8. ISSN 2045-2322. PMC 6440964. PMID 30926823.
- ^ a b c d Thurston, D.K.; Fujita, K. (1994). 1992 Proceedings, International Conference on Arctic Margins. Anchorage, Alaska: U.S. Dept. of the Interior, Minerals Management Service, Alaska Outer Continental Shelf Region. ISBN 978-1125448038.
- ^ Eberle, Jaelyn J.; Clemens, William A.; Erickson, Gregory M.; Druckenmiller, Patrick S. (2023-01-01). "A new tiny eutherian from the Late Cretaceous of Alaska". Journal of Systematic Palaeontology. 21 (1). Bibcode:2023JSPal..2132359E. doi:10.1080/14772019.2023.2232359. ISSN 1477-2019. S2CID 260668330.
- ^ Eberle, Jaelyn J.; Clemens, William A.; McCarthy, Paul J.; Fiorillo, Anthony R.; Erickson, Gregory M.; Druckenmiller, Patrick S. (2019-02-14). "Northernmost record of the Metatheria: a new Late Cretaceous pediomyid from the North Slope of Alaska". Journal of Systematic Palaeontology. 17 (21): 1805–1824. Bibcode:2019JSPal..17.1805E. doi:10.1080/14772019.2018.1560369. ISSN 1477-2019. S2CID 92613824.
- ^ a b c d e f g h i j k l Brinkman, D. B.; López, J. A.; Erickson, G. M.; Eberle, J. J.; Muñoz, X.; Wilson, L. N.; Perry, Z. R.; Murray, A. M.; Van Loon, L.; Banerjee, N. R.; Druckenmiller, P. S. (2025). "Fishes from the Upper Cretaceous Prince Creek Formation, North Slope of Alaska, and their palaeobiogeographical significance". Papers in Palaeontology. 11 (3). e70014. doi:10.1002/spp2.70014.
- ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac Rothwell, Gar W.; Stockey, Ruth A.; Smith, Selena Y. (2020-12-01). "Revisiting the Late Cretaceous Parataxodium wigginsii flora from the North Slope of Alaska, a high-latitude temperate forest". Cretaceous Research. 116: 104592. Bibcode:2020CrRes.11604592R. doi:10.1016/j.cretres.2020.104592. ISSN 0195-6671.
- ^ Flores, R.M.; Myers, M.D.; Houseknecht, D.W.; Stricker, G.D.; Brizzolara, D.W.; Ryherd, T.J.; Takahashi, K.I. (2007). "Stratigraphy and Facies of Cretaceous Schrader Bluff and Prince Creek Formations in Colville River Bluffs, North Slope, Alaska" (PDF). U.S. Geological Survey Professional Paper. 1748: 52.
Bibliography
[edit]- Flaig, P.P. (2010). "Depositional Environments of the Late Cretaceous (Maaastrichtian) Dinosaur-Bearing Prince Creek Formation: Colville River Region, North Slope, Alaska". Unpublished Ph.D. Dissertations, the University of Alaska-Fairbanks: 311.
- Flaig, P.P.; McCarthy, P.J.; Fiorillo, A.R. (2011). "A Tidally-Influenced, High-Latitude Coastal-Plain: the Upper Cretaceous (Maastrichtian) Prince Creek Formation, North Slope, Alaska". In Stephanie K. Davidson; Sophie Leleu; Colin P. North (eds.). From River to Rock Record: The Preservation of Fluvial Sediments and their Subsequent Interpretation. Vol. 97. Society for Sedimentary Geology. pp. 233–264. doi:10.2110/sepmsp.097.233. ISBN 9781565763074.
- Flaig, P.P.; Fiorillo, A.R.; McCarthy, P.J. (2014). "Dinosaur-bearing hyperconcentrated flows of Cretaceous Arctic Alaska—Recurring catastrophic event beds on a distal paleopolar coastal plain". PALAIOS. 29 (11): 594–611. Bibcode:2014Palai..29..594F. doi:10.2110/palo.2013.133. S2CID 128713816.
- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.