Showing posts with label Saurischia. Show all posts
Showing posts with label Saurischia. Show all posts

Thursday, September 17, 2026

[Paleontology • 2026] Sauropod teeth from the Khorat Group of Thailand suggest the Faunal Replacement of Sauropod Dinosaurs across the Late Jurassic–Early Cretaceous


Sauropod diversity interpretation throughout the Jurassic–Cretaceous transition of Thailand based on dental evidence in
A, the Late Jurassic (Tithonian); B, the Early Cretaceous (late Valanginian to Barremian), C, the late Early Cretaceous (Aptian to Albian). 

in Chowchuvech, Manitkoon, Chanthasit et Ketwetsuriya. 2026. 
Illustrations by Pakorn Chotchaiyaporn x.com/Peak4651

ABSTRACT
Sauropod teeth are among the most abundant vertebrate fossils recovered from the Upper Jurassic to Lower Cretaceous Khorat Group of Thailand. However, their taxonomic and palaeoecological significance has not previously been examined in detail. This research presents the first comprehensive taxonomic identification of isolated sauropod teeth from several localities across the Khorat Plateau in Northeastern and Eastern Thailand. Based on morphological analyses, these teeth were assigned to four distinct morphotypes. Additionally, multi-quantitative analyses revealed affinities with four sauropod clades: Mamenchisauridae, Brachiosauridae, Somphospondyli, and Dicraeosauridae. The taxonomic framework recovered in this study is consistent with the broader sauropod fossil record of the Khorat Group and reveals a marked faunal shift across the Jurassic–Cretaceous of Thailand. Mamenchisaurids appeared during the Late Jurassic to the earliest Cretaceous, whereas neosauropods, such as titanosauriforms and diplodocoids, became more prevalent during the Early Cretaceous. These findings suggest new evidence for a major sauropod faunal replacement event, likely driven by ecological changes affecting herbivorous dinosaurs during this crucial timeframe of the Mesozoic.

KEYWORDS: Sauropoda, Mamenchisauridae, Brachiosauridae, Somphospondyli, Diplodocoidea


Sauropod diversity interpretation throughout the Jurassic–Cretaceous transition of Thailand based on dental evidence in A, the Late Jurassic (Tithonian); B, the Early Cretaceous (late Valanginian to Barremian), C, the late Early Cretaceous (Aptian to Albian).
 Illustrations by Pakorn Chotchaiyaporn.


 
Wongwech Chowchuvech, Sita Manitkoon, Phornphen Chanthasit and Chatchalerm Ketwetsuriya. 2026. Sauropod teeth from the Khorat Group of Thailand suggest the Faunal Replacement of Sauropod Dinosaurs across the Late Jurassic–Early Cretaceous. Historical Biology: An International Journal of Paleobiology. DOI: doi.org/10.1080/08912963.2026.2710631 [15 Sep 2026]



Wednesday, July 8, 2026

[Paleontology • 2026] Uragasaurus kalasinensis • A New mamenchisaurid Sauropod (Sauropoda: Mamenchisauridae) from the Lower Phu Kradung Formation, Upper Jurassic of northeastern Thailand


Uragasaurus kalasinensis
Nilpanapan, Manitkoon, Suteethorn & Lauprasert, 2026
 
อุรคาซอรัส กาฬสินธุ์เอนซิส  ||  DOI: doi.org/10.1038/s41598-026-49822-3
 Artwork by Pakorn Chotchaiyaporn (Jæsica ẞababi: x.com/Peak4651).

Abstract
Mamenchisauridae is a group of long-necked non-neosauropodan eusauropod dinosaurs that were abundant in East Asia during the Middle to Late Jurassic, but their diversity and geographic distribution outside China remain poorly documented. Here we describe Uragasaurus kalasinensis gen. et sp. nov., a new sauropod dinosaur from the Phu Kradung Formation of northeastern Thailand. The new taxon is based on a well-preserved anterior dorsal vertebra exhibiting a distinctive combination of characters, including a unique Y-shaped configuration formed by the intraprezygapophyseal and single intraprezygapophyseal laminae and a camellate internal pneumatic structure within the centrum revealed by computed tomography (CT). Phylogenetic analyses recover the new taxon as an early-diverging member of Mamenchisauridae. This discovery represents the first formally named mamenchisaurid from Thailand and expands the known geographic distribution of the clade in Southeast Asia. The occurrence of this taxon in the Lower part of the Phu Kradung Formation also contributes to understanding faunal succession within the unit, supports an Upper Jurassic age for the lower part of the formation, and improves understanding of sauropod diversity in Southeast Asia during the Jurassic-Cretaceous transition.

Keywords: Sauropoda, Mamenchisauridae, Upper Jurassic, Phu Kradung Formation, Northeastern Thailand

Holotype of Uragasaurus kalasinensis (PRC 460) and associated materials in the quarry map. PRC 460 Anterior dorsal vertebra in anterior view (a), KS 34-581 anterior dorsal neural arch in anterior view (b), KS 34-602a middle cervical vertebra in ventral view (c), KS 34-586 anterior dorsal neural arch in anterior view, attached by KS 34-588 fibula (d), KS 34-587 coracoid in lateral view (e), KS 34-602b right cervical rib in lateral view (f).

Uragasaurus kalasinensis gen. et sp. nov.
อุรคาซอรัส กาฬสินธุ์เอนซิส
 
Holotype: The isolated anterior dorsal vertebra PRC 460 has been housed at the Palaeontological Research and Education Centre (PRC), Mahasarakham University, Thailand. Following standard paleontological protocols, the vertebrae were mechanically prepared using pneumatic tools and fine brushes to remove the surrounding sediment matrix.
 
Locality: Phu Noi Locality, Kalasin Province, northeastern Thailand (16.93298° N, 103.72327° E).

Horizon: Lower part of the Phu Kradung Formation, Khorat Group.

Age: Latest Jurassic, based on regional stratigraphic correlations and the composition of the vertebrate assemblage; precise chronostratigraphic constraints remain uncertain.

Diagnosis: Uragasaurus kalasinensis gen. et sp. nov. is a mamenchisaurid sauropod diagnosed by the following unique combination of characters (autapomorphy is marked by *): (1) anterior dorsal vertebra with prominent, elongated teardrop-shaped pneumatic fossae on the distal portion of the transverse processes*; (2) intraprezygapophyseal laminae (tprl) meeting ventromedially to form a Y-shaped configuration in anterior view, incorporating a single vertical intraprezygapophyseal lamina (stprl); and (3) shallow, subtriangular pleurocoel lacking an internal septum.

Etymology: The genus name “Uraga” originates from the Sanskrit word उरग, meaning “snake” or “serpent”, referring to the distinguished long neck of the family. The term “saurus” is derived from the Greek word saûros, meaning lizard. The specific epithet refers to Kalasin Province, where the specimens are from.

Holotype of Uragasaurus kalasinensis (PRC 460) and associated materials in the quarry map. PRC 460 Anterior dorsal vertebra in anterior view (a), KS 34-581 anterior dorsal neural arch in anterior view (b), KS 34-602a middle cervical vertebra in ventral view (c), KS 34-586 anterior dorsal neural arch in anterior view, attached by KS 34-588 fibula (d), KS 34-587 coracoid in lateral view (e), KS 34-602b right cervical rib in lateral view (f).
Quarry map showing the spatial distribution of the holotype and associated materials from the Phu Noi Locality (g). PRC 460, representing the new taxon Uragasaurus kalasinensis, is indicated in red. Associated sauropod elements include KS 34-586, KS 34-587, KS 34-588, and KS 34-602a–b, highlighted in yellow, green, blue, purple, and pink, respectively. The inset shows a close-up of the excavation grid highlighting the relative positions of the holotype and nearby associated materials. Each grid square represents 0.75 × 0.75 m.

Life reconstruction of a herd of five individuals of Uragasaurus kalasinensis inhabiting a Late Jurassic forest in Thailand, accompanied by a pair of rhamphorhynchoid pterosaurs and a metriacanthosaurid theropod.
 Artwork by Pakorn Chotchaiyaporn (Jæsica ẞababi).


Apirut Nilpanapan, Sita Manitkoon, Varavudh Suteethorn and Komsorn Lauprasert. 2026. A New mamenchisaurid Sauropod from the Lower Phu Kradung Formation, Upper Jurassic of northeastern Thailand. Scientific Reports. 16: 21205. DOI: doi.org/10.1038/s41598-026-49822-3 [08 July 2026]


Thursday, July 2, 2026

[Paleontology • 2026] Zhengheornis buyu • Jurassic Avialan reveals stepwise Evolution of Bony Tail in Birds


Zhengheornis buyu
Wang, Tang, Deng, Dong, L. Xu, X. Xu, M. Lin,  Du, G. Lin, Chen, Zhang & Zhou, 2026 
 

Abstract
The evolutionary assembly of the flight-adapted bird body plan encompasses some of the most profound morphological changes in terrestrial vertebrate history. Beyond feathered wings, the short pygostyle-bearing tail has been pivotal to the clade’s ecological success. However, transition from the long bony tail to the short pygostyle-bearing tail remains a mystery, hindered by the scarcity of early branching avialans with transitional morphologies. Here, we report on a new avialan, Zhengheornis buyu, gen. et sp. nov., from the Upper Jurassic of southeastern China, suggesting that the vertebral reduction and shortening preceded pygostyle fusion in early avialan evolution, providing critical evidence for the stepwise evolution of the bird tail. Z. buyu is smaller than all known non-pygostylian paravians, expanding the species and body size diversity of stemward taxa.

Systematics
Theropoda Marsh, 1881  
Maniraptora Gauthier, 1986  
Avialae Gauthier, 1986 


Zhengheornis buyu gen. et sp. nov. 

Etymology: Zhenghe” (Mandarin), referring to Zhenghe Country, where the holotype specimen was found; “ornis,” bird (Greek); “buyu,” unexpected (Mandarin), from the ancient Chinese book Guoyu, referring to the unique tail and pelvic morphologies preserved in this species. 

Holotype: Institute of Vertebrate Paleontology and Paleoanthropology (IVPP) V34168, an articulated and partially complete skeleton (most limb bones are preserved as molds) with feathers preserved on a slab and counter slab (Fig. 1, figs. S1 and S2, and table S1). 

Locality and horizon: Near Yangyuan Village, Zhenghe Country, Nanping City, Fujian Province; Upper Jurassic, Nanyuan Formation [Tithonian stage]. 

Diagnosis: IVPP V34168 is distinguishable from all other paravians in the following combination of characters (*denotes probable autapomorphy): short tail comprising 15 vertebrae that is shorter than the hindlimb (combined length of femur, tibia, and metatarsal III)*; middle and posterior caudal vertebrae less elongate (opposite to the condition in other long tailed avialans); final two caudal vertebrae box-like*; manual phalanx III-1 shorter than III-2, opposite to the condition in Archaeopteryx and Fujianvenator [the three manual digits of maniraptorans are here identified as I, II, and III, as in (Tamura, et al. 2011)]; manual phalanx III-3 50% longer than III-2 (the length ratio greater than 2 in Anchiornis and Archaeopteryx); slender ischium that has a knob-like, distally located obturator process and lacks the posterior process*; short fibula that terminates far proximal to the ankle; metatarsal I that articulates at the distal third of metatarsal II; metatarsal II that ends far proximal to metatarsal III trochlea; short hallux with an ungual that is smaller than that of other pedal digits; and robust digit II that has the longest non-ungual (II-2) and ungual pedal phalanges.


 
Min Wang, Jianrong Tang, Ke Deng, Liping Dong, Liming Xu, Xing Xu, Min Lin, Honggang Du, Ganmin Lin, Runsheng Chen, Chi Zhang and Zhonghe Zhou. 2026. Jurassic Avialan reveals stepwise Evolution of Bony Tail in Birds. Science Advances. 12(27); DOI: doi.org/10.1126/sciadv.aeb5202 [1 Jul 2026]

Friday, June 5, 2026

[Paleontology • 2026] Jian changmaensis • First non-Avian Theropod (Dromaeosauridae: Microraptorinae) from the Bird-bearing Lower Cretaceous Xiagou Formation of the Changma Basin, Gansu Province, Northwestern China

 

Jian changmaensis 
Zhou, Lamanna, Poust, Li, You & O’Connor, 2026
attacks the early bird Gansus yumenensis 
  
 illustration by Lewis LaRosa  x.com/LewisLaRosa, colorized by Jão Canola.

ABSTRACT
Lacustrine sediments of the Lower Cretaceous (lower Aptian) Xiagou Formation exposed near the village of Changma in the Changma Basin of northwestern Gansu Province, China have yielded more than 100 avian partial skeletons, many of which also preserve remnants of soft tissues such as feathers and skin. Collectively, these fossils characterize a rich avifauna dominated by the crownward ornithuromorph Gansus yumenensis Hou and Liu, 1984. Despite this wealth of Early Cretaceous bird material, no skeletal remains of other dinosaurs have been described from Changma to date. Here we report the first non-avian dinosaur body fossil from the Xiagou Formation of the Changma Basin. Consisting of an articulated left pectoral girdle and forelimb lacking the carpus and manus, the specimen pertains to a new dromaeosaurid theropod taxon, Jian changmaensis, gen. et sp. nov. Phylogenetic analysis recovers Jian within Microraptorinae, expanding the definitive fossil record of this clade to include northwestern China. The new Changma microraptorine constitutes an additional similarity between the theropod faunas of the Xiagou Formation of the Changma Basin and penecontemporaneous strata of the Jehol Group of northeastern China. In particular, the Changma theropod assemblage closely resembles that of the Sihedang locality of the Jehol Group in that both include representatives of Microraptorinae and are overwhelmingly dominated by single ornithuromorph taxa that phylogenetic analyses have repeatedly resolved as close relatives. This raises the possibility that the two sites were deposited under comparable paleoenvironmental settings that are otherwise poorly represented at known Jehol localities. 

Key Words: Early Cretaceous, Gansus yumenensis, Jian changmaensis, microraptorine, paleobiogeography, paleoenvironment, phylogeny, Sihedang 


SYSTEMATIC PALEONTOLOGY 

Dinosauria Owen, 1842 
Saurischia Seeley, 1888 
Theropoda Marsh, 1881 
Maniraptora Gauthier, 1986 
Dromaeosauridae Matthew and Brown, 1922 
Microraptorinae Xu, 2002 

Holotype of Jian changmaensis, gen. et sp. nov. (GSGM-D050), an articulated partial left pectoral girdle (scapulocoracoid) and forelimb (humerus, radius, and ulna). A, silhouette of generalized microraptorine dromaeosaurid theropod (courtesy Scott Hartman) showing skeletal elements preserved; B, photograph of specimen as preserved, exposed primarily in dorsomedial (scapulocoracoid), caudodorsal (humerus), and dorsal (radius and ulna) views; C, interpretive line drawing of B; D, detail photograph of scapulocoracoid and proximal end of humerus in caudodorsal view, showing supracoracoid fenestra and other structures; E, interpretive line drawing of D.
Abbreviations: ac, acromion; bc, bicipital crest; C, coracoid; cr, caudal ridge; dep, dorsal epicondyle; dpc, deltopectoral crest; dr, dorsal ridge; ed, epicondylar depression; fs?, fossa for M. supinator?; H, humerus; hh, humeral head; lp, lateral process; ‘mb’, ‘medial bar’; op, olecranon process; R, radius; S, scapula; scb, scapular blade; scf, supracoracoid fenestra; sta, sternal articulation; U, ulna.

Jian changmaensis, gen. et sp. nov.

Diagnosis.—Medium-sized (intermediate in skeletal dimensions between adult specimens of Microraptor zhaoianus and Sinornithosaurus millenii Xu et al., 1999; see Table 2) microraptorine dromaeosaurid theropod characterized by the following three autapomorphies: (1) a coracoid that is proportionally longer relative to the humerus than in any other microraptorine (~36% humerus length; the next closest individuals are the immature Microraptor IVPP V31612, with a value of ~35%, and IVPP V12811, the holotype of Sinornithosaurus, with a value of 33%) (Table 2); (2) humeral distal condyles developed on the cranial surface of this bone (Figs. 2B–C, 3E; a local autapomorphy within Microraptorinae, shared with nonmicroraptorine theropods such as the therizinosaur Erlikosaurus andrewsi Barsbold and Perle, 1980, and Aves); and (3) a well-developed foramen on the ventral aspect of ...

Etymology.—The genus name is for the Jiān (鹣), a one winged bird in Chinese mythology, in reference to the bird-like, possibly volant nature of this microraptorine taxon and the skeletal composition of its holotype (an isolated partial pectoral girdle and forelimb). The specific name is for Changma (昌马), the locality where the holotype was discovered.

 The new microraptor dinosaur Jian changmaensis (left) attacks the early bird Gansus yumenensis (right) in what is now the Changma Basin of northwestern China approximately 120 million years ago. 
 illustration by Lewis LaRosa  x.com/LewisLaRosa,
colorized by Jão Canola.


Ling-Qi Zhou, Matthew C. Lamanna, Ashley W. Poust, Da-Qing Li, Hai-Lu You and Jingmai K. O’Connor. 2026. First non-Avian Theropod (Dromaeosauridae, Microraptorinae) from the Bird-bearing Lower Cretaceous Xiagou Formation of the Changma Basin, Gansu Province, Northwestern China. ANNALS OF CARNEGIE MUSEUM. 92(2); 89–110. [4 June 2026]


Thursday, May 14, 2026

[Paleontology • 2026] Nagatitan chaiyaphumensis • The First Sauropod Dinosaur (Titanosauriformes: Euhelopodidae) from the Lower Cretaceous Khok Kruat Formation of Thailand enriches the Diversity of somphospondylan titanosauriforms in Southeast Asia


Nagatitan chaiyaphumensis 
Sethapanichsakul, Khansubha, Manitkoon, Hanta, Mannion & Upchurch, 2026

นาคาไททัน ชัยภูมิเอนซิส  ||  DOI: doi.org/10.1038/s41598-026-47482-x 

Abstract
Sauropod dinosaur remains comprise the majority of the Mesozoic vertebrate fossil record in Thailand. However, they are rare and fragmentary in the Aptian–Albian (Lower Cretaceous) Khok Kruat Formation, the stratigraphically youngest fossil-bearing Mesozoic Thai stratigraphic unit. Based on a partial postcranial skeleton, we present the first diagnostic sauropod specimen from this formation, which represents a new somphospondylan titanosauriform, Nagatitan chaiyaphumensis n. gen. n. sp. Nagatitan is diagnosed by two autapomorphies and a unique character combination, including the presence of two distinct hyposphene-hypantrum morphologies within the middle–posterior dorsal vertebrae. Phylogenetic analyses under maximum parsimony, using a data matrix containing 153 taxa and 570 characters, produce well-resolved topologies that place Nagatitan within the somphospondylan clade Euhelopodidae. Nagatitan does not form an endemic subclade with the approximately contemporaneous Southeast Asian euhelopodids Phuwiangosaurus and Tangvayosaurus, with a suite of anatomical features distinguishing these taxa. We estimate a body mass of 25–28 tonnes for Nagatitan, and suggest it was part of a broader middle Cretaceous body size increase in Asian titanosauriforms, facilitated by rising temperatures and expanded suitable habitat. The discovery of Nagatitan expands the known diversity of Southeast Asian sauropods and improves our understanding of titanosauriform biogeography within the region.


Schematic representation of the skeleton of Nagatitan chaiyaphumensis gen. et. sp. nov. Preserved bones are highlighted. Scale bar equals 1 m.

Systematic palaeontology
Dinosauria Owen, 1842
Saurischia Seeley, 1887

Sauropoda Marsh, 1878
Titanosauriformes Salgado, Coria & Calvo, 1997
Somphospondyli Wilson & Sereno, 1998

Euhelopodidae Romer, 1956 (sensu D’Emic, 2012)

Nagatitan chaiyaphumensis gen. et sp. nov.
นาคาไททัน ชัยภูมิเอนซิส

Holotype: SM2025-1-546 to SM2025-1-556—four dorsal vertebrae, five dorsal ribs, four sacral vertebrae, five sacral ribs, right humerus, right ilium, left and right pubis, mostly complete right femur.

Diagnosis: Nagatitan can be diagnosed by a unique combination of characters (autapomorphies denoted with an asterisk): (1) paired postzygapophyseal centrodiapophyseal fossa present on posterior dorsal neural arches; (2*) hyposphene of middle dorsal vertebrae exhibits a triangular morphology, becoming a vertical ridge in posterior dorsal vertebrae; (3) parapophysis positioned dorsal to the prezygapophysis on posterior dorsal neural arches; (4) spinopostzygapophyseal laminae of middle and posterior dorsal neural spines divided into lateral and medial branches throughout their length; (5) bifurcated middle dorsal neural spines; (6*) triangular anterior aliform processes present on posterior dorsal neural spines; (7) prominent bulge on posterolateral margin of humerus, approximately level with the deltopectoral crest, that interrupts the lateral humeral margin in anterior view; (8) rounded proximolateral corner of humerus; (9) humeral shaft exhibits a high eccentricity value (> 2.5); (10) distal end of the pubis transversely expanded along the lateral surface relative to the shaft; and (11) proximal third of femur with anteroposteriorly narrowed lateral margin forming a flange-like trochanteric shelf and a medially bounding vertical ridge along the posterior surface.

Locality and Horizon: Ban Pha Nang Sua, Nong Bua Rawe District, Chaiyaphum Province, Thailand; Khok Kruat Formation, Aptian–Albian, upper Lower Cretaceous. 

Etymology: The generic name is derived from Naga, referring to the mythological serpent-like creature found in various Asian cultures, especially in northeastern Thailand, often associated with water and Buddhism, and titan, a giant in Greek mythology. The specific epithet is derived from the province of Chaiyaphum, Thailand.


3D skeletal reconstruction by Matus Charoenjit

Stylized life reconstruction of Nagatitan chaiyaphumensis gen. et. sp. nov. within the arid floodplains of late Early Cretaceous Aptian–Albian Thailand  
Artistic reconstruction by Patchanop Boonsai (Draconos Takeji) 

Non-sauropod faunal remains discovered in the Ban Pha Nang Sua locality:
(a) Allosauroid tooth (SDM2025-1-562) in labial view, (b) spinosaurid tooth (SDM2025-1-561) in labial view, (c) crocodyliform tooth (specimen lost during the excavation) in lingual view, (d) Heteroptychodus steinmanni tooth (SDM2025-1-563) in apical view, and (e) mold of cf. Yunnanoconcha sp. (SDM2025-1-560) in external view. (f) Stylized illustration displaying the vertebrate fauna assemblage known from the Khok Kruat Formation modified from Manitkoon et al. 2023. Shaded black silhouette indicate tentative taxa. Nagatitan chaiyaphumensis gen. et sp. nov. shaded in blue. Scale bars equal 10 mm.

  

 
Thitiwoot Sethapanichsakul, Sasa-On Khansubha, Sita Manitkoon, Rattanaphorn Hanta, Philip D. Mannion and Paul Upchurch. 2026. The First Sauropod Dinosaur from the Lower Cretaceous Khok Kruat Formation of Thailand enriches the Diversity of somphospondylan titanosauriforms in Southeast Asia. Scientific Reports. 16; 12467. DOI: doi.org/10.1038/s41598-026-47482-x [14 May 2026]

Thursday, April 23, 2026

[Paleontology • 2026] Phosphatotitan khouribgaensis • A Titanosaurian Sauropod with South American Affinities (Lognkosauria: Argentinosauridae) from the Late Maastrichtian of Morocco and Evidence for Dinosaur Endemism in Africa

 

Phosphatotitan khouribgaensis
Longrich, Pérez-Moreno, Díez Díaz, Pereda-Suberbiola, Bardet & Jalil, 2026

Artwork by Andrey Atuchin facebook.com/AndreyAtuchin

Abstract
The latest Cretaceous saw the final diversification of dinosaurs before the K/Pg extinction. Discussions of end-Cretaceous dinosaur diversity have focused on well-sampled faunas from Laurasia; far less is known about dinosaurian faunas of the Southern Hemisphere, especially Africa. The late Maastrichtian Phosphates of Morocco provide a rare window into African dinosaur diversity. Abelisaurids, lambeosaurines, and titanosaurian sauropods are known. However, no diagnostic titanosaur remains have been recovered, leaving the affinities of these sauropods unclear. We describe Phosphatotitan khouribgaensis gen. et sp. nov., a new titanosaur from the Maastrichtian of Sidi Chennane, Khouribga Province. Phosphatotitan is represented by dorsal, sacral, and caudal vertebrae, and the pelvis. The new species differs from titanosaurs described from the Cretaceous of Africa and Europe but resembles South American Lognkosauria, and especially Patagotitan, in having short dorsal and caudal centra, expanded dorsal and caudal neural spines, and a broad pubis. Its small size relative to other Lognkosauria (3.5–4 tonnes) suggests a lineage selected for small size. The close relationships of Morocco’s titanosaurs and abelisaurids to South American species may reflect a wide distribution of these clades prior to the opening of the South Atlantic and the separation of Africa and South America ~100 Ma, while a complex pattern of oceanic dispersal may explain the presence of distinct saltasauroid lineages worldwide. The latest Cretaceous Gondwanan dinosaur faunas were highly endemic due to a combination of continental fragmentation, extinction, and dispersal, creating high endemism in southern continents and within Africa, suggesting that Maastrichtian dinosaur diversity is underestimated.

Keywords: Dinosauria; Sauropoda; Titanosauria; Argentinosauria; Upper Cretaceous; biogeography; Gondwana



Phosphatotitan khouribgaensis gen. et sp. nov.






 Nicholas R. Longrich, Agustín Pérez-Moreno, Verónica Díez Díaz, Xabier Pereda-Suberbiola, Nathalie Bardet and Nour-Eddine Jalil. 2026. A Titanosaurian Sauropod with South American Affinities (Lognkosauria: Argentinosauridae) from the Late Maastrichtian of Morocco and Evidence for Dinosaur Endemism in Africa. Diversity. 18(5); 241. DOI: doi.org/10.3390/d18050241 [22 April 2026]

Friday, April 17, 2026

[Paleontology • 2026] Ptychotherates bucculentus • A New Taxon of saurischian Dinosaur (Saurischia: Morphoraptor) from the Coelophysis Quarry of New Mexico, USA (Triassic: latest Norian or Rhaetian) highlights herrerasaurian diversity in the latest Triassic

 

Ptychotherates bucculentus 
Srivastava & Nesbitt, 2026


Abstract
The most complete record of the earliest dinosaur lineages is from the Carnian from the higher latitudes of Pangea (e.g. present-day Brazil, Argentina), but dinosaurian assemblages from the upper stages of the Upper Triassic are better known from the low latitudes of Pangea (present day southwestern USA). How early carnivorous dinosaurian diversity matches or mismatches at various latitudes remains to be documented because of uncertainty around the spatio-temporal ranges and phylogenetic relationships of early dinosaur lineages. We examine low-latitude diversity patterns through the lens of the saurischian dinosaur Tawa hallae and close relatives, including a new species, Ptychotherates bucculentus gen. et sp. nov. The new taxon is known from an incomplete but well-preserved skull (CM 31368) from the uppermost Triassic Coelophysis Quarry in northern New Mexico. The new taxon clearly shares synapomorphies with Tawa hallae, such as distinctive fossae on the quadrate and otoccipital and a dorsoventrally tall and laterally flat jugal. However, the new taxon is distinguishable from all other coeval ornithodirans by a combination of many character states, including the proportionally dorsoventrally deepest jugal known for any Triassic-aged dinosaur. Higher-palaeolatitude ecosystems across Pangea show a complete turnover of carnivorous dinosaurs by neotheropods in the Norian and Rhaetian, but the ‘ChindesaurusTawa’ clade (Morphoraptora clade nov.) coexisted with neotheropods possibly until the End-Triassic Extinction Event. This suggests a low-latitude ‘museum’ where early-diverging lineages survived much longer than at higher latitudes, and that the End-Triassic Extinction Event affected dinosaur diversity more than previously hypothesized.

Keywords: biogeography, Saurischia, extinction, skull, phylogenetics, clade longevity

SYSTEMATIC PALAEONTOLOGY
DINOSAURIA Owen 1842 sensu Langer et al. 2020
SAURISCHIA Seeley 1888 sensu Gauthier et al. 2020

Clade MORPHORAPTORA nov.

Derivation of name: Morphe from the Greek for ‘form, shape’ and raptor from the Latin for ‘robber’, describing the morphological convergence between members of this clade and Theropoda, as if this clade is ‘stealing’ morphology. ‘Morphoraptor’ loosely translates to ‘bodysnatcher’, in honour of the 2007 song by Radiohead in the album In Rainbows, which author S. Srivastava listened to hundreds of times while preparing this manuscript.

The posterior portion of the skull Ptychotherates bucculentus (CM 31368) in posterior view.
Abbreviations: ar, articular bo, basioccipital; bt, basituber; f, frontal; fm, foramen magnum; fno, fenestra ovalis; pa, parietal; par, paroccipital process of the otoccipital; mf, metotic foramen; n, nasal; pbs, parabasisphenoid; pf, prefrontal; po, postorbital; ptf, posttemporal fenestra; qj, quadratojugal; qu, quadrate; rap, retroarticular process; so, supraoccipital; sq, squamosal; st, stapes. Crossed circle indicates posterior direction out of page. Scale bar represents 1 cm.

Digital reconstruction of the skull of Ptychotherates bucculentus (CM 31368) in left lateral view. Dashed lines indicate extrapolation and the coloured infill indicates known bone presence.
Abbreviations: eaf, external antorbital fenestra; en, external naris; emf, external mandibular fenestra; itf, infratemporal fenestra; orb, orbit. Arrow indicates anterior direction. Scale bar represents 2 cm.
 
Genus Ptychotherates nov.
 
Derivation of name: Ptycho from the Greek for ‘fold’ because of the numerous and challenging axes of reorientation on elements of the holotype. Therates from the Greek for ‘hunter’, for the carnivorous habits inferred from its teeth.

 Ptychotherates bucculentus sp. nov.  

Derivation of name: The species epithet is Latin for ‘with full cheeks’ in reference to the exceptionally tall jugal.
 
Diagnosis: Ptychotherates bucculentus bears the following combination of character states (local autapomorphies indicated with *): supratemporal fossa present on posterior portion of the frontal and dorsal surface of the parietal; tapering dorsal process of the maxilla; maxilla lacking antorbital fossa on its posterior portion ventral to the antorbital fenestra; prefrontal symmetrical in lateral view*; jugal body proportionally dorsoventrally deep* (i.e. more than three times as deep as the jugal posterior process, deeper than the length of postorbital ventral process, and more than half the height of the quadrate main body; Table 1); laterally extensive ventral process (= crista interfenestralis) of the otoccipital; ventral process of squamosal anteroposteriorly wide with a lateral fossa on the posterior part; retroarticular process upturned immediately posterior to glenoid; anterolateral portion of postorbital dorsally overhanging orbit; postorbital dorsolaterally overlapping the squamosal; posttemporal fenestra as wide as foramen magnum; nasal and frontals flat dorsally; serrated and recurved teeth with fine serrations (4–5 per 1 mm in the maxilla, 5–6 per 1 mm in the dentary) with pointed apices of the serrations.

Artistic rendition of Ptychotherates bucculentus.
Artwork by Megan Sodano 


 
Simba Srivastava and Sterling J. Nesbitt. 2026. A New Taxon of saurischian Dinosaur from the Coelophysis Quarry of New Mexico, USA (Triassic: latest Norian or Rhaetian) highlights herrerasaurian diversity in the latest Triassic. Papers in Palaeontology. 12(2); e70069. DOI: doi.org/10.1002/spp2.70069 [14 April 2026]


Friday, February 20, 2026

[Paleontology • 2026] Spinosaurus mirabilis • Scimitar-crested Spinosaurus species from the Sahara caps stepwise spinosaurid radiation


Spinosaurus mirabilis
Sereno, Vidal, Myhrvold, Johnson-Ransom, Ciudad Real, Baumgart, Sánchez Fontela, Green, Saitta, Adamou, Bop, Keillor, Fitzgerald, Dutheil,  Laroche, Demers-Potvin, Simarro, Gascó-Lluna,  Lázaro, Gamonal, Beightol, Reneleau, Vautrin, Bertozzo, FGranados, Kinney-Broderick, Mallon, Lindoso, Ramezani & Jahandar, 2026
 
Artwork: Dani Navarro

 Abstract
INTRODUCTION: The fossils of Spinosaurus aegyptiacus, a giant sail-backed, fish-eating theropod dinosaur from northern Africa, have inspired competing lifestyle interpretations, either as a semiaquatic ambush predator stalking shorelines and shallows or a fully aquatic predator in pursuit of prey underwater. Its bones and teeth have been found only in coastal deposits near marine margins, a locale potentially consistent with either lifestyle interpretation.

RATIONALE: In the central Sahara, a new fossiliferous area (Jenguebi) was discovered in beds equivalent in age [Farak Formation; Cenomanian ~95 million years ago (Mya)] to those yielding fossil remains of S. aegyptiacus. We describe from this area a new species, Spinosaurus mirabilis sp. nov., which is very similar to S. aegyptiacus in skeletal form but with a much taller, scimitar-shaped cranial crest. Two new sauropods were found in close association with the new spinosaurid buried in fluvial sediments indicative of an inland riparian habitat.

RESULTS: Spinosaurus mirabilis sp. nov. is distinguished by the low profile of its snout, a hypertrophied nasal-prefrontal crest, greater spacing of posterior maxillary teeth, and other features. Its features highlight the extraordinary specializations of both species of the genus Spinosaurus, including interdigitating upper and lower teeth. Principal component analysis of body proportions places spinosaurids between semiaquatic waders (e.g., herons) and aquatic divers (e.g., darters) distant from all other predatory dinosaurs. A time-calibrated phylogenetic analysis resolves three evolutionary phases: an initial Jurassic radiation when their distinctive elongate fish-snaring skull evolved and split into two distinctive designs, baryonychine and spinosaurine; an Early Cretaceous circum-Tethyan diversification when both reigned as dominant predators; and a final early Late Cretaceous phase when spinosaurines attained maximum body size as shallow water ambush specialists limited geographically to northern Africa and South America.

CONCLUSION: The discovery of the tall-crested S. mirabilis sp. nov. in a riparian setting within an inland basin supports a lifestyle interpretation of a wading, shoreline predator with visual display an important aspect of its biology. At the end of the Cenomanian about 95 million years ago, an abrupt eustatic rise in sea level and the attendant climate change brought the spinosaurid radiation to an end.





Sheathed bony head crests in extinct and living dinosaurs. Spinosaurus mirabilis sp. nov., evolved the tallest head crest of any theropod dinosaur, drawing attention to the midline ornamentation that characterizes the cranium and axial skeleton of all spinosaurids. In life, the crest would have been extended to some degree by a keratinous sheath, as in the living helmeted guinea fowl (Numida meleagris). Visual signaling, as is the case in guinea fowl and other crested avians, was likely the function of spinosaurid cranial crests and trunk and tail sails. Scale bar, 20 cm for S. mirabilis and 3 cm for N. meleagris.

Spinosaurus mirabilis



A single Spinosaurus mirabilis rears over a carcass of the coelacanth Mawsonia on the forested bank of a river some 95 million years ago in what is now the Sahara Desert in Niger. A scimitar-shaped head crest and interdigitating teeth characterize this wading giant, one of the last-surviving species of a spinosaurid radiation some 50 million years in the making.
Artwork: Dani Navarro

Sereno, Paul C.; Vidal, Daniel; Myhrvold, Nathan P.; Johnson-Ransom, Evan; Ciudad Real, María; Baumgart, Stephanie L.; Sánchez Fontela, Noelia; Green, Todd L.; Saitta, Evan T.; Adamou, Boubé; Bop, Lauren L.; Keillor, Tyler M.; Fitzgerald, Erin C.; Dutheil, Didier B.; Laroche, Robert A. S.; Demers-Potvin, Alexandre V.; Simarro, Álvaro; Gascó-Lluna, Francesc; Lázaro, Ana; Gamonal, Arturo; Beightol, Charles V.; Reneleau, Vincent; Vautrin, Rachel; Bertozzo, Filippo; Granados, Alejandro; Kinney-Broderick, Grace; Mallon, Jordan C.; Lindoso, Rafael M.; Ramezani, Jahandar. 2026. Scimitar-crested Spinosaurus species from the Sahara caps stepwise spinosaurid radiation. Science. 391 (6787) eadx5486. DOI: doi.org/10.1126/science.adx5486 [19 Feb 2026] 
 
Editor’s summary: Recent descriptions of and debates about the massive, fish-eating dinosaur Spinosaurus have brought this striking predator to the forefront of the dinosaur pantheon. Its huge size and distinctive morphology have stimulated much debate about the degree to which it lived an aquatic lifestyle. Sereno et al. describe a crested fossil Spinosaurus found in northern Africa as a new species. The researchers argue that this group of dinosaurs underwent three phases of evolution with increasing aquatic adaptations and existence in habitats around the Tethys Sea. —Sacha Vignieri