Nanuqsaurus
Nanuqsaurus (meaning "polar bear lizard") is a genus of tyrannosaurine theropod dinosaur known from the mid Maastrichtian age of the Late Cretaceous Prince Creek Formation in the North Slope of Alaska, having lived roughly 70-68 million years ago. It contains a single species, Nanuqsaurus hoglundi, which known only from a partial skull and multiple undescribed postcranial and teeth elements.
Nanuqsaurus Temporal range: Late Cretaceous, | |
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A reconstructed skull with a cast of the holotype in place at the Perot Museum | |
Scientific classification ![]() | |
Kingdom: | Animalia |
Phylum: | Chordata |
Clade: | Dinosauria |
Clade: | Saurischia |
Clade: | Theropoda |
Family: | †Tyrannosauridae |
Subfamily: | †Tyrannosaurinae |
Genus: | †Nanuqsaurus Fiorillo & Tykoski, 2014 |
Type species | |
†Nanuqsaurus hoglundi Fiorillo & Tykoski, 2014 |
Discovery and Naming
Initial Material
Before the formal description of Nanuqsaurus, numerous tyrannosaurid teeth were known from the Kogosukruk Tongue of the Prince Creek Formation and were first referred to Gorgosaurus.[1] After the locale was later understood to be younger than previously thought, the consensus switched to referring to the teeth to Albertosaurus.[2][3]
Holotype Specimen
In 2006, within the North Slope Borough of Alaska, the fossilized remains of what appeared to be a medium sized theropod were located at the Kikak-Tegoseak Quarry of the Prince Creek Formation. The material was found to contain multiple fragments of the animal's skull, all of which were collected from the same area and thus were found to most likely belong to a single individual. Of the disarticulated fragments preserved were the nasal branch of the right maxilla, fragmentary skull roof including pieces of both frontals, parietals as well as a piece of the right laterosphenoid, and a fragment of the left dentary. These anatomical features were later used to determine the probable skull length of the animal, with estimates giving it a length of 24-28 inches.[3] Radiometric dating of nearby rock suggests that the fossils were deposited roughly 68 to 70 million years ago.[2][4]

It wasn't until after preparation and analysis at the Perot Museum of Nature and Science (Dallas Museum of Natural History) when the Alaskan Tyrannosaurid remains were finally recognized to represent a new taxon, as opposed to being synonymous with previous genera. This prompted the creation of a new genus, Nanuqsaurus, described and named by Anthony R. Fiorillo and Ronald S. Tykoski in 2014. The initially discovered material, referred to as DMNH 21461, is now recognized as the holotype of Nanuqsaurus. As well as this, the initial discoveries of teeth were placed as more likely to be the remains of Nanuqsaurus as opposed to any other known creature, contrary to the initial proposals of the origin of the teeth.[3]
Etymology
The type species, Nanuqsaurus hoglundi, has its generic name derived from the Iñupiaq word nanuq, which means “polar bear”, and the Greek word sauros, which means "lizard". The specific name honors the philanthropist Forrest Hoglund in regards to his work on philanthropy and cultural institutions.[3]
Description

Initially, Nanuqsaurus was estimated to have been about 16 to 20 feet long, based on the holotype specimen, which put the animal at about half the length of Tyrannosaurus rex.[5][6][7] The length of the same specimen's reconstructed skull, based on the proportions of related animals, was 24 to 28 inches.[3] Its weight was also estimated to be 1,100 to 2,000 lbs.[5][7] This diminutive size was postulated by Fiorillo and Tykoski as being an adaptation to its high latitude arctic habitat.[3] However, later studies suggested that its supposed small size was unfounded, and that it was likely similar in size to other North American tyrannosaurids, such as Albertosaurus, based on undescribed adult sized teeth and postcranial elements.[8] Some of the undescribed postcranial elements scale to around 23 feet in length, described as comparable to a juvenile Tarbosaurus.[9] If Nanuqsaurus did indeed grow to a similar length as Albertosaurus, as previously suggested, a total body length of anywhere between 26 to 30 feet is generally expected.[8]

Nanuqsaurus would have likely resembled other large tyrannosaurines, such as Daspletosaurus, with both animals being closely related and probably serving similar roles in their respective ecosystems.[10] Nanuqsaurus itself is anatomically diagnosed by 1) a thin, rostrally forked, median spur of the fused parietals on the dorsal skull roof that overlaps and separates the frontals within the sagittal crest, 2) frontals with a long, rostrally pointed process separating the prefrontal and lacrimal facets, and 3) that the first two dentary teeth are much smaller than the dentary teeth behind them.[3]
Classification
Phylogenetic analysis of Tyrannosauridae finds that Nanuqsaurus is a close relative of Daspletosaurus and Tyrannosaurus within Tyrannosaurinae. The cladogram below illustrates the relationships of Tyrannosauridae.[10]

Tyrannosauridae |
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Paleobiology
Reproduction at Polar Latitudes
Analysis of material attributed to Nanuqsaurus and other Alaskan dinosaurs from the same environment has resulted in the Prince Creek Formation being recognized as having preserved an exceptionally high percentage of young dinosaurs when compared to the amount of families represented in the formation. Material from young dinosaur specimens, including birds, has been determined to be present from seven different major clades, or 70% of all the recognized families of the quarry. The families in question are Hadrosauridae, Thescelosauridae, Leptoceratopsidae, Ceratopsidae, Tyrannosauridae, Dromaeosauridae, Troodontidae, and Avialae. This evidence suggests that both Nanuqsaurus and its likely prey items remained in the Arctic yearlong, and thus would have had to cope with about 120 days of constant winter darkness each year, as opposed to migrating further south to escape the harsh conditions. It is proposed that the animals would likely have laid their eggs toward the beginning of the constant daylight period, around the month of April, allowing time for their eggs to incubate in the relative heat of this part of the year.[8][11]
Paleoecology

The holotype specimen assigned to Nanuqsaurus comes from the mid Maastrichtian age Prince Creek Formation. At an age of 70 to 68 million years ago, the Kikak-Tegoseak Quarry region if the Prince Creek Formation dates to the mid Maastrichtian. An average age found in dating rocks from the formation is 69.1 ± 0.3 million years ago, so it is likely that Nanuqsaurus is from around that age. The formation is along the Colville River on the North Slope Borough, and is made up of alluvial sediments. It is one of a few dinosaurs to live at very high latitude arctic areas.[3][12]
Nanuqsaurus lived alongside many other dinosaurs in the Prince Creek formation region during the Edmontonian faunal stage in a climate that was around 50 to 53.6° F during summer and about 27° F ± 39° F during the winter.[8] Other animals alongside Nanuqsaurus include an unnamed leptoceratopsid, the hadrosaurid Edmontosaurus (similar to E. regalis),[13] an unnamed lambeosaurine, an unnamed thescelosaurine (mentioned to be similar to Parkosaurus and Thescelosaurus), an unnamed orodromine (mentioned to be similar to Orodromeus), the ceratopsid Pachyrhinosaurus perotorum, the pachycephalosaurid Alaskacephale, a large troodontid referred to the dubious genus Troodon, the dromaeosaurids Dromaeosaurus and Richardoestesia (similar to R. isosceles), an unnamed saurornitholestine, an unnamed ornithomimosaur, and multiple avialans.[8] In contrast to the contemporary large herbivores Edmontosaurus and Pachyrhinosaurus, which apparently preferred coastal lowland and upland environments respectively, Nanuqsaurus appears to have been fairly ubiquitous throughout the Prince Creek landscape.[14]
See also
References
- Fiorillo, Anthony R.; Gangloff, Roland A. (2010-08-24). "Theropod teeth from the Prince Creek Formation (Cretaceous) of northern Alaska, with speculations on Arctic Dinosaur paleoecology". Journal of Vertebrate Paleontology. 20: 675. doi:10.1671/0272-4634(2000)020[0675:TTFTPC]2.0.CO;2. ISSN 0272-4634.
- Ryan, Michael J.; Chinnery-Allgeier, Brenda J.; Eberth, David A. (2010). New Perspectives on Horned Dinosaurs: The Royal Tyrrell Museum Ceratopsian Symposium. Indiana University Press. ISBN 978-0-253-35358-0.
- 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.
- Conrad, James E.; McKee, Edwin H.; Turrin, Brent D. (1992). Age of Tephra Beds at the Ocean Point Dinosaur Locality, North Slope, Alaska, Based on K-Ar and 40Ar/39Ar Analyses. U.S. Government Printing Office.
- Molina-Pérez & Larramendi 2016. Récords y curiosidades de los dinosaurios Terópodos y otros dinosauromorfos, Larousse. Barcelona, Spain p. 259
- "New Pygmy Tyrannosaur Found, Roamed the Arctic". news.nationalgeographic.com. Archived from the original on 12 April 2019. Retrieved 11 January 2022.
- Paul, Gregory S. (2016). The Princeton Field Guide to Dinosaurs 2nd Edition. New Jersey: Princeton University Press. p. 114.
- Druckenmiller, Patrick S.; Erickson, Gregory M.; Brinkman, Donald; Brown, Caleb M.; Eberle, Jaelyn J. (2021-06-24). "Nesting at extreme polar latitudes by non-avian dinosaurs". Current Biology. 31 (16): 3469–3478.e5. doi:10.1016/j.cub.2021.05.041. ISSN 0960-9822. PMID 34171301.
We note that other Prince Creek Formation tyrannosaurid material in the UAMES collection do not support the assertion that Nanuqsaurus is a diminutive, small-bodied tyrannosaur. Rather, adult-sized teeth and isolated postcranial elements suggest an adult body size more closely comparable to other North American tyrannosaurid taxa, such as Albertosaurus sarcophagus.
- "Nanuqsaurus description by Pat Druckenmiller for Alaska Paleo-Project "Northern Tyrant King"". Youtube.
{{cite web}}
: CS1 maint: url-status (link) - Voris, Jared T.; Therrien, François; Zelenitsky, Darla K.; Brown, Caleb M. (2020-06-01). "A new tyrannosaurine (Theropoda:Tyrannosauridae) from the Campanian Foremost Formation of Alberta, Canada, provides insight into the evolution and biogeography of tyrannosaurids". Cretaceous Research. 110: 104388. doi:10.1016/j.cretres.2020.104388. ISSN 0195-6671. S2CID 213838772.
- Herman, Alexei B.; Spicer, Robert A.; Spicer, Teresa E. V. (2016-01-01). "Environmental constraints on terrestrial vertebrate behaviour and reproduction in the high Arctic of the Late Cretaceous". Palaeogeography, Palaeoclimatology, Palaeoecology. Selected papers based on Geological Society of America, Annual Meeting, Theme Session 241, Ancient Polar Ecosystems and Climate History in Deep Time, Denver, Colorado, USA, 30 October 2013. 441: 317–338. doi:10.1016/j.palaeo.2015.09.041. ISSN 0031-0182.
- Fiorillo, Anthony R.; Gangloff, Roland 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. doi:10.1671/0272-4634(2000)020[0675:TTFTPC]2.0.CO;2.
- Takasaki, Ryuji; Fiorillo, Anthony R.; Tykoski, Ronald S.; Kobayashi, Yoshitsugu (2020-05-06). "Re-examination of the cranial osteology of the Arctic Alaskan hadrosaurine with implications for its taxonomic status". PLOS ONE. 15 (5): e0232410. Bibcode:2020PLoSO..1532410T. doi:10.1371/journal.pone.0232410. ISSN 1932-6203. PMC 7202651. PMID 32374777.
- Fiorillo, Anthony R.; McCarthy, Paul J.; Flaig, Peter P. (1 January 2016). "A multi-disciplinary perspective on habitat preferences among dinosaurs in a Cretaceous Arctic greenhouse world, North Slope, Alaska (Prince Creek Formation: lower Maastrichtian)". Palaeogeography, Palaeoclimatology, Palaeoecology. 441, Part 2: 377–389. doi:10.1016/j.palaeo.2015.07.024.