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Synchrotron scanning reveals amphibious ecomorphology in a new clade of bird-like dinosaurs

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Maniraptora includes birds and their closest relatives among theropod dinosaurs. During the Cretaceous period, several maniraptoran lineages diverged from the ancestral coelurosaurian bauplan and evolved novel ecomorphologies, including active flight, gigantism, cursoriality and herbivory. Propagation X-ray phase-contrast synchrotron microtomography of a well-preserved maniraptoran from Mongolia, still partially embedded in the rock matrix, revealed a mosaic of features, most of them absent among non-avian maniraptorans but shared by reptilian and avian groups with aquatic or semiaquatic ecologies. This new theropod, Halszkaraptor escuilliei gen. et sp. nov., is related to other enigmatic Late Cretaceous maniraptorans from Mongolia in a novel clade at the root of Dromaeosauridae. This lineage adds an amphibious ecomorphology to those evolved by maniraptorans: it acquired a predatory mode that relied mainly on neck hyperelongation for food procurement, it coupled the obligatory bipedalism of theropods with forelimb proportions that may support a swimming function, and it developed postural adaptations convergent with short-tailed birds.
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21/28 DECEMBER 2017 | VOL 552 | NATURE | 395
LETTER doi:10.1038/nature24679
Synchrotron scanning reveals amphibious
ecomorphology in a new clade of bird-like dinosaurs
Andrea Cau1, Vincent Beyrand2,3, Dennis F. A. E. Voeten2,3, Vincent Fernandez2, Paul Tafforeau2, Koen Stein4, Rinchen Barsbold5,
Khishigjav Tsogtbaatar6, Philip J. Currie7 & Pascal Godefroit8
Maniraptora includes birds and their closest relatives among
theropod dinosaurs1–5. During the Cretaceous period, several
maniraptoran lineages diverged from the ancestral coelurosaurian
bauplan and evolved novel ecomorphologies, including active
flight2, gigantism3, cursoriality4 and herbivory5. Propagation X-ray
phase-contrast synchrotron microtomography of a well-preserved
maniraptoran from Mongolia, still partially embedded in the rock
matrix, revealed a mosaic of features, most of them absent among
non-avian maniraptorans but shared by reptilian and avian groups
with aquatic or semiaquatic ecologies6–14. This new theropod,
Halszkaraptor escuilliei gen. et sp. nov., is related to other enigmatic
Late Cretaceous maniraptorans from Mongolia
15,16
in a novel clade
at the root of Dromaeosauridae17. This lineage adds an amphibious
ecomorphology to those evolved by maniraptorans: it acquired a
predatory mode that relied mainly on neck hyperelongation for food
procurement, it coupled the obligatory bipedalism of theropods with
forelimb proportions that may support a swimming function, and it
developed postural adaptations convergent with short-tailed birds.
Theropoda Marsh, 1881
Maniraptora Gauthier, 1986
Dromaeosauridae Matthew and Brown, 1922
Halszkaraptorinae subfam. nov.
Definition. The most inclusive clade that contains Halszkaraptor
escuilliei gen. et sp. nov., but not Dromaeosaurus albertensis, Unenlagia
comahuensis, Saurornithoides mongoliensis or Vu ltur g r yph u s. Taxa
included: Halszkaraptor escuilliei, Hulsanpes perlei15 and Mahakala
omnogovae16. Type species: Halszkaraptor escuilliei.
Diagnosis. Long-necked dromaeosaurids with proximal caudal
vertebrae that have horizontally oriented zygapophyses and prominent
zygodiapophyseal laminae; flattened ulna with a sharp posterior margin;
metacarpal III shaft transversely as thick as that of metacarpal II;
ilium with a shelf-like supratrochanteric process; posterodistal
surface of femoral shaft with an elongate fossa bound by a lateral crest;
proximal half of metatarsal III unconstricted and markedly convex
anteriorly.
Halszkaraptor escuilliei gen. et sp. nov.
Et y m ology. Halszka, a Latinized form of archaic Polish Halżka, honours
Halszka Osmólska (1930–2008) for her contributions to theropod
palaeontology, which include the description of the first halszkarap-
torine species found (Hulsanpes perlei)15; raptor, ‘robber’ (Latin). The
specific name escuilliei refers to François Escuillié, who returned the
poached holotype to Mongolia.
Holotype. MPC (Institute of Paleontology and Geology, Mongolian
Academy of Sciences, Ulaanbaatar, Mongolia) D-102/109 (Figs 1, 2,
3a–f, Extended Data Figs 2–8, Supplementary Table 1); an articulated
and almost complete skeleton preserved three-dimensionally.
Locality and horizon. Bayn Dzak Member, Djadokhta Formation
(Campanian, ~ 75–71 Mya), Ukhaa Tolgod, Mongolia (see
Supplementary Information).
Diagnosis. Autapomorphies are marked by asterisks; differential
diagnosis can be found in Supplementary Information. Platyrostral
premaxilla that forms 32% of snout length* and bears 11 teeth* ; external
naris posterior to the premaxillary oral margin; rod-like jugal with an
ascending process excluded from the orbital margin that forms only
10% of the postorbital bar* ; rod-like ventral ramus of the postorbital;
22 presacral vertebrae; neck forms 50% of snout–sacrum length* ;
absence of epipophyses* ; ridge-like cervical neural spines restricted
to the 2nd–5th vertebrae* ; postzygapophyses on cervicals 2–5 are
fused medially and form single lobate processes* ; pleurocoels restricted
to cervicals 7–9; tuber-like neural spines in tail are restricted to the
1st–3rd vertebrae* ; proximal-most chevrons large and pentagonal* ;
transition point in 7th–8th caudals; 3rd finger longer than 2nd; elongate
pedal phalanx III-1 is 47% of the length of metatarsal III* .
We performed multi-resolution scanning at the European
Synchrotron Radiation Facility using BM05 and ID19 beamlines;
this revealed all the elements that were still embedded in matrix
and demonstrated the integrity of the specimen (Supplementary
Information, Extended Data Figs 1–3). Histological analysis indi-
cates that MPCD-102/109 was a subadult individual (Supplementary
Information, Extended Data Figs 4, 5). The platyrostral premaxilla
with a dorsolaterally oriented external naris that is retracted beyond
the oral margin is unique among theropods, although in its elonga-
tion, the premaxilla is similar to those of spinosaurids8 (Fig. 2a–g,
Extended Data Figs 6, 8). A hypertrophied network of neurovascular
chambers penetrates throughout the premaxilla. This condition
is also seen in aquatic reptiles, such as plesiosaurs12 and crocodiles
(Fig. 2e, f, Extended Data Fig. 8), whereas in other theropods this neuro-
vascular network resides exclusively in the lateral half of the premaxilla13.
Each premaxilla bears 11 teeth (Fig. 2g, Extended Data Figs 6, 7),
which is the highest number found in any dinosaur. Spinosaurids and
Pelecanimimus approach Halszkaraptor in having six or seven premaxil-
lary teeth
8
, whereas most theropods have four. Both the maxilla and
the dentary bear 20–25 teeth; this is comparable to the condition seen
in unenlagiines
17
and baryonychines
8
. Although some maniraptori-
forms carry a total of over 30 small maxillary and/or dentary teeth
5
,
most theropods have fewer than 20. The heterodont dentition of
Halszkaraptor involves closely packed premaxillary teeth with long
roots and incisiviform crowns, and a labiolingually compressed pos-
terior dentition with shorter roots and concave distal crown margins
(Fig. 3d, Extended Data Fig. 7). All teeth lack serrations, as is the
case in most paravians7, spinosaurines8 and a few other theropods.
Synchrotron scanning revealed a delayed replacement pattern in the
anterior dentition14, whereas the majority of the posterior teeth are
associated with a replacement tooth.
1Geological and Palaeontological Museum ‘Giovanni Capellini’, I-40126 Bologna, Italy. 2European Synchrotron Radiation Facility, F-38043 Grenoble, France. 3Department of Zoology and
Laboratory of Ornithology, Palacký University, CS-40220 Olomouc, Czech Republic. 4Earth System Science – AMGC Vrije Universiteit Brussel, B-1050 Brussels, Belgium. 5Palaeontological Center,
Mongolian Academy of Sciences, Ulaanbaatar 201-351, Mongolia. 6Institute of Palaeontology and Geology, Mongolian Academy of Sciences, Ulaanbaatar 210-351, Mongolia. 7Department of
Biological Sciences, University of Alberta, Edmonton, Alberta T6G 2E9, Canada. 8Directorate Earth & History of Life, Royal Belgian Institute of Natural Sciences, B-1000 Brussels, Belgium.
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