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Showing posts with label Dinosaur. Show all posts
Showing posts with label Dinosaur. Show all posts

Thursday, January 2, 2025

[PaleoOrnithology • 2025] Shuilingornis angelai • A New gansuid bird (Avialae: Euornithes) from the Lower Cretaceous (Aptian) Jiufotang Formation of Jianchang, western Liaoning, China

 

  Shuilingornis angelai
Wang, Cau, Wang, Kundrát, Zhang, Liu & Chiappe, 2025


Abstract
The study of the Cretaceous birds closest to the living euornithine species has mainly focused on the evolutionary patterns leading to the modern group. Yet, the morphological and ecological diversity of the euornithine branches not directly ancestral to the crown-group is probably underestimated. A new euornithine bird, Shuilingornis angelai gen. et sp. nov., is erected based on a nearly complete skeletal material from the Early Cretaceous (Aptian) Jehol Biota in western Liaoning, China. The new taxon is similar to the penecontemporary gansuids, yet it differs in the smaller body size and in the retention of plesiomorphic features widespread among non-gansuid euornithines. The osteohistological analysis indicates that Shuilingornis gen. nov. represents an early adult stage at the time of death. The phylogenetic analysis robustly supports the referral of Shuilingornis gen. nov. to Gansuidae. Except for the controversial Hollanda, the gansuids have been uncovered from four Aptian basins deposited under similar paleoclimatic conditions. Gansuid success in the middle part of the Cretaceous demonstrates that the exploration of semi-aquatic ecologies was a consistent euornithine pattern which preceded the later ornithurine radiation.


  Photo (A) and line drawing (B) of skull of  Shuilingornis angelai gen. et sp. nov (LY2022JZ3002).
 Abbreviations: an, angular; ar, articula; cv, cervical vertebrae; de, dentary; det, dentary teeth; fr, frontal; ju, jugal; la, lacrimal; ma, maxilla; mat, maxillary teeth; na, nasal; pa, parietal; po, postorbital; prd, predentary; prm, premaxilla; qj, quadjugal; qu, quadrate. 
Scale bar = 2 cm.

 Holotype of Shuilingornis angelai gen. et sp. nov. (LY2022JZ3002).
 Abbreviations: ca, carpals; ce, cervical vertebrae; fu, furcula; fv, fused vertebrae il, ilium; lfe, left femur; lfi, left fibula; lhu, left humerus; lra, left radius; lsc, left scapula; ltm, left tarsometatarsus; lul, left ulna; mc, metacarpals; md, manual digits; pu, pubis; rco, right coracoid; rfi, right fibula; rti, right tibiotarsus; rtm, right tarsometatarsus; sk, skull; st, sternum; Ⅰ, Ⅱ, Ⅲ, Ⅳ, pedal digit Ⅰ, Ⅱ, Ⅲ, Ⅳ. 
Scale bar = 2 cm.

Avialae Gauthier, 1986
Pygostylia Chiappe, 2002
Euornithes Sereno, 1998
Gansuidae Hou and Liu, 1984

Definition (new). The most inclusive clade containing Gansus yumenensis but not Hesperornis regalis, Hongshanornis longicresta, Patagopteryx deferrariisi, Songlingornis linghensis, Vultur gryphus or Yanornis martini.
Included taxa. Based on the result of our phylogenetic analysis, Gansuidae includes the genera Changzuiornis, Gansus, Khinganornis, Iteravis, and Shuilingornis gen. nov. Although supported by the phylogenetic analysis, the placement in this clade of the fragmentary Hollanda from the Upper Cretaceous of Mongolia (Bell et al., 2010) is considered as tentative.

Shuilingornis angelai gen. et sp. nov.

Holotype. LY2022JZ3002, a nearly complete and articulated skeleton preserved in a single slab (Fig. 2) and housed at Shandong Laiyang Cretaceous National Geological Park.

Locality and horizon. Lamadong locality, Jianchang County, Huludao City, Liaoning Province, China; Jiufotang Formation, Lower Cretaceous (Aptian) (Yu et al., 2021).

Diagnosis. Small euornithine bird with the unique combination of characteristics that can be distinguished from other Mesozoic birds: acuminate edentulous premaxilla longer than preantorbital ramus of maxilla; nasal with large subnarial process; procumbent maxillary teeth restricted to rostral end of bone which are much larger than the underlying dentary teeth (autapomorphy); humerus with robust shaft and elongate and gently curved deltopectoral crest; gracile alular digit less than half radius shaft width; large “U-shaped” furcula contacts the triangular apex of sternum; laterodistal end of coracoid does not define a distinct process, describing an acuminate 45° corner; manual phalangeal formula 2-3-2, with first phalanx of minor digit more than four times longer than the second phalanx.

Etymology. The genus name is composed of Chinese “Shuiling” (“pretty and vivid”) and Greek “ornis” (bird). The species name honors the Italian journalist and science writer Piero Angela (1928–2022) for his extraordinary contribution to the popularization of scientific knowledge and the promotion of rational thinking.


Xuri Wang, Andrea Cau, Yinuo Wang, Martin Kundrát, Guili Zhang, Yichuan Liu and Luis M. Chiappe. 2025. A New gansuid bird (Avialae, Euornithes) from the Lower Cretaceous (Aptian) Jiufotang Formation of Jianchang, western Liaoning, China. Cretaceous Research.  106014; In Press. DOI: doi.org/10.1016/j.cretres.2024.106014 


Monday, December 16, 2024

[Paleontology • 2024] Lishulong wangi • The largest sauropodomorph skull from the Lower Jurassic Lufeng Formation of China


 Lishulong wangi  
 
Q.-N. Zhang​, Jia, Wang, Y.-G. Zhang & You,. 2024 
 
The Lower Jurassic Lufeng Formation of China has long been recognized for its diverse early-diverging sauropodomorph dinosaurs, with eight genera and ten species, representing more than half the Laurasian records. In this paper, we describe a new genus and species of non-sauropodan sauropodomorph, Lishulong wangi gen. et sp. nov., from Yunnan Province in southwestern China. This new taxon is represented by a partial skeleton including the skull and nine articulated cervical vertebrae, which differs from other Lufeng forms in both cranial and cervical characteristics. It bears several autapomorphies of the nasal process, the maxillary neurovascular foramen, and the cervical neural spine. Phylogenetic analysis reveals that Lishulong is an early-diverging member of the Sauropodiformes, and the sister-taxon of Yunnanosaurus. Elucidating the novel osteology of Lishulong, it possessed the largest sauropodomorph cranial material currently identified from the Lufeng Formation, not only enriches the diversity of the Lufeng dinosaur assemblage, but also enhances our understanding of the character evolution in early-diverging sauropodiforms. Furthermore, information about paleobiogeographic distributions indicates that Early Jurassic sauropodomorphs, especially Chinese taxa, have maintained multiple dispersions and exchanges within Pangaea.



the cranium of Lishulong wangi gen. et sp. nov. 
 Photograph (A) and interpretative line drawing (B), 
in right lateral view and left lateral view.

Systematic Paleontology
Dinosauria Owen, 1842
Saurischia Seeley, 1888

Sauropodomorpha von Huene, 1932 (sensu Sereno, 2007)
Massopoda Yates, 2007
Sauropodiformes Sereno, 2007 (sensu McPhee et al., 2014)

Lishulong wangi gen. et sp. nov.

Holotype: LFGT-ZLJ0011. An associated partial skeleton that includes the cranium and mandible, and nine cervical vertebrae (axis and C3–C10)

Differential diagnosis: A large non-sauropodan sauropodiform dinosaur with the following unique combination of character states (autapomorphies are indicated by an asterisk): width of the anteroventral process of nasal at its base less than that of its anterodorsal process*; size of the neurovascular foramen at the posterior end of the lateral maxillary row not larger than the others*; shape of the supraoccipital is semilunate and wider than high in posterior view; height to length ratio of the dentary greater than 0.2; lingual concavities of the teeth present; lateral expansion at the anterior region of the dorsal surface of the cervical neural spines*.


Type locality and horizon: The specimen was discovered near the Jiudu Village in Konglongshan Town (formerly named Chuanjie Township), Lufeng County, Yunnan Province, China; and the upper-middle part of the Shawan Member of the Lufeng Formation (Fang et al., 2000), Lower Jurassic. Magnetostratigraphic analyses (Cheng et al., 2004; Huang et al., 2005) revealed the age to be Early Jurassic (late Sinemurian–Toarcian).

Etymology: The generic name is from ‘Lishu’ (chestnut tree in Chinese spelling), the name of the locality where the specimen was found, and ‘long’ refers to a dragon (in Chinese spelling); this specific epithet is in honor of Mr. Zheng-Ju Wang, for his great contributions to the early discoveries of vertebrate fossils from Lufeng.


Qian-Nan Zhang​, Lei Jia, Tao Wang, Yu-Guang Zhang and Hai-Lu You​. 2024. The largest sauropodomorph skull from the Lower Jurassic Lufeng Formation of China. PeerJ. 12:e18629 DOI: doi.org/10.7717/peerj.18629 


Sunday, December 15, 2024

[Paleontology • 2024] Body Size and Evolutionary Rate Analyses reveal Complex Evolutionary History of Alvarezsauria

 

1, Bonapartenykus; 2, Patagonykus; 3, Alvarezsaurus;
4, Alnashetri; 5, Albertonykus; 6, Heptasteornis;
7, Dzharaonyx; 8, Linhenykus; 12, Bannykus

in Meso, Pol, Chiappe, Qin, Díaz-Martínez, ... et Pittman. 2024. 
Artwork by Abel G. Montes.

Abstract
Some of the smallest examples of dinosaurian body size are from alvarezsaurians, an enigmatic group of maniraptoran coelurosaurians with a peculiar combination of anatomical features unique among theropods. Despite the large number of alvarezsaurian species described worldwide and the increased understanding this has provided, the body-size macroevolution of alvarezsaurians has received little attention. Here we reconstruct and analyse directional trends of alvarezsaurian body-size evolution through an integrated analysis of body mass, ontogenetic age, and morphological rate data enabled by a comprehensively revised phylogeny. Our analyses identify four periods of high morphological rate evolution (Bathonian–Callovian, Hauterivian–early Berriasian, early Cenomanian, and late Cenomanian–Turonian) that we link to the key effects of animal body-size changes for the first time, including morphological novelty, structural reduction and simplification, elevated homoplasy, and behavioral changes associated with miniaturization. In doing so, this study provides a holistic example of miniaturization in a Mesozoic vertebrate group that offers a framework for other detailed studies of animal body-size evolution, including in more disparate groups.

Relative body sizes of Alvarezsauria calibrated with the geological age of known alvarezsaurian taxa and showing their continental distribution. Silhouettes calibrated with body mass. The range of blues represents the forms of the Upper Jurassic, the range of pink represents the forms of the Lower Cretaceous, the range of reds represents the forms of the Upper Cretaceous of Patagonia, and the range of greens represents the Parvicursorinae.



Life reconstruction of 12 alvarezsaurians that illustrate body-size change in the clade.
1, Bonapartenykus; 2, Patagonykus; 3, Alvarezsaurus; 4, Alnashetri; 5, Albertonykus; 6, Heptasteornis; 7, Dzharaonyx; 8, Linhenykus; 9, Haplocheirus; 10, Shishugounykus; 11, Kol; 12, Bannykus.
 Artwork by Abel G. Montes.


Jorge Gustavo Meso, Diego Pol, Luis Chiappe, Zichuan Qin, Ignacio Díaz-Martínez, Federico Gianechini, Sebastián Apesteguía, Peter J. Makovicky and Michael Pittman. 2024. Body Size and Evolutionary Rate Analyses reveal Complex Evolutionary History of Alvarezsauria. Cladistics. Early View. DOI: doi.org/10.1111/cla.12600

Monday, December 9, 2024

[Paleontology • 2024] Theropod Dinosaur Diversity of the lower English Wealden: Analysis of a tooth-based fauna from the Wadhurst Clay Formation (Lower Cretaceous: Valanginian) via phylogenetic, discriminant and machine learning methods


An Early Cretaceous floodplain in southeastern England, 135 million years ago:
a spinosaur takes over the carcass of an ornithopod, much to the annoyance of the smaller tyrannosaurs (left) and dromaeosaurids.


in Barker, Handford, Naish, Wills, Hendrickx, ... et Gostling, 2024. 
artwork by Anthony Hutchings.
 
Abstract
The Lower Cretaceous Wealden Supergroup of southern England yields a diverse assemblage of theropod dinosaurs, its taxa being represented by fragments in addition to some of the most informative associated skeletons of the European Mesozoic. Spinosaurids, neovenatorid allosauroids, tyrannosauroids and dromaeosaurids are among reported Wealden Supergroup clades. However, the majority of relevant specimens are from the Barremian Upper Weald Clay and Wessex formations, and theropod diversity in the older Berriasian–Valanginian Hastings Group has remained poorly known, the fragmentary specimens reported thus far remaining enigmatic both in terms of phylogenetic affinities and sometimes provenance. A better understanding would be welcome given the paucity of Berriasian–Valanginian dinosaurs worldwide. Here, we describe an assemblage of Hastings Group theropod teeth from the Valanginian Wadhurst Clay Formation, mostly collected from the Ashdown Brickworks locality near Bexhill, East Sussex. These teeth were assessed using phylogenetic, discriminant and machine learning analyses and were found to include members of Spinosauridae, Tyrannosauroidea and Dromaeosauridae, in addition to others that remain of uncertain affinity within Coelurosauria. The taxa appear distinct from those already known from Wealden Supergroup strata: the spinosaurid cannot be referred to Baryonyx or the tyrannosauroid to Eotyrannus, for example, but we have not named new taxa at this time. Combined with other findings in the Wadhurst Clay Formation, our study indicates that Valanginian theropod diversity was comparable to that of younger Wealden Supergroup units, implying that the ‘characteristic’ theropod components of Wealden faunas were established early in the deposition of this famous geological succession.

Keywords: theropod, Wealden Supergroup, phylogenetics, machine learning, dinosaur, Cretaceous

Theropod teeth from the Wadhurst Clay Formation.
A, BEXHM 1995.485 (morphotype I). B, BEXHM 2002.50.123 (morphotype II). C, BEXHM 2002.50.124 (morphotype III). D, BEXHM 2005.29 (morphotype IV). E, NHMUK PV R37630 (morphotype V).
 A, C–E, lingual; B, labial view. Scale bar represents 10 mm.

Schematic representation of the theropod diversity throughout the Wealden Supergroup, with specimens from the Wealden Group (Wessex sub-basin) and the Hastings and Weald Clay groups (Weald sub-basin).

An Early Cretaceous floodplain in southeastern England, 135 million years ago: a spinosaur (centre) takes over the carcass of an ornithopod, much to the annoyance of the smaller tyrannosaurs (left) and dromaeosaurids (bottom right).
artwork by Anthony Hutchings.


Chris T. Barker, Lucy Handford, Darren Naish, Simon Wills, Christophe Hendrickx, Phil Hadland, Dave Brockhurst and Neil J. Gostling. 2024. Theropod Dinosaur Diversity of the lower English Wealden: Analysis of a tooth-based fauna from the Wadhurst Clay Formation (Lower Cretaceous: Valanginian) via phylogenetic, discriminant and machine learning methods. Papers in Palaeontology. DOI: doi.org/10.1002/spp2.1604


Sunday, December 1, 2024

[Paleontology • 2024] Digestive Contents and Food Webs Record the advent of Dinosaur Supremacy

  



in Qvarnström, Wernström, Wawrzyniak, Barbacka, ... et Niedźwiedzki, 2024. 


Abstract
The early radiation of dinosaurs remains a complex and poorly understood evolutionary event. Here we use hundreds of fossils with direct evidence of feeding to compare trophic dynamics across five vertebrate assemblages that record this event in the Triassic–Jurassic succession of the Polish Basin (central Europe). Bromalites, fossil digestive products, increase in size and diversity across the interval, indicating the emergence of larger dinosaur faunas with new feeding patterns. Well-preserved food residues and bromalite-taxon associations enable broad inferences of trophic interactions. Our results, integrated with climate and plant data, indicate a stepwise increase of dinosaur diversity and ecospace occupancy in the area. This involved (1) a replacement of non-dinosaur guild members by opportunistic and omnivorous dinosaur precursors, followed by (2) the emergence of insect and fish-eating theropods and small omnivorous dinosaurs. Climate change in the latest Triassic resulted in substantial vegetation changes that paved the way for ((3) and (4)) an expansion of herbivore ecospace and the replacement of pseudosuchian and therapsid herbivores by large sauropodomorphs and early ornithischians that ingested food of a broader range, even including burnt plants. Finally, (5) theropods rapidly evolved and developed enormous sizes in response to the appearance of the new herbivore guild. We suggest that the processes shown by the Polish data may explain global patterns, shedding new light on the environmentally governed emergence of dinosaur dominance and gigantism that endured until the end-Cretaceous mass extinction.



 
Martin Qvarnström, Joel Vikberg Wernström, Zuzanna Wawrzyniak, Maria Barbacka, Grzegorz Pacyna, Artur Górecki, Jadwiga Ziaja, Agata Jarzynka, Krzysztof Owocki, Tomasz Sulej, Leszek Marynowski, Grzegorz Pieńkowski, Per E. Ahlberg and Grzegorz Niedźwiedzki. 2024. Digestive Contents and Food Webs Record the advent of Dinosaur Supremacy. Nature. DOI: doi.org/10.1038/s41586-024-08265-4

Monday, November 11, 2024

[Paleontology • 2024] Huaxiazhoulong shouwen • A New ankylosaurid Dinosaur (Ankylosauria: Ankylosauridae) from the Upper Cretaceous of Jiangxi Province, southern China


Huaxiazhoulong shouwen 
Zhu, Wu, You, Jia, Chen, Yao, Zheng & Xu, 2024 
 
artwork by YE Jianhao

ABSTRACT
Huaxiazhoulong shouwen gen. et sp. nov. is a new ankylosaurid recovered from the Upper Cretaceous Tangbian Formation of Jiangxi Province, southern China. Huaxiazhoulong shouwen can be diagnosed on the basis of three autapomorphies (the middle shaft and distal end of the ischium are expanded; the ratio of width of distal end to minimum shaft width is greater than 3 in humerus, the maximum length of femur to humerus length ratio is about 1.45) and a unique combination of characters (the centra of anterior caudal vertebrae in anterior view is heart-shaped; the dorsal surface of scapula is straight; the scapulocoracoid has a large medial brace; the humeral head and deltopectoral crest are separated by a distinct notch anteriorly). The phylogenetic analysis shows that Huaxiazhoulong shouwen is an early member of Ankylosauridae.

KEYWORDS: Ankylosauria, Upper Cretaceous, Tangbian Formation, Jiangxi Province, Huaxiazhoulong shouwen


  
Huaxiazhoulong shouwen gen. et sp. nov.



Ziheng Zhu, Jie Wu, Yue You, Yingli Jia, Chujiao Chen, Xi Yao, Wenjie Zheng and Xing Xu. 2024. A New ankylosaurid Dinosaur from the Upper Cretaceous of Jiangxi Province, southern China. Historical Biology: An International Journal of PaleobiologyDOI: doi.org/10.1080/08912963.2024.2417208  

Wednesday, November 6, 2024

[Paleontology • 2024] Extremely rapid, yet noncatastrophic, Preservation of the Flattened-feathered and 3D Dinosaurs of the Early Cretaceous of China

  

 Extremely rapid preservation of the flattened-feathered and 3D Dinosaurs of the Early Cretaceous, Yixian Formation in China

in MacLennan, Sha, Olsen, Kinney, Chang, Fang, Liu, Slibeck, Chen et Schoene, 2024.

Significance: 
Traditionally, the spectacular preservation of fossils of feathered dinosaurs and early birds and other animals found in sedimentary strata of the Yixian Formation in northeast China has been attributed to Pompeii-like volcanic catastrophes. We provide high-resolution geochronology and sedimentological analysis challenging this model and show that these strata instead record normal life and death processes preserved in a succession of depositional environments that span less than 100 thousand years.

Abstract
Northeast China’s Early Cretaceous Yixian Formation preserves spectacular fossils that have proved extraordinarily important in testing evolutionary hypotheses involving the origin of birds and the distribution of feathers among nonavian dinosaurs. These fossils occur either flattened with soft tissue preservation (including feathers and color) in laminated lacustrine strata or as three-dimensional (3D) skeletons in “life-like” postures in more massive deposits. The relationships of these deposits to each other, their absolute ages, and the origin of the extraordinary fossil preservation have been vigorously debated for nearly a half century, with the prevailing view being that preservation was linked to violent volcanic eruptions or lahars, similar to processes that preserved human remains at Pompeii. We present high-precision zircon U-Pb geochronology from cores and outcrops, demonstrating that Yixian Formation accumulation rates are more than an order of magnitude higher than usually estimated. Additionally, we provide zircon provenance and sedimentological data from 3D dinosaur fossils, which imply that their death and burial occurred in collapsed burrows, rather than via a catastrophic volcanogenic mechanism. In the studied area, the three principal fossil-rich intervals of the Yixian occur as a cyclic sequence that correspond to periods of high precipitation. Using Bayesian–Markov Chain Monte Carlo approaches, we constrain the total duration of the sequence to less than ~93,000 y and suggest that climatic precession paced the expression of these cyclic sediments. Rather than representing multiple, Pompeii-like catastrophes, the Yixian Formation is instead a brief snapshot of normal life and death in an Early Cretaceous continental community.

Two perfectly articulated skeletons of the sheep-size dinosaur Psittacosaurus, found in China's Yixian Formation. New research suggests they died in burrow collapses, not via volcanism, as previously thought.
by Jun Liu, IVPP, Chinese Academy of Sciences

Artist's rendition of a Psittacosaurus dinosaur with babies being hunted by Repenomamus, a mammal. One fossil assemblage from the Yixian Formation preserved the remains of these species in mortal combat, frozen in mid-action. The dinosaur here is shown with bristly proto-feathers on its tail.
artwork by Alex Boersma


 Scott A. MacLennan, Jingeng Sha, Paul E. Olsen, Sean T. Kinney, Clara Chang, Yanan Fang, Jun Liu, Bennett B. Slibeck, Elaine Chen, and Blair Schoene. 2024. Extremely rapid, yet noncatastrophic, Preservation of the Flattened-feathered and 3D Dinosaurs of the Early Cretaceous of China. PNAS. 121 (47) e2322875121. DOI: doi.org/10.1073/pnas.2322875121

Thursday, October 17, 2024

[Paleontology • 2025] Emiliasaura alessandrii • First Valanginian (Early Cretaceous) Ornithopod (Ornithischia: Ornithopoda) from Patagonia

  

Emiliasaura alessandrii
R.A. Coria, Cerda, Escaso, Baiano, Bellardini, Braun, L.M. Coria, Gutierrez, Pino, Windholz, Currie & Ortega, 2024 


Highlights: 
• A new taxon of the dinosaur clade Ornithopoda, Emiliasaura alessandri, is described.
Emiliasaura is the first recognized South American rhabdodontoid ornithopod taxon.
Emiliasaura represents the earliest Patagonian Cretaceous ornithischian dinosaur.

Abstract
Here we describe a new ornithopod speciesEmiliasaura alessandrii gen. et sp. nov. from Valanginian rocks (Early Cretaceous) of northwestern Patagonia. This new taxon exhibits affinities with the Rhabdodontomorpha and is primarily represented by two specimens of mid-sized ornithopods collected from different sites and stratigraphical levels of the Mulichinco Formation. The holotype specimen MLL-Pv-001 includes the coracoid, the proximal end of a scapula, a humerus and a complete right hind limb, whereas the paratype specimen MLL-Pv-006 preserves vertebral elements, haemal arches, an incomplete pelvis, and nearly complete hind limbs. The new taxon has an anteroposteriorly elongate ilium with a sigmoidal dorsal border and broad brevis shelf, a femur shaft with an extensive, proximally positioned fourth trochanter, and a second pedal digit with a short, robust, blunt ungual phalanx similar to those in Ankylopollexia ornithopods. The new ornithopod taxon formed part of a diverse dinosaur association from the Mulichinco Fm that includes dicraeosaurid sauropods and carcharodontosaurid theropods, and represents the first South American record of a rhabdodontoid, and the oldest and most primitive representative of this clade.
 


Emiliasaura alessandrii gen. et sp. nov. 


R.A. Coria, I.A. Cerda, F. Escaso, M.A. Baiano, F. Bellardini, A. Braun, L.M. Coria, J.M. Gutierrez, D. Pino, G.J. Windholz, P.J. Currie and F. Ortega. 2024. First Valanginian (Early Cretaceous) Ornithopod (Dinosauria, Ornithischia) from Patagonia. Cretaceous Research. 106027. DOI: doi.org/10.1016/j.cretres.2024.106027

Wednesday, October 9, 2024

[Paleontology • 2024] Ardetosaurus viator • A New diplodocine Sauropod from the Morrison Formation, Wyoming, USA


 Ardetosaurus viator
van der Linden, Tschopp, Sookias, Wallaard, Holwerda & Schulp, 2024

 DOI: 10.26879/1380 
  Life reconstruction by Ole Zant. x.com/TheBioBob

ABSTRACT
The Morrison Formation of the western United States is well-known for its high diversity of sauropod dinosaurs. The Howe-Stephens Quarry in northern Wyoming is one of several quarries which has yielded several associated to completely articulated dinosaur specimens, among which a semi-articulated diplodocid specimen, MAB011899, which was excavated in 1993. This diplodocid specimen is represented by posterior cervical, dorsal, sacral, and anterior caudal vertebrae, multiple thoracic ribs, two chevrons, a left coracoid, a left ilium, both pubes and ischia, a left femur, a left tibia, and a left fibula. Through comparative anatomy, we interpret this specimen as a new species of diplodocine sauropod, Ardetosaurus viator gen. et sp. nov. Unambiguous autapomorphies include paired accessory laminae in the spinoprezygapophyseal fossae of posterior cervical and anterior dorsal vertebrae, bifurcating anterior centrodiapophyseal laminae in the anterior dorsal vertebrae, fossae present in the centropostzygapophyseal laminae of the second dorsal vertebra, a low vertebral height/centrum length ratio of the posterior dorsal vertebrae and reduced to absent centroprezygapophyseal laminae in the anterior caudal vertebrae. Local autapomorphic features include single centroprezygapophyseal laminae in the posterior cervical vertebrae and a highly elliptical cross-section of the femoral midshaft. Ardetosaurus viator is the first skeletally mature sauropod specimen described from the Howe-Stephens Quarry. This specimen provides insight into serial variation of vertebral laminae and laminar transitions. Finally, the peculiar morphology of the—often not preserved—first chevron is described in detail, and its possible use in studying sexual dimorphism in sauropods is discussed.

Keywords: sauropod; new genus; new species; Morrison Formation; Diplodocinae; Wyoming




  Skeletal reconstruction of  Ardetosaurus viator MAB011899. Skeletal reconstruction indicating preserved bones (white), excavated bones but subsequently lost (light gray) and not preserved (dark gray). Unknown elements are based on other diplodocines.
Scale bar equals 1 m. Reconstruction by Ole Zant.

SYSTEMATIC PALEONTOLOGY
DINOSAURIA Owen, 1842
SAUROPODA Marsh, 1878
EUSAUROPODA Upchurch, 1995
NEOSAUROPODA Bonaparte, 1986

DIPLODOCOIDEA Marsh, 1884
FLAGELLICAUDATA Harris and Dodson, 2004

DIPLODOCIDAE Marsh, 1884
DIPLODOCINAE Marsh, 1884

ARDETOSAURUS gen. nov.
 
Ardetosaurus viator gen. et sp. nov.
 
Holotype. MAB011899: two cervical vertebrae, 10 dorsal vertebrae, sacrum, five caudal vertebrae, eight dorsal ribs, two chevrons, a left coracoid, a left ilium, both pubes, both ischia, a left femur, a left tibia, and a partial left fibula.

Diagnosis. Ardetosaurus viator is diagnosed by the combination of the following autapomorphies: 1) the presence of distinct, paired accessory laminae in the spinoprezygapophyseal fossae (SPRF) in the posterior cervical and anterior dorsal vertebrae, 2) anteroventrally bifurcating anterior centrodiapophyseal laminae (ACDLs) in the anterior dorsal vertebrae, 3) the presence of centropostzygapophyseal lamina fossae (CPOL-f) in the second dorsal vertebra, 4) a vertebral height/centrum length ratio of <2.5 of the posterior dorsal vertebrae, and 5) reduced or absent centroprezygapophyseal laminae (CPRLs) in the anterior-most caudal vertebrae. Ardetosaurus viator differs from all other diplodocines by having unbifurcated CPRLs in the posterior cervical vertebrae and a highly elliptical femoral cross-section. Ardetosaurus viator differs from Amphicoelias Cope, 1878, in lacking the rounded, lateral projections of the neural spine tip and the thin neural spine base in the dorsal vertebrae; from Barosaurus Marsh, 1890, by having tall cervical neural spines, single midline keels, narrower prezygapophyseal rami in the cervical vertebrae, ten dorsal vertebrae, the presence of ...


Etymology. ‘Ardeto’ is an inflection of Latin ārdēre, meaning ‘to burn.’ It refers to the history of some of the elements, which were either fully destroyed in a fire, or still show burn scars from the fire. ‘saurus, ’ Latinized form of the Greek σαῦρος (saúros), meaning lizard or reptile. ‘viator’ is Latin for traveler, referring to the journey of the specimen from the USA, via Switzerland and Germany, to the Netherlands.

Locality and horizon. Ardetosaurus viator comes from the Howe-Stephens Quarry of northern Wyoming, USA. The quarry is dated, based on magnetostratigraphy and correlation with other sections in the Morrison basin (Maidment and Muxworthy, 2019; Maidment, personal communication, 2022) at 150.44 to 149.21 million years old, placing it in the Kimmeridgian Stage of the Upper Jurassic.


 Quarry map of Ardetosaurus viator MAB011899. Excavation map of the Howe-Stephens Quarry, indicating the major finds from 1992-2000. Individual dinosaurs are color coded, and MAB011899 is coded with dark blue, and named ‘Diplodocus Brösmeli’ herein. The red crosses indicate the missing/lost cervical vertebrae. Note the relatively similar color for ‘Brösmeli’ and ‘David’ (SMA 0086), but their significant separation in the quarry.
 Figure is courtesy of the SMA. Quarry sections equal 1 by 0.5 m.


  Life reconstruction of  Ardetosaurus viator MAB011899.
Illustration by Ole Zant.

The skeleton of Brösmeli is on display in the Oertijdmuseum.


Tom T.P. van der Linden, Emanuel Tschopp, Roland B. Sookias, Jonathan J.W. Wallaard, Femke M. Holwerda, and Anne S. Schulp. 2024. A New diplodocine Sauropod from the Morrison Formation, Wyoming, USA. Palaeontologia Electronica. 27(3): a50. DOI: doi.org/10.26879/1380
palaeo-electronica.org/content/2024/5327-new-diplodocine-sauropod

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

Thursday, September 12, 2024

[PaleoOrnithology • 2024] Direct Evidence of Frugivory in the Mesozoic Bird Longipteryx contradicts Morphological Proxies for Diet


 Longipteryx, a fossil bird with unusually strong teeth right at the tip of its beak.

in O’Connor, Clark, Herrera, Yang, Wang, Zheng, Hu et Zhou. 2024. 
Illustration by Ville Sinkkonen.

Highlights: 
• Unusual enantiornithine Longipteryx with an elongate rostrum predicted to be a faunivore
• Direct evidence indicates Longipteryx was a frugivore, eating gymnosperm “fruits”
• Like crown birds, morphological proxies fail to predict diet in early birds

Summary: 
Diet is one of the most important aspects of an animal’s ecology, as it reflects direct interactions with other organisms and shapes morphology, behavior, and other life history traits. Modern birds (Neornithes) have a highly efficient and phenotypically plastic digestive system, allowing them to utilize diverse trophic resources, and digestive function has been put forth as a factor in the selectivity of the end-Cretaceous mass extinction, in which only neornithine dinosaurs survived. Although diet is directly documented in several early-diverging avian lineages, only a single specimen preserves evidence of diet in Enantiornithes, the dominant group of terrestrial Cretaceous birds. Morphology-based predictions suggest enantiornithines were faunivores, although the absence of evidence contrasts with the high preservation potential and relatively longer gut-retention times of these diets. Longipteryx is an unusual Early Cretaceous enantiornithine with an elongate rostrum; distally restricted dentition; large, recurved, and crenulated teeth; and tooth enamel much thicker than other paravians. Statistical analysis of rostral length, body size, and tooth morphology predicts Longipteryx was primarily insectivorous. Contrasting with these results, two new specimens of Longipteryx preserve gymnosperm seeds within the abdominal cavity interpreted as ingesta. Like Jeholornis, their unmacerated preservation and the absence of gastroliths indicate frugivory. As in Neornithes, complex diets driven by the elevated energetic demands imposed by flight, secondary rostral functions, and phylogenetic influence impede the use of morphological proxies to predict diet in early-diverging avian lineages.

Keywords: trophics, gymnospermous disseminules, consumulites, stomach contents, Cretaceous, Enantiornithes, Aves/Avialae
 

 Longipteryx, a fossil bird with unusually strong teeth right at the tip of its beak.
Illustration by Ville Sinkkonen.

 
Jingmai O’Connor, Alexander Clark, Fabiany Herrera, Xin Yang, Xiaoli Wang, Xiaoting Zheng, Han Hu and Zhonghe Zhou. 2024. Direct Evidence of Frugivory in the Mesozoic Bird Longipteryx contradicts Morphological Proxies for Diet.  Current Biology.  DOI: doi.org/10.1016/j.cub.2024.08.012