Showing posts with label Coelurosauria. Show all posts
Showing posts with label Coelurosauria. Show all posts

Thursday, January 15, 2026

[Paleontology • 2026] Xenovenator espinosai • A Thick-Skulled Troodontid Theropod (Maniraptora: Troodontidae) from the Late Cretaceous of Mexico

 

Xenovenator espinosai 
Rivera-Sylva, Aguillón-Martinez, Flores-Ventura, Sánchez-Uribe, Guzman-Gutierrez & Longrich, 2026


Abstract
Dinosaurs repeatedly evolved adaptations for sexual selection over their 150-million year history, including adaptations for display and intraspecific combat. Adaptations for intraspecific combat have not previously been described in non-avian maniraptorans. We report a troodontid from the Campanian Cerro del Pueblo Formation of Coahuila, Mexico, showing a thickened and domed skull roof. The cranium is domed and bones are extremely thick, a morphology convergent on that of Pachycephalosauridae. Referred specimens show less thickening or doming, suggesting ontogenetic changes or perhaps sexual dimorphism. The holotype shows fusion of the frontal midline suture and tightly interdigitating sutures between skull bones, and a rugose skull roof. The specializations seen here suggest adaptation for intraspecific combat, specifically head-butting as hypothesized for pachycephalosaurids and pachyrhinosaurin ceratopsids. Repeated evolution of elaborate weapons and display features in the Cretaceous suggests that sexual selection became increasingly important in dinosaur evolution during the Cretaceous.

Keywords: Dinosauria; Theropoda; Maniraptora; Troodontidae; Cretaceous; Campanian; Laramidia; sexual selection; intraspecific combat


Saurischia Seeley, 1888 
Theropoda Marsh, 1881  
Avetheropoda Paul, 1988  
Coelurosauria Von Huene 1914  
Maniraptora Gauthier 1986  
Deinonychosauria Colbert and Russell, 1969 
Troodontidae Gilmore, 1924  
Troodontinae van der Reest and Currie, 2017 

Troodontini n. tax.


Xenovenator gen. nov.

Diagnosis. Troodontid characterized by thick frontals, anterior displacement of frontal postorbital processes relative to the parietal suture, broad and transversely arched interfrontal ridge, broad frontal-lacrimal suture.

Etymology. Greek xenos, ‘strange’ + Latin venator, ‘hunter’.

Xenovenator espinosai sp. nov. 

Holotype. CPC 2973, braincase including frontals, parietals, orbitosphenoids, laterosphenoids, exoccipitals, prootics, basisphenoid, basioccipital (Figure 4, Figure 5, Figure 6, Figure 7 and Figure 8).
 
Etymology. The species name honors Luis Espinosa, a pioneer in the study of Mexican dinosaurs and mentor to many generations of paleontologists.

Diagnosis. Xenovenator characterized by the following characters (* = autapomorphy): frontals extensively fused; frontals, parietals, and other cranial bones with strongly interdigitating sutures *; strong doming of frontals *; frontals and parietals massive (up to 12 mm thick) *, thickening well-developed anteriorly and less well-developed in the center of the frontal *; dorsal surface of frontals and parietals rugose and striated *, nasal processes broad between lacrimals *, orbital fossae widely separated ventrally *, frontal with notch and shelf to receive posterior end of lacrimal, parietal forms narrow process inserting between frontals *; triangular parietal table *, anteroventral expansion of the orbitosphenoids and laterosphenoids to enclose braincase ventrally *.

Horizon and Locality. Cerro Del Pueblo Formation, uppermost/latest Campanian (Figure 3), Coahuila, Mexico. CPC 2973 and CPC 3112 are from the La Parrita locality, 54 km west of Saltillo; municipality of General Cepeda, Coahuila, Mexico. CPC 3112 is from the Ejido Trincheras locality, 109 km west of Saltillo, municipality of Parras de la Fuente, Coahuila, Mexico (Figure 2).



 Hector E. Rivera-Sylva, Martha C. Aguillón-Martinez, Jose Flores-Ventura, Ivan E. Sánchez-Uribe, Jose Ruben Guzman-Gutierrez and Nicholas R. Longrich. 2026. A Thick-Skulled Troodontid Theropod from the Late Cretaceous of Mexico. Diversity. 18(1), 38. DOI: doi.org/10.3390/d18010038 [9 January 2026]

 

Saturday, November 29, 2025

[Paleontology • 2025] The coelurosaur theropods of the Romualdo Formation, early Cretaceous (Aptian) of Brazil: Santanaraptor placidus meets Mirischia asymmetrica


Hypothetical reconstruction of Mirischia asymmetrica (left) and Santanaraptor placidus (right) disputing a lizard in what is now northeastern Brazil ~112 million years ago (Early Cretaceous, Aptian).

Santanaraptor placidus Kellner, 1999 
Mirischia asymmetrica Naish, Martill & Frey, 2004

in Delcourt, Grillo, Hendrickx, Kellermann et Langer, 2025.
 Santanaraptor   Mirischia 
Illustration by Guilherme Gehr. 
 
Abstract
The upper carbonate concretion levels of the Romualdo Formation (Aptian, Brazil) have yielded several theropod dinosaur remains, including spinosaurids and the coelurosaurs Santanaraptor placidus and Mirischia asymmetrica, the phylogenetic affinities of which are controversial. Here, we present a comprehensive anatomical reassessment of the holotypes of both species (MN 4802-V and SMNK 2349 PAL, respectively), integrating newly observed osteological features and a detailed comparison of the pelvic and hind limb elements. Our preferred phylogenetic hypothesis places S. placidus and M. asymmetrica in the earliest-branching maniraptoromorph clade, along with Juratyrant langhami and Tanycolagreus topwilsoni from the Late Jurassic of Laurasia, suggesting an early diversification of coelurosaurs in that area, followed by Early Cretaceous dispersal events towards Gondwana. The comparative analysis of the two Romualdo taxa refutes their synonymy, given consistent differences in ischial (position and shape of the obturator plate and foramen) and tibial (condylar configuration) morphology. The observed morphological variation in the ischial obturator plate across early coelurosaurs further highlights a significant degree of homoplasy in this structure during the early radiation of the group. This revision underscores the need for additional research to further resolve the early evolutionary history of coelurosaur theropods.

Keywords: Araripe, Coelurosauria, Dinosauria, Gondwana, Theropoda

Hypothetical reconstruction of Mirischia asymmetrica (left) and Santanaraptor placidus (right) disputing a lizard in what is now northeastern Brazil ~112 million years ago (Early Cretaceous, Aptian).
Illustration by Guilherme Gehr. 

Santanaraptor placidus Kellner, 1999
Mirischia asymmetrica Naish, Martill & Frey, 2004

CONCLUSIONS: 
The comprehensive reassessment of Santanaraptor placidus (MN 4802-V) and Mirischia asymmetrica (SMNK 2349) presented here offers new insights into the anatomy, taxonomy, and phylogenetic affinities of these two coelurosaur theropods from the Early Cretaceous (Aptian) Romualdo Formation of Brazil. Despite the minor overlapping of skeletal elements, both specimens exhibit consistent anatomical differences that support their recognition as distinct species. These differences are particularly evident in the configuration of the ischial obturator plate and the structure of the proximal tibial condyles.

Some of our phylogenetic results place S. placidus and M. asymmetrica together with Juratyrant langhami and Tanycolagreus topwilsoni, from the Late Jurassic of Laurasia, in a clade of early branching maniraptoromorphs. This is the first time that these Brazilian taxa are found closely related within a lesser-inclusive clade, corroborating previous assumptions of close biogeographic relations between Laurasian and Gondwanan landmasses by the Early Cretaceous. Further biogeographic patterns are, however, harder to define, especially having in mind the still patchy record of Jurassic theropods in areas such as Africa, Australia, India, Antarctica, and South America.

 
Rafael Delcourt, Orlando Nelson Grillo, Christophe Hendrickx, Maximilian Kellermann, Max Cardoso Langer. 2025. The coelurosaur theropods of the Romualdo Formation, early Cretaceous (Aptian) of Brazil: Santanaraptor placidus meets Mirischia asymmetrica. The Anatomical Record. DOI: doi.org/10.1002/ar.70085 [18 November 2025]

Saturday, November 1, 2025

[Paleontology • 2025] Nanotyrannus and Tyrannosaurus coexisted at the close of the Cretaceous


Nanotyrannus   

in Zanno et Napoli, 2025.
Artwork: Anthony Hutchings

Tyrannosaurus rex ranks among the most comprehensively studied extinct vertebrates1 and a model system for dinosaur paleobiology. As one of the last surviving non-avian dinosaurs, Tyrannosaurus is a crucial datum for assessing terrestrial biodiversity, ecosystem structure, and biogeographic exchange immediately preceding the end-Cretaceous mass extinction —one of Earth’s greatest biological catastrophes. Paleobiological studies of Tyrannosaurus, including ontogenetic niche partitioning, feeding, locomotor biomechanics, and life history have drawn upon an expanding skeletal sample comprising multiple hypothesized growth stages—and yet the Tyrannosaurus hypodigm remains controversial. A key outstanding question relates to specimens considered to exemplify immature Tyrannosaurus, which have been argued to represent the distinct taxon Nanotyrannus. Here, we describe an exceptionally well-preserved, near somatically mature tyrannosaur skeleton (NCSM 40000) from the Hell Creek Formation that shares autapomorphies with the holotype specimen of N. lancensis. We couple comparative anatomy, longitudinal growth models, observations on ontogenetic character invariance, and a novel phylogenetic dataset to test the validity of Nanotyrannus, demonstrating conclusively that this taxon is distinguishable from Tyrannosaurus, sits outside Tyrannosauridae, and unexpectedly contains two species—N. lancensis and Nanotyrannus lethaeus, sp. nov. Our results prompt a re-evaluation of dozens of existing hypotheses based on currently indefensible ontogenetic trajectories. Finally, we document at least two co-occurring, ecomorphologically distinct genera in the Maastrichtian of North America, demonstrating that tyrannosauroid alpha diversity was thriving within one million years of the end-Cretaceous extinction.



A pack of Nanotyrannus attacks a juvenile Tyrannosaurus rex.
Artwork: Anthony Hutchings




  Lindsay E. Zanno and James G. Napoli. 2025. Nanotyrannus and Tyrannosaurus coexisted at the close of the Cretaceous. Nature.  DOI: doi.org/10.1038/s41586-025-09801-6  [30 October 2025]

Monday, July 14, 2025

[Paleontology • 2025] Shri rapax • A New bird-like Dinosaur from the Upper Cretaceous of Mongolia with extremely robust hands supports niche partitioning among velociraptorines


Shri rapax
Moutrille, Cau, Chinzorig, Escuillié, Tsogtbaatar, Ganzorig, Mallet & Godefroit, 2025

 
ABSTRACT
Dromaeosauridae is a clade of bird-like theropod dinosaurs including, among others, the genera Deinonychus and Velociraptor, and characterised by a specialised second toe bearing an enlarged and falciform ungual. Here, we describe an exquisitely-preserved velociraptorine dromaeosaurid from the Upper Cretaceous Djadokhta Formation of Mongolia, and refer it to the new species Shri rapax. This dromaeosaurid is diagnosed by a peculiar combination of vertebral and pelvic features and by an exceptionally robust hand with a very stout pollex bearing the ungual proportionally larger than in any other dromaeosaurid. Combined with cranial adaptations which could support a bite more powerful than in other velociraptorines, the enlarged unguals in both Shri species suggest ecological partitioning in prey preference among the sympatric Djadokhtan dromaeosaurids.

KEYWORDS: Cretaceous, Djadokhta Formation, Dromaeosauridae, Mongolia, Theropoda



Shri rapax
 

 
Léa Moutrille, Andrea Cau, Tsogtbaatar Chinzorig, François Escuillié, Khishigjav Tsogtbaatar, Bayasgaa Ganzorig, Christophe Mallet and Pascal Godefroit. 2025. A New bird-like Dinosaur from the Upper Cretaceous of Mongolia with extremely robust hands supports niche partitioning among velociraptorines. Historical Biology: An International Journal of Paleobiology. DOI: doi.org/10.1080/08912963.2025.2530148 [13 Jul 2025] 

Thursday, June 12, 2025

[Paleontology • 2025] Khankhuuluu mongoliensis • A new Mongolian tyrannosauroid and the Evolution of Eutyrannosauria


Khankhuuluu mongoliensis 
Voris, Zelenitsky, Kobayashi, Modesto, Therrien, Tsutsumi, Chinzorig & Tsogtbaatar, 2025


Abstract
Eutyrannosaurians were large predatory dinosaurs that dominated Asian and North American terrestrial faunas in latest Cretaceous times. These apex predators arose from smaller-bodied tyrannosauroids during the ‘middle’ Cretaceous that are poorly known owing to the paucity of fossil material. Here we report on a new tyrannosauroid, Khankhuuluu mongoliensis gen. et sp. nov., from lower Upper Cretaceous deposits of Mongolia that provides a new perspective on eutyrannosaurian origins and evolution. Phylogenetic analyses recover Khankhuuluu immediately outside Eutyrannosauria and recover the massive, deep-snouted Tyrannosaurini and the smaller, gracile, shallow-snouted Alioramini as highly derived eutyrannosaurian sister clades. Khankhuuluu and the late-diverging Alioramini independently share features related to a shallow skull and gracile build with juvenile eutyrannosaurians, reinforcing the key role heterochrony had in eutyrannosaurian evolution. Although eutyrannosaurians were mainly influenced by peramorphosis or accelerated growth, Alioramini is revealed as a derived lineage that retained immature features through paedomorphosis and is not a more basal lineage as widely accepted. Our results reveal that Asian tyrannosauroids (similar to Khankhuuluu) dispersed to North America, giving rise to Eutyrannosauria in the mid-Late Cretaceous. Eutyrannosauria diversified and remained exclusively in North America until a single dispersal to Asia in the latest Cretaceous that established Alioramini and Tyrannosaurini. Stark morphological differences between Alioramini and Tyrannosaurini probably evolved due to divergent heterochronic trends—paedomorphosis versus peramorphosis, respectively—allowing them to coexist in Asia and occupy different ecological niches.




Khankhuuluu mongoliensis gen. et sp. nov.



Jared T. Voris, Darla K. Zelenitsky, Yoshitsugu Kobayashi, Sean P. Modesto, François Therrien, Hiroki Tsutsumi, Tsogtbaatar Chinzorig and Khishigjav Tsogtbaatar. 2025. A new Mongolian tyrannosauroid and the Evolution of Eutyrannosauria. Nature. DOI: doi.org/10.1038/s41586-025-08964-6 [11 June 2025]

Thursday, April 10, 2025

[Paleontology • 2025] Huadanosaurus sinensis & Sinosauropteryx lingyuanensis • Two New compsognathid-like Theropods (Coelurosauria: Sinosauropterygidae) show diversified predation strategies in Theropod Dinosaurs


Huadanosaurus sinensis gen. et sp. nov. and
Sinosauropteryx lingyuanensis sp. nov.  

 Qiu, Wang, Jiang, Meng & Zhou, 2025
 illustrated by ZHAO Chuang facebook.com/PNSOus

ABSTRACT
The Compsognathidae was originally considered an early-diverging clade of coelurosaur theropods. However, recent study suggests that Compsognathidae is not monophyletic. Here, we describe two new compsognathid-like species, Sinosauropteryx lingyuanensis sp. nov. and Huadanosaurus sinensis gen. et sp. nov. from the Lower Cretaceous Yixian Formation of Dawangzhangzi (Lingyuan, Western Liaoning, China). The phylogenetic results indicate that all compsognathid-like theropods from the Early Cretaceous Jehol Biota form a monophyletic group Sinosauropterygidae nested among early-diverging coelurosaurs. Morphological comparison between various species of sinosauropterygids from the Early Cretaceous of Northeast China, combined with the phylogenetic results, suggests that at least three distinct hunting strategies were present among coeval species. The diversification of theropods should be attributed to the landscape caused by the destruction of the North China craton.

Early Cretaceous, Jehol Biota, Yixian Formation, Sinosauropterygidae, North China craton

Holotype of Huadanosaurus sinensis gen. et sp. nov. (IVPP V 14202: a, b) and
Sinosauropteryx lingyuanensis sp. nov. (IVPP V 12415:c, d).
Photographs and line drawings.
Black shading indicates the impression made by the skeleton. Dark grey shading indicates the mammalian bony stomach content.
 f, furcula; lc, left coracoid; lf, left femur; lh, left humerus; li, left ilium; lis, left ischium; lmt, left metatarsal; ls, left scapula; lt, left tibia; lu, left ulna; pu, pubis; rc, right coracoid; rd, right dentary; rf, right femur; rh, right humerus; ri, right ilium; ris, right ischium; rmc, right metacarpal; rmt, right metatarsal; rr, right radius; rs, right scapula; rt, right tibia; ru, right ulna. Scale bar, 10 cm.

Dinosauria Owen, 1842
Saurischia Seeley, 1888
Theropoda Marsh, 1881

Coelurosauria Von Huene, 1914
Sinosauropterygidae Ji et Ji, 1996

Sinosauropteryx Ji et Ji, 1996

Sinosauropteryx lingyuanensis sp. nov

Diagnosis. Differs from other sinosauropterygids in possessing the following autapomorphies: the jugal ramus of the maxilla subequal to the length of the snout; maxilla relatively low and elongated, maxillary fenestra large and subequal in size to the external naris; absence of the ischiatic boot.


Huadanosaurus sinensis gen. et sp. nov.

Diagnosis. Differs from other sinosauropterygids in possessing the following autapomorphies: large oval concavity between the anterior margin of the antorbital fossa and the maxilla; large lacrimal recess on the lacrimal, U-shaped bifurcation at the posteroventral margin of the dentary, small and crescent-shaped external mandibular fenestra, fanshaped neural spine on the axis, strongly anteroposteriorly elongated centrum in the posterior cervical vertebrae, small pleurocoel on centrum of the anterior dorsal vertebrae, the coracoid elongated lateromedially, not oval-shaped, the supracetabular crest well developed on the ilium, the obturator process >70% of the length of the ischial shaft, and the tibia ∼1.3 times of the femoral length.

Etymology. Huadan’, a Chinese word meaning the birthday of a great person or a great institution, commemorating the 75th anniversary of the founding of the People’s Republic of China and the Chinese Academy of Sciences, the 95th anniversary of the founding of the Palaeontological Society of China and the Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, and the 40th anniversary of the founding of the Chinese Society of Vertebrate Paleontology; ‘saurus’, Greek for lizard. ‘sine’, Latin referring to China

Huadanosaurus sinensis (left) and Sinosauropteryx lingyuanensis (right)
 illustrated by ZHAO Chuang


Rui Qiu, Xiaolin Wang, Shunxing Jiang, Jin Meng and Zhonghe Zhou. 2025. Two New compsognathid-like Theropods show diversified predation strategies in theropod dinosaurs. National Science Review, Volume 12(5); nwaf068. DOI: doi.org/10.1093/nsr/nwaf068 [22 February 2025]

  

   

Tuesday, March 25, 2025

[Paleontology • 2025] Duonychus tsogtbaatari • Didactyl therizinosaur (Coelurosauria: Therizinosauridae) with a preserved keratinous claw from the Late Cretaceous of Mongolia

 

Duonychus tsogtbaatari
Kobayashi, Zelenitsky, Fiorillo & Chinzorig, 2025
 
illustration by Masato Hattori

Highlights: 
• Duonychus tsogtbaatari is described as another therizinosaur from Mongolia
• It is a didactyl therizinosaur, possessing only two manual digits
• A keratinous sheath on digit I provides rare insight into theropod claw structure
• Duonychus reveals convergent digit III loss in at least five theropod clades

Summary
Therizinosaurs were a group of herbivorous/omnivorous theropod dinosaurs that lived in Asia and North America during the Cretaceous Period. These theropods are notable for their three-fingered hands sporting large claw-like unguals. Here, we describe a new and unusual species of the therizinosaurid Duonychus tsogtbaatari, recovered from the lower Upper Cretaceous Bayanshiree Formation of the Gobi Desert of Mongolia. This species is different from other therizinosaurs in that the hand possesses only two fingers, rather than three fingers, the typical condition for Avetheropoda, providing further insight into forelimb/hand reduction among theropods. Phylogenetically, Duonychus reveals a broader but still limited appearance of didactyly among avetheropodans. The manual ungual of Duonychus tsogtbaatari also preserves a nearly complete three-dimensional structure covering the ungual of the left manual digit I, which represents a keratinous manual claw. The strong curvature of this large claw and high ungual flexion indicate that Duonychus was likely amplectorial (grasping) and an effective grasper of vegetation, despite having only two functional fingers.

Systematic Paleontology
Theropoda  
Coelurosauria  
Therizinosauria  
Therizinosauridae 

 

Duonychus tsogtbaatari gen. et sp. nov.
 
Horizon and locality: The holotype specimen was collected from the Urlibe Khudak Locality (N43°27.092′, E107°23.476′) within the Bayanshiree Formation (Figure 1), which primarily consists of conglomerates, sandstones, and mudstones deposited in alluvial and fluvial settings, in the eastern Gobi Desert, Mongolia. This formation, dated to the Late Cretaceous, spans the Cenomanian to Santonian stages, as indicated by radiometric dating and biostratigraphic data. ...

Diagnosis: A derived therizinosaur exhibiting the following unique combination of characters: dorsal vertebrae with a long neural spine; a thick centrodiapophyseal lamina without additional laminae; dorsal vertebrae lacking pleurocoels; sacral vertebrae (2–4) with flat ventral surfaces; dorsal vertebrae possessing a weak ventral keel; pneumatic dorsal ribs; fused distal carpals 1 and 2; distal carpals 1 and 2 semilunate-shaped with a mediodorsal process; a small angle between the articular surfaces of the radiale for the semilunate carpal and the radius; a reduced metacarpal III forming a splint; absence of digit III; equally sized manual unguals I-2 and II-3; absence or reduction of the flexor fossa in manual phalanges; and a reduced dorsal process at the proximal end of manual phalanges. Duonychus can be distinguished from other therizinosaurs of the Bayanshiree Formation by several features. Its humerus has a more proximally positioned deltopectoral crest compared to Erlikosaurus, and in Duonychus, the entepicondyle is reduced with a markedly narrow groove separating it from the ulnar condyle. Unlike Enigmosaurus, which has a fused pubic boot and coalesced sacral vertebrae, Duonychus has an unfused pubic boot and ventrally flat sacral vertebrae with a shorter second sacral. Duonychus has an anteriorly deflected humeral shaft and a nearly straight ventral border of the pubic boot, distinguishing it from the convex shape seen in Segnosaurus.


Etymology: The generic epithet is derived from duo for two in Greek in reference to the presence of a didactyl hand which is unusual in therizinosaurs, and from onyx for claw in Greek. The species epithet honors Khishigjav Tsogtbaatar, a paleontologist and former director of the Institute of Paleontology, Mongolian Academy of Sciences in Ulaanbaatar, Mongolia.


 
Yoshitsugu Kobayashi, Darla K. Zelenitsky, Anthony R. Fiorillo and Tsogtbaatar Chinzorig. 2025. Didactyl therizinosaur with a preserved keratinous claw from the Late Cretaceous of Mongolia.  iScience. www.cell.com/iscience/fulltext/S2589-0042(25)00401-8  
DOI: 10.1016/j.isci.2025.112141 [March 25, 2025]

Thursday, February 20, 2025

[Paleontology • 2025] Evolutionary and Paleobiogeographic Implications of New carcharodontosaurian, megaraptorid, and unenlagiine Theropod Remains from the upper Lower Cretaceous of Victoria, southeast Australia

 


Cretaceous Australia Landscape
 
in Kotevski, Duncan, Ziegler, Bevitt, Vickers-Rich, Rich, Evans & Poropat, 2025. 
artwork by Jonathan Metzger

ABSTRACT
The Early Cretaceous non-avian theropod body fossil record of Victoria, Australia dominantly comprises isolated dental and postcranial remains. Numerous specimens have been collected from both the upper Strzelecki Group (upper Barremian–lower Aptian) and Eumeralla Formation (upper Aptian–lower Albian), yet theropod diversity in each unit remains poorly resolved. In both deposits, specimens pertaining to Megaraptoridae—a clade seemingly endemic to South America and Australia in the Cretaceous—are most frequently encountered. However, evidence of other typically common Gondwanan theropod groups, including Abelisauridae and Carcharodontosauria, has remained unknown. Herein, we describe five new theropod specimens: three tibiae, and two articulated caudal vertebrae with haemal arches, from the upper Strzelecki Group; and a single tibia from the Eumeralla Formation. Two of these tibiae—one each from the upper Strzelecki Group and the Eumeralla Formation—provide the first evidence for Carcharodontosauria in Australia. Two megaraptorid specimens from the upper Strzelecki Group—a tibia, and two caudal vertebrae with haemal arches—demonstrate that this clade had achieved large body size at the time of its first appearance in the fossil record. A tibia from the upper Strzelecki Group is interpreted to represent the Gondwanan dromaeosaur clade Unenlagiinae. Collectively, the new theropod remains described herein strengthen the evidence for mid-Cretaceous faunal interchange between Australia and South America across Antarctica, and highlight the presence of carcharodontosaurians and unenlagiines at high latitudes in the late Early Cretaceous.

Carcharodontosauria indet. right tibia (NMV P221042)
from the Eumeralla Formation of Victoria, Australia.  

Cretaceous Australia Landscape.
artwork by Jonathan Metzger, Museums Victoria


Jake Kotevski, Ruairidh J. Duncan, Tim Ziegler, Joseph J. Bevitt, Patricia Vickers-Rich, Thomas H. Rich, Alistair R. Evans and Stephen F. Poropat. 2025. Evolutionary and Paleobiogeographic Implications of New carcharodontosaurian, megaraptorid, and unenlagiine Theropod Remains from the upper Lower Cretaceous of Victoria, southeast Australia. Journal of Vertebrate Paleontology. e2441903. DOI: doi.org/10.1080/02724634.2024.2441903  

Wednesday, September 25, 2024

[Paleontology • 2024] Labocania aguillonae • A New Tyrant Dinosaur (Theropoda: Tyrannosauridae) from the Late Campanian of Mexico Reveals a Tribe of Southern Tyrannosaurs

  

 Labocania aguillonae
    Rivera-Sylva & Longrich, 2024

Artwork by Andrey Atuchin.

Abstract
The end of the Cretaceous saw the Western Interior Seaway divide North America into two land masses, Laramidia in the west and Appalachia in the east. Laramidian dinosaurs inhabited a narrow strip of land extending from Mexico to Alaska. Within this geographically restricted area, dinosaurs evolved high diversity and endemism, with distinct species in the north and south. Here, we report a new tyrannosaurid from the Late Campanian-aged Cerro del Pueblo Formation of Coahuila, Mexico, which is part of a tribe of tyrannosaurs originating in southern Laramidia. Phylogenetic analysis recovers the new tyrannosaur as part of a clade including Labocania anomala from the La Bocana Roja Formation of Baja California Norte, Bistahieversor sealeyi from the Kirtland Formation of New Mexico, Teratophoneus curriei from the Kaiparowits Formation in Utah, and Dynamoterror dynastes from the Menefee Formation of New Mexico. Distinct frontal morphology and the younger age (~72.5–73 Ma versus >75.8 Ma for L. anomala) support recognition of the new tyrannosaur as a distinct species of Labocania, Labocania aguillonae. The Labocania clade dominated southern Laramidia at a time when the north was dominated by daspletosaurins and albertosaurines. The high endemism seen in tyrannosaurids is remarkable, given that modern apex predators have large geographic ranges and hints that the diversity of carnivorous dinosaurs has been underestimated.

Keywords: Tyrannosauridae; dinosauria; Campanian; Cretaceous; Laramidia


Skeletal reconstruction of Labocania aguillonae (CPC 2974) showing preserved material. Scale = 1 m.

Systematic paleontology
Dinosauria—Owen 1842  
Theropoda—Marsh, 1881  
Coelurosauria—von Huene 1914  

Tyrannosauridae—Osborn, 1906 
Tyrannosaurinae—Osborn, 1906  
Teratophoneini—Scherer & Voiculescu-Holvad, 2024  

Labocania—Molnar 1974  
Labocania aguillonae sp. nov.

Diagnosis: Tyrannosaurine diagnosed by the following character combination (*—autapomorphies): orbit large and circular, with a very strongly convex anteroventral margin of the lacrimal* with a prominent, strongly dorsally extended* subocular process on the lacrimal along the anteroventral margin of the orbit; strong posteroventral extension of the antorbital fossa onto the lacrimal to end below the anterior margin of the orbit; lateral ends of frontals with a very prominent, acutely triangular shape, with strong transversely expanded overlap of frontal onto lacrimal; broad anteromedial extension of supratemporal fossa extending far forward onto frontal*; strong medial projection of postorbitals behind frontals onto dorsolateral surface of postorbital process, such that frontal underlaps the postorbital anteriorly*, lateral teeth with a figure-eight basal cross-section, and deep, prominent grooves or fullers extending from the root up the labial and lingual surfaces of the crown.

 Etymology: The species name honors Martha C. Aguillón, discoverer of the specimen and a long-time career paleontologist of Coahuila.


Conclusions: 
CPC 2974 represents a new species of tyrannosaurid, Labocania aguillonae, closely related to Labocania anomala, Bistahieversor sealeyi, and Teratophoneus curriei. It adds to the diversity of the Cerro del Pueblo Formation and shows that endemicity existed within tyrannosaurs in the Late Campanian, with distinct species and clades inhabiting the northern Great Plains in the north and the American Southwest and Mexico in the south. Given the limited geographic sampling, many tyrannosaur species likely remain undiscovered. Competition between species likely helped to enforce endemism among dinosaurs. Why large dinosaurs seem to have such unusually high levels of endemism compared to modern mammals remains unclear.



 Héctor E. Rivera-Sylva and Nicholas R. Longrich. 2024. A New Tyrant Dinosaur from the Late Campanian of Mexico Reveals a Tribe of Southern Tyrannosaurs. Foss. Stud. 2024, 2(4), 245-272. DOI: doi.org/10.3390/fossils2040012  www.mdpi.com/2813-6284/2/4/12

Sunday, July 28, 2024

[Paleontology • 2024] Asiatyrannus xui • The first deep-snouted tyrannosaur from Upper Cretaceous Ganzhou City of southeastern China


Asiatyrannus xui
 Zheng, Jin, Xie & Du, 2024
 

Abstract
Tyrannosaurids were the most derived group of Tyrannosauroidea and are characterized by having two body plans: gracile, long-snouted and robust, deep-snouted skulls. Both groups lived sympatrically in central Asia. Here, we report a new deep-snouted tyrannosauridAsiatyrannus xui gen. et sp. nov., from the Upper Cretaceous of Ganzhou City, southeastern China, which has produced the large-bodied and long-snouted Qianzhousaurus. Based on histological analysis, the holotype of Asiatyrannus xui is not a somatically mature adult, but it already passed through the most rapid growth stages. Asiatyrannus is a small to medium-sized tyrannosaurine, with a skull length of 47.5 cm and an estimated total body length of 3.5–4 m; or around half the size of Qianzhousaurus and other large-bodied tyrannosaurines in similar growth stages. Asiatyrannus and Qianzhousaurus are sympatric tyrannosaurid genera in the Maastrichtian of southeastern China. Asiatyrannus differs from Qianzhousaurus in that it has a proportionally deeper snout, longer premaxilla, deeper maxilla, and deeper dentary, and the cornual process of the lacrimal is inflated without developing a discrete horn. The different skull proportions and body sizes suggest that Asiatyrannus and Qianzhousaurus likely had different feeding strategies and occupied different ecological niches.
 
Keywords: Asiatyrannus xui, Tyrannosauridae, Nanxiong Formation, Upper Cretaceous, China
 

Systematic paleontology
Theropoda Marsh, 1881
Tetanurae Gauthier, 1986
Coelurosauria Huene, 1914

Tyrannosauroidea Osborn, 1905
Tyrannosauridae Osborn, 1905
Tyrannosaurinae Osborn, 1905

Asiatyrannus xui gen. et sp. nov.

Diagnosis: Asiatyrannus xui is a small to medium-sized tyrannosaurine theropod that differs from other tyrannosauroids in possessing the following autapomorphies: two small, deep fossae located on the lateral surface of the premaxilla just lateral to the anteroventral border of the external naris, a large and sub-rectangular shaped maxillary fenestra, the posterior protuberances of the nasals connect to form two separated medium low ridges, a low ridge-like jugal accessory horn, the ventral margin of the anterior ramus of the jugal curving ventrally anterior to the accessory horn, the lateral surface of the descending process of the postorbital developed the anterodorsally trending fine lineations, the slender, straight, and banded-shaped postorbital bar, with almost straight and parallel anterior and posterior margins in lateral view, and the lateral surangular shelf extends to the posterior end of the surangular.

Type locality: Nanxiong Formation (Upper Cretaceous, Maastrichtian) of Shahe Town, Nankang District, Ganzhou City, Jiangxi Province, China.


The photograph (A) and line drawing (B) of the skull of Asiatyrannus xui (ZMNH M30360) in right lateral view. The inset box in (A) indicates the position of the detailed jugal accessory horn in (C).
 acf accessory fossa of maxilla; ang angular; aof antorbital fenestra; cor cornual process; d dentary; d.t dentary tooth; emf external mandibular fenestra; en external naris; f frontal; gr groove; itf infratemporal fenestra; j jugal; jah jugal accessory horn; L left; la lacrimal; mf maxillary fenestra; mnvf maxillary neurovascular foramina; mx maxilla; nas nasal; nr nasal ridge; orb orbit; par parietal; pal palatine; pmx premaxilla; po postorbital; q quadrate; qj quadratojugal; R right; sa surangular; sf surangular foramen; snf subnarial foramen; sq squamosal; t1–6 maxillary tooth 1–6.

Fossil remains of Asiatyrannus xui (ZMNH M30360).
(A) Skeletal outlines showing recovered elements in yellow color. The skeletal reconstruction is the proportional scaling of Lythronax argestes drawn by Scott Hartman from Loewen et al.23; (B) the skull in right lateral view; (C) the caudal vertebrae in left lateral view; (D) the right femur in posterior view; (E) the right tibia and fibula in posterior view; (F) The distal portion of the right metatarsal III in medial view and metatarsal IV in anterior view; (G) the middle shaft of the left tibia and fibula in anterior view; (H) The middle shaft of the left metatarsals in anterior view. ft the fourth trochanter; ift iliofibularis tubercle; mt metatarsal.


Etymology: The generic name is derived from Asia, and the suffix ‘tyrannus’ is derived from the Latin word for ‘king’ or ‘tyrant’, to emphasize that this is the new tyrannosaur collected in the continent of Asia. The specific name honors Dr. Xing Xu (Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences), a distinguished dinosaurologist who contributed greatly to the study of dinosaurs from China, including the research of several tyrannosaurs: GuanlongDilong, and Yutyrannus. Dr. Xing Xu has also been a great supporter of the paleontological research and science popularization work of the Zhejiang Museum of Natural History.



Wenjie Zheng, Xingsheng Jin, Junfang Xie and Tianming Du. 2024. The first deep-snouted tyrannosaur from Upper Cretaceous Ganzhou City of southeastern China. Scientific Reports. 14,  16276. DOI:  doi.org/10.1038/s41598-024-66278-5