[PaleoEntomology • 2026] Cretolala kachinensis (Hemiptera: Fulgoromorpha: Delphacoidea) • the First lalacid from mid-Cretaceous Kachin Amber: Morphological and Taphonomic Implications

Cretolala kachinensis 

Tang, ŠMÍDOVÁ, Ding, BODERAU, Fabrikant, Mähler, Deng, Nyunt, Fu, Jouault, Tomaschek, Szwedo & Jiang, 2026

 

 DOI: doi.org/10.11646/palaeoentomology.9.2.5

Abstract 

We report Cretolala kachinensis gen. et sp. nov., the first formally described representative of the family Lalacidae from mid-Cretaceous (~99 Ma) Kachin amber. The morphology and taphonomy of the specimen were studied using optical microscopy, micro-computed tomography (micro-CT), confocal laser scanning microscopy (CLSM), and scanning electron microscopy coupled with energy-dispersive X-ray spectroscopy (SEM‒EDS). Cretolala kachinensis gen. et sp. nov. exhibits a unique combination of forewing characters, including a strengthened, broad, and wrinkled costal margin; ScP+R fork proximal to both the Pcu+A1 fusion and the CuA fork; MP with five terminals; and CuA1 and CuA2 each with two terminals. Crossvein patterns differ between the left and right forewings, indicating that crossvein expression alone is not diagnostic. The forewing bears distinct maculation, with a face-like pattern dorsally and an extensive lateral pattern that may indicate aposematism, mimicry, or plant-like camouflage in an arboreal herbivore. Taphonomic analyses based on optical micrographs and material-dependent X-ray attenuation in micro-CT show that minerals are distributed throughout the fossil, coating anatomical surfaces and infilling pre-existing cavities and voids. These phases help stabilize morphology and influence the micro-CT reconstruction of soft-bodied structures. SEM–EDS analyses indicate that the body-coating and void-filling minerals are dominated by quartz and pyrite, with feldspars and aluminosilicate mixtures also present, locally enriched in K, Na, Mg, or Ca. This assemblage and its textures point to a polyphase paragenetic sequence, with early detrital infill and later authigenic mineralization. Our results suggest that minerals and some chemicals derived from the host sediments can be transported into and, in some cases, precipitated within amber inclusions, infilling voids and providing structural support that influences fossil preservation. Collectively, these phases occlude porosity, stabilize morphology, and enhance X-ray contrast, although they locally obscured primary tissue boundaries. Our results highlight multistage diagenesis in Kachin amber and underscore variability among inclusions in both mineral assemblages and the timing of mineralization/diagenetic events.

Hemiptera, Fulgoromorpha, Delphacoidea, Mesozoic, Burmese amber, Planthopper, taxonomy, taphonomy, mineral infilling, wing maculation

Cretolala kachinensis gen. et sp. nov., holotype (HMJ–2016–019).
A–D, Reflected-light micrographs. A, Right lateral view. B, Left lateral view. C, Dorsal view. D, Ventral view. E, F, Micro-computed tomography (micro-CT) reconstructions. E, Dorsal view. F, Ventral view. Scale bars = 1 mm.

Systematic palaeontology

Order Hemiptera Linnaeus, 1758

Suborder Fulgoromorpha Evans, 1946

Superfamily Delphacoidea Leach, 1815

Family Lalacidae Hamilton, 1990

Cretolala Jiang, Boderau, Jouault & Szwedo gen. nov.

  

Etymology. The generic name is formed from the combination of “Cretaceous” and generic name “Lalax”; the latter is derived from the Greek λάλαξ (“croaker”, “caller”), in reference to a lalacid planthopper from the Cretaceous. Gender is feminine.

Diagnosis (provisional, pending confirmation from additional specimens and in combination with specieslevel diagnostic characters). Tegmen with narrow base and distinctly widened apical portion; costal margin strengthened, broad and wrinkled. Pc+CP shifted away from anterior margin near tegmen base, parallel to CA, forming a narrow, sclerotized costal area. ScP+R forks basad both CuA fork and Pcu+A1 fusion. RA with two terminals; RP with three terminals; MP with five terminals; CuA1 and CuA2 with two terminals each. 

Cretolala kachinensis Jiang, Boderau, Jouault & Szwedo sp. nov.  

Material. Holotype: HMJ–2016–019, adult female in Kachin (Burmese) amber from northern Myanmar. Repository: Myanmar Gems Museum, Nay Pyi Taw, Myanmar. Condition: the specimen is incomplete, with the head and the dorsal part of the thorax missing. 

Etymology. The specific epithet is derived from “Kachin”, the name of the state in northern Myanmar where the amber originates, and is Latinized with the adjectival suffix -ensis, meaning from “Kachin”. 

Diagnosis. As for the genus, due to monotypy. Additional features include forewing coloration and venation details: costal margin with a continuous dark band along costal area; membrane bearing nearly continuous aligned patches and short transverse bands; a discrete insular macula on ScP+RA; a sub-elliptical isolated macula near distal Pcu; distad of forks of RP and MP, pigment is vein-following, tracking adjacent longitudinal and crossveins; postnodal cell centers unpigmented, ...

 Life reconstruction of Cretolala kachinensis gen. et sp. nov.

 (illustrated by Lucia Šmídová).

Ya-Ni TANG, Lucia ŠMÍDOVÁ, Ying-Ying DING, Mathieu BODERAU, Dolev FABRIKANT, Bastian MÄHLER, Jun-Chen DENG, Thet Tin NYUNT, Yan-Zh FU, Corentin JOUAULT, Frank TOMASCHEK, Jacek SZWEDO, Hui JIANG. 2026. Cretolala kachinensis gen. et sp. nov. (Hemiptera: Fulgoromorpha: Delphacoidea), the First lalacid from mid-Cretaceous Kachin Amber: Morphological and Taphonomic implications. Palaeoentomology. 9(2); 125-138. DOI: doi.org/10.11646/palaeoentomology.9.2.5 [2026-04-29]

[PaleoEntomology • 2026] Qiongqi multispurous • A New Cricket (Orthoptera: Trigonidiidae) from mid-Cretaceous Kachin Amber in Northern Myanmar

Qiongqi multispurous 

Ji, Nel, Xiao & Xu, 2026

DOI: doi.org/10.54103/2039-4942/29769

Abstract

A new species of Trigonidiidae, †Qiongqi multispurous sp. nov., is described from mid-Cretaceous Kachin amber. It can be definitely attributed to the family Trigonidiidae, but excluded from the two extant subfamilies. It also exhibits a different morphology from all reported trigonidiids genera and species from the Mesozoic, including subapical/apical spurs on the hind tibia and setae-like processes on the hind basitarsomere. This new discovery provides novel morphological information of Cretaceous Trigonidiidae, and highlights the potential of biodiversity of Cretaceous crickets.

Keywords: Trigonidiidae; mid-Cretaceous; new species; fossil; morphology

Qiongqi multispurous sp. nov., holotype NIGP210185.
A) Photograph of  habitus in dorsal view. B) Drawing of  habitus in dorsal view.
C) Drawing of  habitus in ventral view. D) Photograph of  habitus in ventral view.

Scale bars = 1 mm.

Qiongqi multispurous sp. nov.

XIA JI, ANDRÉ NEL, CHUANTAO XIAO and CHUNPENG XU. 2026. A NEW CRICKET (ORTHOPTERA: TRIGONIDIIDAE) FROM MID-CRETACEOUS KACHIN AMBER IN NORTHERN MYANMAR. RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA. 132(1); DOI: doi.org/10.54103/2039-4942/29769 [06-03-2026]

[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 

  

 facebook.com/CarnegieMNH 

 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]

https://carnegiemnh.org/wp-content/uploads/2026/06/Jian-changmaensis-Annals-of-Carnegie-Museum.pdf

 facebook.com/CarnegieMNH/posts/1431015332396739

 x.com/LewisLaRosa/status/2062606679980556631

[Paleontology • 2026] Patagoniaemys aeschyli • A New meiolaniform Turtle from the Maastrichtian of Northern Patagonia, Argentina

Patagoniaemys aeschyli

Agnolin, Rolando, Sterli, Chimento, Novas & Muñoz, 2026

DOI: doi.org/10.4202/app.01268.2025 

 www.macnconicet.gob.ar 

Meiolaniformes are a group of chelonians including the famous horned-turtles Niolamia argentina (Patagonia) and Meiolania platyceps (Australia). In South America, the Late Cretaceous meiolaniforms are represented by two named taxa: Patagoniaemys gasparinae coming from Campanian–Maastrichtian beds of the La Colonia Formation, Chubut province, and Trapalcochelys sulcata from the Campanian–Maastrichtian beds of the Allen Formation, Río Negro Province. The aim of the present contribution is to describe a new meiolaniform chelonian coming from the Upper Cretaceous (Maastrichtian) Los Alamitos Formation, at Río Negro Province, Argentina. The material is represented by a partial basicranium, incomplete carapace and fragmentary postcranial bones (MPMIK 1839/P/33) belonging to a new species Patagoniaemys aeschyli. To this new species we refer all the material previously referred as indeterminate meiolaniid, meiolaniform and cf. Niolamia sp., coming from the same site and locality, and described by different authors since the 1980s. This new species differs from the type species P. gasparinae, particularly by the presence of longitudinal ridges in the nuchal bone. We also include brief comments about meiolaniform palaeobiogeography and the impact of K/Pg extinction event in Patagonian chelonians.

Key words: Testudinata, Meiolaniformes, Los Alamitos Formation, Maastrichtian, Cretaceous, Patagonia, Argentina.

Meiolaniform turtle Patagoniaemys aeschyli sp. nov. holotype (MPMIK 1839/P/33); Cerro Cuadrado locality, Argentina, Los Alamitos Formation Maastrichtian (Upper Cretaceous).
A. Carapace; anterior border in dorsal (A1, A2) and ventral (A3, A4) views, detail of the anterior margin in ventral view (A7, A8), showing the presence of longitudinal ridges that characterize the new species (light grey, nuchal bone; dark grey, broken surfaces).
B. Left hyoplastron fragment Scale bars 100 mm.

Testudinata Klein, 1760 

Meiolaniformes Sterli & de la Fuente, 2013 

Genus Patagoniaemys Sterli & de la Fuente, 2011a 

Type species: Patagoniaemys gasparinae Sterli & de la Fuente, 2011a;
Chubut Province, Argentina, Campanian–Maastrichtian. 

Patagoniaemys aeschyli sp. nov.

Diagnosis.—Large chelonian (maximum anterior carapace width about 60 cm, maximum inferred carapace length 80 cm). Referable to meiolaniforms by several features, namely the presence of small pits and grooves ornamenting carapace bones, anteriorly curved grooves among marginal scutes, opisthocoelous caudal vertebrae, and carapace-plastron connection through ligaments (Gaffney 1996; Hirayama et al. 2000; Sterli and de la Fuente 2013; Sterli et al. 2013). It is referred to Patagoniaemys by having a basioccipital with well-developed basal tubera with a concave surface between them, posteriorly flat occipital condyle, a shallowly notched anterior carapace margin, presence of a thickened bump on ...

Etymology: In reference to Aeschylus (525–455 BC), an ancient Greek writer often described as the father of tragedy. During a visit to the city of Gela (Italy), he was killed outside the city by a tortoise dropped by an eagle, which had mistaken his bald head for a rock suitable for shattering the shell.

the excavation work at the Los Alamitos Formation southwest of Cerro Cuadrado.  

Federico L. Agnolin, Mauro Aranciaga Rolando, Juliana Sterli, Nicolás R. Chimento, Fernando E. Novas, and Gonzalo L. Muñoz. 2026. A New meiolaniform Turtle from the Maastrichtian of Northern Patagonia, Argentina. Acta Palaeontologica Polonica. 71(1); 173-184. DOI: doi.org/10.4202/app.01268.2025 

 Researchgate.net/publication/403290389_A_new_meiolaniform_turtle_from_the_Maastrichtian_of_Northern_Patagonia_Argentina

DESCUBREN UNA TORTUGA GIGANTE DEL FIN DE LA ERA DE LOS DINOSAURIOS EN PATAGONIA

https://www.macnconicet.gob.ar/descubren-una-tortuga-gigante-del-fin-de-la-era-de-los-dinosaurios-en-patagonia

[Paleontology • 2026] Kank australis • New unenlagiid (Theropoda: Unenlagiidae) from the Chorrillo Formation (Late Cretaceous, Maastrichtian), SW Patagonia, Argentina

 

Kank australis

Motta, Rolando, Rozadilla, Agnolín, Egli, Herrera, Chimento, Coco, Tsuihiji, Manabe, Pol & Novas, 2026

 

DOI: doi.org/10.1080/02724634.2026.2656456 

A reconstruction by Gabriel Díaz Yantén

 

ABSTRACT

Unenlagiids constitute a group of paravian theropods up to now represented in Gondwanan landmasses. They are particularly diverse in northern Patagonia, where at least seven species were discovered in Upper Cretaceous beds. In southern Patagonia, by contrast, the record is restricted to a few isolated remains of indeterminate taxa from Argentina and Chile. The aim of the present contribution is to describe an unenlagiid, Kank australis gen. et sp. nov. from the Maastrichtian beds of southern Santa Cruz, southern Patagonia, Argentina. Kank australis is represented by vertebrae, isolated pedal phalanges, and shed teeth. The holotype individual has a unique combination of characters, including a highly pneumatized cervical vertebra with well-developed parapophysis and carotid processes. Further, a pedal phalanx II-2 resembles those of troodontids due the reduction of the distal condyles, and differs from other known unenlagiids. The apomorphic condition of the few available elements suggests that Kank australis was probably distinct from its kin and reinforces the hypothesis that Unenlagiidae was a morphologically disparate clade.

SYSTEMATIC PALEONTOLOGY

DINOSAURIA OWEN, 1842

SAURICHIA SEELEY, 1888

THEROPODA MARSH, 1881

PARAVES SERENO, 1997

UNENLAGIIDAE (Bonaparte, 1999)

KANK AUSTRALIS gen. et sp. nov.

Diagnosis—Medium-sized unenlagiid (phalanges similar in size to Neuquenraptor argentinus estimated in ∼27 kg; Motta, 2023) showing the following combination of characters (autapomorphies marked by an asterisk): (1) dentary teeth having mesial carinae restricted to the apical third of the crown (shared with Austroraptor); (2) labiolingually compressed maxillary teeth “8” in cross-section (shared with Buitreraptor); (3) dentary teeth having a crenulate mesial carina restricted to its apical third; (4) cervicodorsal vertebra having three pneumatic foramina on its ventral surface*; (5) cervicodorsal vertebra having epipophyseal fossa*; and (6) phalanx 2-II showing reduced distal condyles and collateral pits located very close to the anterodorsal corner of the condyles (shared with troodontids).

Etymology—“Kank,” in reference to the “elder Rhea,” who created the constellation Choiols (Southern Cross constellation) in the Aonikenk mythology, and “australis,” which means “from south” in Latin, in reference to the southern latitude where this dinosaur was found.

 

Matías J. Motta, Alexis M. Aranciaga Rolando, Sebastián Rozadilla, Federico L. Agnolín, Federico Brissón Egli, Gerardo P. Álvarez Herrera, Nicolás R. Chimento, Gastón Lo Coco, Takanobu Tsuihiji, Makoto Manabe, Diego Pol and Fernando E. Novas. 2026. New unenlagiid from the Chorrillo Formation (Late Cretaceous, Maastrichtian), SW Patagonia, Argentina. Journal of Vertebrate Paleontology. e2656456. DOI: doi.org/10.1080/02724634.2026.2656456  [28 May 2026]

https://newsroom.taylorandfrancisgroup.com/heron-like-fish-eating-dinosaur-from-70-million-years-ago-discovered-in-argentina

https://www.macnconicet.gob.ar/kank-australis-el-nuevo-raptor-descubierto-en-la-patagonia-argentina

[PaleoOrnithology • 2026] Plumadraco bankoorum • Hyperelongate Ornamental Tail Feathers in A New early Cretaceous enantiornithine Bird

 

Plumadraco bankoorum

Clark, O’Connor, X. Wang, Y. Wang, Pruett-Jones, Zhang, X.Wang, Zheng & Zhou, 2026 

 

DOI: doi.org/10.1371/journal.pone.0347641

Illustration: Ville Sinkkonen

Abstract

Bird diversity is reflected in the abundance and variety of extraordinary plumages. Some of these include elongate, ornamental tail feathers that are typically attributed to either intraspecific communication in monomorphic species or sexual selection in sexually-dimorphic ones. Enantiornithines (Aves: Ornithothoraces) were the most diverse group of birds during the Cretaceous. Importantly, some enantiornithine fossils preserve soft tissues, most often in the form of feathers surrounding the body. Unlike any living bird, many enantiornithine specimens lack tail feathers (rectrices) all together, with the tail region consisting entirely of contour feathers. However, when present, enantiornithine rectrices typically consist of a pair of elongate, ornamental feathers with unusually wide rachises, referred to as rachis-dominated feathers. Here we describe Plumadraco bankoorum gen. et sp. nov., a new bohaiornithid enantiornithine with a pair of exceptionally long rectrices. These tail feathers measure twice the individual’s body length, ending in proportionally small pennaceous rackets, thus adding to the growing diversity of these unusual feathers. The fine preservation of these tail feathers, in comparison to other enantiornithine rectrices, reveals previously unrecognized structural variation that hints at their potential function in courtship displays. Although ornamental feathers in enantiornithines are widely considered sexually dimorphic, determining the selection pressures that shaped them is difficult due primarily to limited soft tissue data. Enantiornithine rectrices are likely the result of an interplay between both sexual and naturally selective pressures, similar to the processes which produce analogous structures in birds today.

Plumadraco bankoorum. The skull of STM11−4.
(A) Photo of fossil specimen and (B) a corresponding line drawing. Well preserved bones are colored white, crushed or poorly preserved bones (or portions of bones) are grey, and preserved soft tissues are brown.

Abbreviations: at, atlas; cev, cervical vertebrae; dn, dentary; fe, feathers; fp, frontal process of the premaxilla; fe, feather; fr, frontal; l, left; mx, maxilla; ns, nasal; pmx, premaxilla; pr, parietal; r, right; su, surangular; to, tooth. 

Scale bar 10 mm.

Plumadraco bankoorum. Specimen STM11−4 
(A) The holotype specimen of Plumadraco, (B) a closer view of the body and, (C) a line drawing of the same portion of the body shown in B. Well preserved bones are colored white, crushed or poorly preserved bones (or portions of bones) are grey, and preserved soft tissues are brown. The extent of the feather traces are denoted by the thin black outline around the body. Potential outline or crural feather present along the cranial face of the tibia.

Abbreviations: al, alula; cev, cervical vertebrae; co, coracoid; fm, femur; fu, furcula; hu, humerus; il, ilium; is, ischium; ma, manus; ph, phalanges (of the peds); pu, pubis; py, pygostyle; ri, rib(s); ra, radius; sc, scapula; sk, skull; sp, sternal plate; sy, synsacrum; tb, tibia; tmt, tarsometatarsus; tf, tail feathers; tv, thoracic vertebrae; ul, ulna. 

Scale bar (A, C) equals 50 mm.

Systematic paleontology

Aves Linnaeus, 1758

Pygostylia Chiappe et al., 2002  

Ornithothoraces Chiappe, 1995 

Enantiornithes Walker, 1981

Plumadraco bankoorum gen. et sp. nov.

Holotype. STM11−4 is a complete, articulated specimen preserved in a single slab primarily in dorsal aspect with feathers preserved around the head, body, wings, and tail.

Locality and horizon. Near Xiaotaizi Village, Jianchang County, Liaoning Province, Jiufotang Formation, 121 Ma (Lower Aptian). 

Diagnosis: Mid-sized [112–144 g, similar to some extant turdids (e.g., Cochoa, Turdus) and meliphagids (e.g., Anthochaera) enantiornithine (ventral margin of the furcula wider than dorsal margin; acrocoracoid, glenoid, and scapular cotyla omal-sternally aligned; minor metacarpal extending distally farther than the major metacarpal; metatarsal IV thinner than metatarsals II and III with the trochlea reduced to a single condyle; and a J-shaped metatarsal I), belonging to the family Bohaiornithidae (basally robust, apically tapered dentition; unforked dentary- surangular articulation; proportional width of the coracoid’s sternal margin; caudolateral projection of the sternal plate’s lateral trabeculae; well-developed abruptly terminating deltopectoral crest; robust pedal unguals), with the unique combination of the following features: corpus of the premaxillae dorsoventrally deeper than the dentaries; rostral ~80% of the dentary with parallel dorsal and ventral margins; tip of dentary is rostrodorsally tapered; at least nine sacral vertebrae; caudally-oriented lateral trabeculae of the sternum with asymmetrical, fan-shaped distal expansions; phalanx I of the manual digit craniocaudally thin; weakly curved pedal unguals; RDFs approximately twice body length.

Etymology. “Pluma”, Latin for feather, and “draco”, Latin for dragon. In the theme of avian biology and evolution, the specific name, “bankoorum”, honors Winston E. and Paul C. Banko. Together, their momentous life-long efforts have significantly contributed to our understanding of avian biology and conservation, particularly across the Hawaiian archipelago. Plumadraco bankoorum, the Banko’s feather dragon.

 B) Finely-preserved structures present in the proximal portion of the right RDF of Plumadraco bankoorum, C) and the preserved racket showing the differentiated barbs and the reduction, and eventual complete termination, of the central support structures (i.e., ramus and medial stripe). (D) The unique, undifferentiated barbs of the occipital plumes of Pteridophora alberti (King-of-Saxony Bird-of-Paradise) (FMNH 280831) forming tab-like laminated sheets. These structures may be uniquely analogous to the lateral margins (ribbon-like sheets) of enantiornithine RDFs preceding the distal ornaments.
 (E) An in-life restoration of Plumadraco. Illustration by Ville Sinkkonen.

  Results of phylogenetic analyses suggest Plumadraco belongs to the diverse Bohaiornithidae.

 

 male and female Plumadraco bankoorum

Illustration: Ville Sinkkonen

 Alexander D. Clark, Jingmai K. O’Connor, Xiaoli Wang, Yan Wang, Stephen Pruett-Jones, Xiangyu Zhang, Xing Wang, Xiaoting Zheng and Zhonghe Zhou. 2026. Hyperelongate Ornamental Tail Feathers in A New early Cretaceous enantiornithine Bird. PLoS One 21(5): e0347641. DOI: doi.org/10.1371/journal.pone.0347641 [May 27, 2026]

[Paleontology • 2026] Acutodon villeveyracensis • A New pan-shinisaur Lizard (Anguimorpha) from the lower Campanian of Villeveyrac (Hérault, France)

Acutodon villeveyracensis 

Jansen, Augé, Garcia, Otero & Valentin, 2026

DOI: doi.org/10.1080/02724634.2026.2636649 

Artwork by Olivier Jansen

ABSTRACT

The Chinese crocodile lizard (Anguimorpha, Pan-Shinisaurus Shinisaurus crocodilurus) is an endangered species inhabiting the lowland rainforests of southeastern China and northern Vietnam. The evolutionary history of this clade remains poorly understood, as only five fossil species and a few fossil specimens are described from the Lower Cretaceous of China and the Cenozoic of Europe and North America, revealing a considerable gap in the fossil record. A new anguimorph, Acutodon villeveyracensis gen. et sp. nov., is described from the lower Campanian (Upper Cretaceous) locality of Villeveyrac (Hérault, France), corresponding to a freshwater subtropical paleoenvironment. The species is attributed to a pan-shinisaur anguimorph based on a toothed maxilla sharing multiple characters with the extant Sh. crocodilurus and its fossil relatives, notably tall, tapered, and recurved teeth, with mesiodistally constricted tooth bases lacking basal infoldings but possessing medial resorption pits, and a posteromedially shifted anterior superior alveolar foramen. This Cretaceous record is the oldest in Europe for pan-shinisaur lizards. It pre-dates the occurrence of this clade in Europe by around 30 Myr, raising questions about the paleobiogeographic history of pan-shinisaur lizards.

Acutodon villeveyracensis holotype and unique material (UP.VIL.2010.55). Photographs, virtual reconstruction, and interpretative drawings of the maxilla in A, labial; B, lingual; C, occlusal; and D, dorsal views. Note that the posteriormost tooth was lost after CT scanning.

Abbreviations: asaf, anterior superior alveolar foramen; ce, cutting edge; cl, crista lateralis; ct, crista transversalis; fp, facial process; lf, labial foramina; lic, lamina intercristalis; lpp, lateral premaxillary process; lr, lacrimal recess; mpp, medial premaxillary process; ps, palatal shelf; rp, resorption pit; sds, supradental shelf. Scale bar equals 10 mm.

Details of the teeth of Acutodon villeveyracensis holotype and unique material (UP.VIL.2010.55) from the virtual reconstruction.
A, morphology in anterior view; B, section in median plane; C, section in horizontal plane.

Abbreviations: asaf, anterior superior alveolar foramen; c, cement; cl, crista lateralis; ct, crista transversalis; d, dentine; lf, labial foramen; lpp, lateral premaxillary process; m, maxilla; mpp, medial premaxillary process; ps, palatal shelf; t1–t4, teeth numbered from front to back. Scale bar equals 2 mm.

SQUAMATA Oppel, 1811

ANGUIMORPHA Fürbringer, 1900

PAN-SHINISAURUS sensu Smith and Gauthier, 2013

ACUTODON gen. nov.

ACUTODON VILLEVEYRACENSIS, gen. et sp. nov.

Diagnosis—Large anguimorph lizard characterized by the following combination of characters: the teeth are tall, thin, and possess a tapered apex; anterior teeth are strongly posteriorly recurved, but the most posterior teeth are straight; the teeth lack striations and basal infoldings; the base of the teeth expands lingually but is strongly anteroposteriorly compressed, and is covered in a thin layer of cementum; the crowns have a faint cutting edge, restricted to the most apical portion; medial resorption pits are ...

Etymology—‘acutus’ (Latin), sharp, pointed, piercing, and thin; ‘ὀδόντος’ (Greek), teeth; the genus name refers to the tapered, sharp, and thin teeth of this new genus; ‘villeveyracensis’ (Latin) from the locality of Villeveyrac, department of Hérault, France, where this new lizard taxon has been found.

Acutodon villeveyracensis
Paleoartistic reconstruction of the new genus and species of pan-shinisaur lizard from the lower Campanian of Villeveyrac (Hérault, France). Original artwork by Olivier Jansen.

Olivier Jansen, Marc Augé, Geraldine Garcia, Olga Otero and Xavier Valentin. 2026. A New pan-shinisaur Lizard (Anguimorpha) from the lower Campanian of Villeveyrac (Hérault, France). Journal of Vertebrate Paleontology. DOI: doi.org/10.1080/02724634.2026.2636649  [20 May 2026]

[Paleontology • 2026] Tylosaurus rex • A gigantic New Species of Tylosaurus (Squamata: Mosasauridae) from Texas: and A revised character list for phylogenetic analyses of Mosasauridae

Tylosaurus rex

Zietlow, Polcyn & Tykoski, 2026

 

hdl.handle.net/2246/7549 

 x.com/TyrantLzrdQueen

Abstract

At least four subfamily-level clades of mosasaurs are broadly recognized (Mosasaurinae, Plioplatecarpinae, Tylosaurinae, Halisaurinae), each of which independently evolved flippers and other aquatic adaptations, including large body size. Tylosaurine mosasaurs are distinguished from other mosasaurs, in part, by edentulous extensions of both upper and lower jaws, proportionally long tails, and poorly ossified limbs, and they were the first mosasaur clade to achieve gigantic (>8 m) body size. Several tylosaurine species are known from Europe, Asia, New Zealand, Africa, and Antarctica, but they were most common in the Western Interior Seaway of North America. Here, we describe a new species, Tylosaurus rex, sp. nov., from the Campanian of Texas and analyze tylosaurine in-group systematics using a significantly updated phylogenetic character list. Our new species is distinguished by a unique suite of characters, including some associated with increased jaw and neck musculature, and others that may be convergent with other giant mosasaur species (e.g., Mosasaurus). Body length estimates for specimens referred to our new species are consistently larger (7.7–13.2 m) than those for the largest Niobrara species, T. proriger (3.9–9.5 m), although it is unclear whether this is a taxonomic signal or taphonomic bias. Several specimens that we refer to T. rex were previously referred to T. proriger in various collections databases, and some of the traits distinguishing them had been previously attributed to ontogenetic differences. However, we rule out this possibility as specimens of T. proriger and T. rex that do overlap in size can be differentiated by unique suites of diagnostic characters. The implicit association between body size and ontogeny, as well as the general absence of reliable locality and stratigraphic data associated with historical collections of North American mosasaurs, raises the possibility of the presence of other currently unrecognized species, previously dismissed as ontogenetic stages of other species.

 

Keywords: Tylosaurus rex, Tylosaurus, Texas, Classification, Mosasauridae, Phylogeny 

The holotype for the newly described Tylosaurus rex is a giant specimen displayed at the Perot Museum of Nature and Science in Dallas that was first discovered in 1979.

 Perot Museum of Nature and Science

Tylosaurus rex, sp. nov.

A reconstruction of Tylosaurus rex in the Cretaceous-era Western Interior Seaway of North America

artwork by Alderon Games - Path of Titans

Zietlow, Amelia R.; Polcyn, Michael J. and Tykoski, Ronald S. 2026. A gigantic New Species of Tylosaurus (Squamata, Mosasauridae) from Texas: and A revised character list for phylogenetic analyses of Mosasauridae. Bulletin of the American Museum of Natural History. 482; DOI: 10.1206/0003-0090.482.1.1 https://hdl.handle.net/2246/7549

  x.com/TyrantLzrdQueen/status/2057493465521393765

[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 

Artwork by facebook.com/DinoThaiThai

 facebook.com: Perth Thitiwoot

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]

 facebook.com/perth.thitiwoot/posts/3901053680026079