Dakotaraptor

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Dakotaraptor
Temporal range: Late Cretaceous, 66 Ma
Dakotaraptor lateral Wiki.jpg
A restored replica of the Dakotaraptor holotype compared to silhouettes of Deinonychus, Velociraptor and a human
Scientific classification e
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Order: Saurischia
Suborder: Theropoda
Clade: Deinonychosauria
Genus: Dakotaraptor
DePalma et al. 2015[1]
Type species
Dakotaraptor steini
DePalma et al. 2015[1]

Dakotaraptor is a genus of large dromaeosaurid theropod dinosaur that lived in North America during the Late Cretaceous period. The remains have been found in the Maastrichtian stage of the Hell Creek Formation, dated to the very end of the Mesozoic era, making Dakotaraptor one of the last surviving dromaeosaurids. The remains of D. steini were discovered in a multi-species bonebed.[1] Elements of the holotype and referred specimens were later found to belong to trionychid turtles[2],and further analysis of potential non-dromaeosaurid affinities of the holotype and referred material have not yet been conducted. Phylogenetic analyses of D. steini place it in a variety of positions in the Dromaeosauridae.[1][3]

Discovery and naming[edit]

In 2005, paleontologist Robert DePalma in Harding County, South Dakota discovered a fluvial bonebed bearing the remains of a variety of dinosaurian and non-dinosaurian remains, which yielded a partial skeleton attributed by DePalma to a large dromaeosaurid. Subsequently, the same site produced additional dromaeosaurid remains.[4] In 2015, the type species Dakotaraptor steini was named and described by Robert A. DePalma, David A. Burnham, Larry Dean Martin, Peter Lars Larson and Robert Thomas Bakker. The generic name, Dakotaraptor, combines a reference to South Dakota and the Dakota people with the Latin word raptor, meaning "plunderer". The specific name, steini, honours paleontologist Walter W. Stein.[1] Dakotaraptor was one of eighteen dinosaur taxa from 2015 to be described in open access or free-to-read journals.[5]

Quarry map of the bones

The holotype, PBMNH.P.10.113.T, was found in a sandstone layer of the upper Hell Creek Formation, dating from the late Maastrichtian. It consists of a partial skeleton, lacking the skull, of an adult individual. It contains a piece of a back vertebra, ten tail vertebrae, both humeri, both ulnae, both radii, the first and second right metacarpals, three claws of the left hand, a right thighbone, both shinbones, a left astragalus bone, a left calcaneum, the left second, third and fourth metatarsal, the right fourth metatarsal, and the second and third claw of the right foot. An assigned furcula was later excluded from the specimen.[6] Apart from the remains of the holotype, in the site bones were discovered that also belonged to Dakotaraptor but which represented a more gracile morph. These included the specimens PBMNH.P.10.115.T: a right shinbone; PBMNH.P.10.118.T: a connected left astragalus and calcaneum; and KUVP 152429: originally identified as a furcula, but now also excluded from the known remains of Dakotaraptor.[6] Additionally four isolated teeth were referred, specimens PBMNH.P.10.119.T, PBMNH.P.10.121.T, PBMNH.P.10.122.T, and PBMNH.P.10.124.T. These fossils are part of the collection of The Palm Beach Museum of Natural History. Other referred fossils are KUVP 156045, an isolated tooth,[1] and NCSM 13170, a third supposed furcula later identified as not belonging to Dakotaraptor.[6]

Description[edit]

Size[edit]

Dakotaraptor is exceptionally large for a dromaeosaurid; it has an estimated adult length of 5.5 m (18 ft).[1] This approaches the size of the largest known dromaeosaurid, Utahraptor. Dakotaraptor however, does not have the proportions and adaptations of Utahraptor, but more closely resembles smaller dromaeosaurids like Deinonychus.[1]

Distinguishing traits[edit]

Life restoration by Emily Willoughby, 2015

Apart from the large size, the description of 2015 indicated some additional distinguishing traits. On the fourth foot claw, the boss that serves as an attachment for the tendon of the flexor muscle is reduced in size. The "blood groove" on the outer side of the fourth claw of the foot, towards the tip is fully enclosed over half of its length, forming a bony tubular structure. The second and third claws of the foot have sharp keels at their undersides. The second foot claw, the "sickle claw", equals 29% of the thighbone length. On the shinbone, the crista fibularis, the crest that contacts the calfbone, is long and lightly built with a height that does not exceed 9% of the crest length. The upper edge of this crest ends in a hook. On the second metacarpal, of the two condyles that contact the finger, the inner one is almost as large as the outer one. The outer side of the second metacarpal has but a shallow groove for the ligament that connects it to the third metacarpal. When the arm is seen in a flat position, of the second metacarpal the edge between the wrist joint and the upper shaft is straight in top view. The teeth have fifteen to twenty denticles per 5 millimetres (0.20 in) on the rear edges and twenty to twenty-seven denticles on the front edges.[1]

Skeleton[edit]

Vertebral column[edit]

Skeletal composite showing the known elements

The vertebrae of the back are highly pneumatised, filled with trabecular bone that shows many air spaces. On the middle tail vertebrae the front joint processes, the prezygapophyses, are extremely elongated with an estimated intact length of 70 centimetres (28 in), spanning about ten vertebrae. This stiffens the tail.[1]

Forelimb[edit]

Like virtually all other theropods, Dakotaraptor likely possessed a furcula, or “wishbone”, as part of the shoulder girdle. Theropod wishbones are quite varied and often different from the strongly U-shaped furculae most modern birds possess; the elements originally identified as the furcula of Dakotaraptor were U- to V-shaped, similar to many other dromaeosaurids such as Velociraptor, and even the large spinosaurid theropod Suchomimus. In 2015, a study by Victoria Megan Arbour et al. proposed that the presumed Dakotaraptor furculae in fact represented a part of a turtle armour, the entoplastron of Axestemys splendida, a member of the Trionychidae.[2] In 2016, DePalma et al. recognized that none of the referred furculae actually belonged to Dakotaraptor, and excluded them from its hypodigm.[6]

Proposed furcula compared with other theropod dinosaurs. Said furcula was later shown to be an element from a trionychid turtle.

The wing of Dakotaraptor was given much attention in the describing article. Here, “wing” is used as an anatomical descriptive term not related to its functionality, since Dakotaraptor was flightless. This is similar to the term “wing” for the same appendages in ostriches, emus, and other flightless birds. It is meant to express that arm is equipped with long feathers. Many of the wing bones were discovered (humerus, radius, ulna, two of the three metacarpal wrist bones, and parts of the finger digits), so the wing is very complete. The humerus, the upper arm bone, is relatively long and slender. It is somewhat bent to the inside. The most notable anatomical feature is the row of very prominent bumps along a ridge on the lower edge of the ulna, one of the forearm bones. These are called ulnar papillae, or quill knobs. In birds and some other theropod dinosaurs, these bumps were spots for reinforced attachment of the remiges, or wing feathers. When quill knobs are present, this is considered a strong indication that the animal had long remiges on the wings. Since quill knobs are rare in the fossil record, paleontologists mainly relied on phylogenetic bracketing to determine if a species was likely to have had wing feathers - if a relative on a "higher" branch of the evolutionary tree had the feathers, and one on a "lower" branch down had them also, then a species in the middle position likely did as well. Dakotaraptor’s quill knobs show that the animal unequivocally had prominent wing feathers, making it the largest dromaeosaurid with confirmed plumage of that type. The quill knobs of Dakotaraptor have a diameter of about 8–10 millimetres (0.31–0.39 in), which shows that these feathers were rather large. It was estimated that a complete series might include fifteen of these papillae ulnares. The ulna is 36 centimetres (14 in) long and the other lower arm bone, the radius, measures 32 centimetres (13 in). The hand bones show that their joints allowed for little mobility. The wingspan of Dakotaraptor was estimated at 120 centimetres (47 in), not taking into account possible primary remiges longer than the hand.[1]

The second metacarpal of the metacarpus of the hand, the bone that primary remiges attach to, also had a flat bony shelf as its dorsal surface. The shelf made a perfect spot for the primary feathers to lay across in their life-attachment.[1]

Hindlimb[edit]

The foot claws of the Dakotaraptor holotype, showing the flexor tubercles for muscle attachment

Overall, the hindlimb is built lightly and with long elements, contrary to the robust, stocky hind limbs of Utahraptor. Dakotaraptor more closely resembles the agile, springy smaller dromaeosaurids and would have been well-suited at running and pursuit predation. The length of the thighbone is 558 millimetres (22.0 in). It is relatively shorter and more lightly built than that of Utahraptor. To the contrary the shinbone is rather elongated. The holotype shinbone is, with a length of 678 millimetres (26.7 in), the longest dromaeosaurid tibia known. It is 22% longer than the thighbone, indicating a good running capability. The shinbone's cnemial crest has a sharp corner pointing to the front. Its fibular crest ends in a hook-shaped process pointing to above, a condition that is unique in the entire Theropoda. The astragalus and calcaneum, the upper ankle bones, are fused just as in Bambiraptor. The top of the calcaneum has but a small contact facet for the calfbone, indicating that this fibula must have had a very narrow lower end.[1] The metatarsus has an estimated length of 32 centimetres (13 in), which makes it rather long relative to the remainder of the hindlimb.[1]

The foot claws of Dakotaraptor include a typical dromaeosaurid raptorial second claw, or "sickle claw", which was used for killing or holding down prey. It is large and robust with a diameter of 16 centimetres (6.3 in) and a length of 24 centimetres (9.4 in) measured along the outer curve. This equals 29% of the length of the thighbone, compared to 23% in Deinonychus. The claw is transversely flattened and has a droplet-shaped cross-section. The flexor tubercle, a large bump near the base, served as an attachment site for flexor muscles - the larger it was, the greater the slashing strength. Dakotaraptor has a flexor tubercle that is larger relative to overall claw size than it is in other discovered dromaeosaurids, potentially giving it the strongest slashing strength of any known member of this group. The flexor tubercle on the third claw of the foot is almost non-existent, very reduced in size compared to other dromaeosaurids, suggesting a more minimized use of that claw. As these are the bony cores of the claws, they would have been covered in a keratinous sheath that extended the "nail" and ended in a sharp tip. The third claw too is keeled but is much smaller with a tip to joint length of 7 centimetres (2.8 in) and a curve length of 9 centimetres (3.5 in). The groove on its outer side towards the tip ends in a bone tunnel, a rare condition.[1]

Classification[edit]

Comparison between Dakotaraptor and other giant Dromaeosaurids

Dakotaraptor was placed in the Dromaeosauridae. A cladistic analysis showed that it was the sister species of Dromaeosaurus. They again formed a clade with Utahraptor, of which clade Achillobator was the direct side branch. Despite being related to other gigantic dromaeosaurids, Dakotaraptor was suggested to represent a separate fourth instance of dromaeosaurid size increase, besides Deinonychus, Unenlagia, and the Achillobator plus Utahraptor clade.[1]

Eudromaeosauria

Saurornitholestes

Velociraptor

Dromaeosaurinae

Deinonychus

Atrociraptor

Achillobator

Utahraptor

Dakotaraptor

Dromaeosaurus

A recent study conducted by Hartman et al. 2019, proposed a placement of Dakotaraptor in the Unenlagiinae.[7]

Unenlagiinae

Austroraptor

Buitreraptor

Pyroraptor

Pamparaptor

Rahonavis

Ornithodesmus

Dakotaraptor

Unenlagia

Possible synonymy with Acheroraptor[edit]

Acheroraptor temertyorum is another theropod from the Hell Creek Formation, named in 2013 for a lower jaw, a maxilla, and some teeth. Acheroraptor was diagnosed by multiple features, including the possession of ridges on the teeth.[8] Teeth are the only overlapping features between Acheroraptor and Dakotaraptor. However Acheroraptor is significantly smaller, and differs from Dakotaraptor only in that it possesses vertical ridges on the teeth crowns.[9] Andrea Cau noted that though Dakotaraptor is known from individuals of differing sizes, some of the smaller specimens are also fully mature, and it is possible that the size difference means Dakotaraptor is simply a different species or size morph of Acheroraptor. A phylogenetic analysis presented by Cau, though relying on fragmentary specimens, did not result in a close relationship between the two.[9]

Paleobiology[edit]

Dakotaraptor might have used its arms to keep its balance while subduing prey; here Ornithomimus is the victim

The keeled claw of the second toe, the "sickle claw", was used to bring down prey and had a more robust flexor tubercle than that of Utahraptor. To the contrary, the third foot claw was relatively smaller in size than with other dromaeosaurids and seems not to have had an important function in attacking prey animals.[1]

Two morphs, a robust and a gracile one, were present in the fossil material. A study of the bone histology showed that both morphs were adult, so the lighter build of some bones was not caused by a young age. Individual variety or pathologies might account for the difference but the simplest explanation is sexual dimorphism. It can as yet not be deduced which morph was male and which female.[1]

On the ulna of the lower arm, wide papillae ulnares or quill knobs are present, attachment points for large pennaceous feathers. Adult Dakotaraptor individuals were much too heavy to fly. Despite this flightless condition, the feathers were not reduced. There is a variety of possible alternative functions for its wings, including shielding of eggs, display, intimidation and keeping balance while pinning down prey with the sickle claw. These functions however, do not necessitate quill knobs and the describing authors considered it likely that Dakotaraptor descended from a smaller flying ancestor which had them.[1]

Paleoecology[edit]

Dakotaraptor is the first medium-sized predator discovered in the Hell Creek Formation (aside from the dubious Nanotyrannus), intermediate in length between gigantic tyrannosaurids like Tyrannosaurus and smaller Deinonychosaurians like Acheroraptor.[8] Its shinbone was longer than its thighbone, Dakotaraptor would have had a good running capacity, filling the niche of pursuit predator. Especially if it was a pack-hunter, cooperating in groups, it could have preyed upon larger herbivores, possibly competing with subadult tyrannosaurids in the 6–9 metres (20–30 ft) length range. It lived alongside other famous dinosaurs, such as: Tyrannosaurus, Triceratops, Pachycephalosaurus, Ornithomimus and Edmontosaurus.[1][10][11]

Dakotaraptor compared to contemporaneous fauna of the Hell Creek Formation (Dakotaraptor in caramel brown)

References[edit]

  1. ^ a b c d e f g h i j k l m n o p q r s t DePalma, R. A.; Burnham, D. A.; Martin, L. D.; Larson, P. L.; Bakker, R. T. (2015). "The First Giant Raptor (Theropoda: Dromaeosauridae) from the Hell Creek Formation". Paleontological Contributions (14). doi:10.17161/paleo.1808.18764.
  2. ^ a b Arbour, V.M.; Zanno, L.E.; Larson, D.W.; Evans, D.C.; Sues, H. (2015). "The furculae of the dromaeosaurid dinosaur Dakotaraptor steini are trionychid turtle entoplastra". PeerJ PrePrints. 3: e1957.
  3. ^ Hartman, Scott; Mortimer, Mickey; Wahl, William R.; Lomax, Dean R.; Lippincott, Jessica; Lovelace, David M. (2019-07-10). "A new paravian dinosaur from the Late Jurassic of North America supports a late acquisition of avian flight". PeerJ. 7: e7247. doi:10.7717/peerj.7247. ISSN 2167-8359. PMC 6626525. PMID 31333906.
  4. ^ DePalma, R. A. (2010). Geology, taphonomy, and paleoecology of a unique Upper Cretaceous bonebed near the Cretaceous-Tertiary Boundary in South Dakota (Master of Science thesis). University of Kansas. pp. 227 pp.
  5. ^ "The Open Access Dinosaurs of 2015". PLOS Paleo. 2016-01-06.
  6. ^ a b c d DePalma, R.A.; Burnham, D.A.; Martin, L.D.; Larson, P.L.; Bakker, R.T. (2016). "Corrigendum to: The First Giant Raptor (Theropoda: Dromaeosauridae) from the Hell Creek Formation". Paleontological Contributions. 16. doi:10.17161/1808.22120.
  7. ^ Hartman, S.; Mortimer, M.; Wahl, W. R.; Lomax, D. R.; Lippincott, J.; Lovelace, D. M. (2019). "A new paravian dinosaur from the Late Jurassic of North America supports a late acquisition of avian flight". PeerJ. 7: e7247. doi:10.7717/peerj.7247. PMID 31333906.
  8. ^ a b Evans, David C.; Larson, Derek W.; Currie, Philip J. (2013-11-19). "A new dromaeosaurid (Dinosauria: Theropoda) with Asian affinities from the latest Cretaceous of North America". Naturwissenschaften. 100 (11): 1041–1049. Bibcode:2013NW....100.1041E. doi:10.1007/s00114-013-1107-5. ISSN 0028-1042. PMID 24248432.
  9. ^ a b Cau, A. (2015-10-31). "Dakotaraptor... a giant Acheroraptor?". Theropoda.
  10. ^ Pearson, D. A.; Schaefer, T.; Johnson, K. R.; Nichols, D. J.; Hunter, J. P. (2002). "Vertebrate Biostratigraphy of the Hell Creek Formation in Southwestern North Dakota and Northwestern South Dakota". In Hartman, John H.; Johnson, Kirk R.; Nichols, Douglas J. (eds.). The Hell Creek Formation and the Cretaceous-Tertiary boundary in the northern Great Plains: An integrated continental record of the end of the Cretaceous. Geological Society of America. pp. 145–167. ISBN 9780813723617. Special Paper 361.
  11. ^ Arens, N. C.; Jahren, A. H.; Kendrick, D. (2014). "Carbon isotope stratigraphy and correlation of plant megafossil localities in the Hell Creek Formation of eastern Montana, USA". Special Paper of the Geological Society of America. 503: 149–171. doi:10.1130/2014.2503(05). ISBN 9780813725031.