Showing posts with label Liaoning. Show all posts
Showing posts with label Liaoning. Show all posts

Friday, May 29, 2026

[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 
 
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]

Wednesday, March 12, 2025

[Paleontology • 2025] Darwinopterus camposi • A New Species of Darwinopterus (Pterosauria: Wukongopteridae) from western Liaoning provides some new information on the Ontogeny of this clade

 

Darwinopterus camposi
Cheng, Jiang, Bantim, Sayão, Saraiva, Meng, Kellner & Wang, 2025
 

Abstract
The Wukongopteridae is an important pterosaur clade from the Yanliao Biota, combining features of basal and derived pterosaurs. So far, the Wukongopteridae consists of five species divided into three genera: Wukongopterus lii, Darwinopterus modularis, Darwinopterus linglongtaensis, Darwinopterus robustodens, and Kunpengopterus sinensis. Here we report a new species, Darwinopterus camposi sp. nov., based on an almost complete skeleton (IVPP V 17957). The new species is referred to Darwinopterus due to the presence of an elongated posterior region of the skull and the bony premaxillary crest that starts about the anterior margin of the nasoantorbital fenestra. It differs from all other wukongopterids by having the dorsal margin of the premaxillary crest straight, without an extensive dorsal projection and presenting a smooth lateral surface. Furthermore, D. camposi sp. nov. has eighteen and fourteen teeth on each side of the upper and lower jaws, respectively, and the fourth phalanx of the wing finger shorter than the first. IVPP V 17957 shows some fused postcranial bones, like the extensor tendon process to the first wing finger phalanx, but also has unfused premaxilla and frontal, which provides further information about wukongopterid ontogeny.

Key words: Pterosauria; Wukongopteridae; ontogeny; Yanliao Biota; Middle-Late Jurassic; China



SYSTEMATIC PALEONTOLOGY
Pterosauria Kaup 1834
Wukongopteridae Wang, Kellner, Jiang and Meng 2009

Darwinopterus Lü, Unwin, Jin, Liu and Ji 2010

Darwinopterus camposi sp. nov.

 Holotype: Almost complete skeleton lacking the distal end of the tail and hindlimbs, housed at the Institute of Vertebrate Paleontology and Paleoanthropology, Beijing, under the number IVPP V 17957 (Figs. 1-Fig. 4).

Etymology: In honor to Dr. Diogenes de Almeida Campos, an important geologist and vertebrate paleontologist who has contributed to pterosaur research and the cooperation between Brazilian and Chinese paleontologists.
 


Cheng, X.; Jiang, S.; Bantim, R. A. M.; Sayão, J. M.; Saraiva, A. Á. F.; Meng, X.; Kellner, A. W. A.; Wang, X. 2025. A New Species of Darwinopterus (Wukongopteridae, Pterosauria) from western Liaoning provides some new information on the Ontogeny of this clade. Anais da Academia Brasileira de Ciências. 97 (Suppl. 1). e20240707. DOI: doi.org/10.1590/0001-3765202520240707

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 


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

Wednesday, March 6, 2024

[PaleoOrnithology • 2024] Imparavis attenboroughi • First Edentulous Enantiornithine (Aves: Ornithothoraces) from the Lower Cretaceous Jehol Avifauna


Imparavis attenboroughi
  Wang, Clark, O'Connor, Zhang, Wang, Zheng & Zhou, 2024

Artwork: Ville Sinkkonen.

Abstract
Among Mesozoic birds, enantiornithines exhibit great morphological variation, which likely reflects their species diversity, range, and overall success throughout the Cretaceous. The majority of enantiornithines come from the Lower Cretaceous Jehol deposits (130–120 Ma) in northeastern China. In contrast to living birds, most enantiornithines were fully toothed. However, the rostral lengths, appendicular proportions, and pedal morphologies of extant birds can still inform on possible diet, flight mode, and ecology. Both partial (e.g., Longipterygidae) and complete tooth loss (e.g., Yuornis, Gobipteryx) are observed among enantiornithines, with edentulous rostra previously restricted to Upper Cretaceous taxa. Here, we describe the first edentulous enantiornithine from the Lower Cretaceous, Imparavis attenboroughi gen. et sp. nov., indicating a toothless beak evolved in this group 48 Ma earlier than previously recognized. Additionally, we reinterpret Chiappeavis as edentulous which together with the discovery of Imparavis indicates the complete loss of teeth in enantiornithines was not uncommon although still less frequent than observed in ornithuromorphs. The absence of gastroliths in all known enantiornithines suggests that the loss of teeth evolved under different pressures in these two ornithothoracine clades. Differences in rostral occlusion between Imparavis and Chiappeavis suggest they utilized different foraging strategies and possibly diet. Appendicular morphology in Imparavis suggest the capacity for relatively high wing beat frequency and powerful take-off capabilities. Together with the morphology of the hindlimb, we suggest Imparavis was primarily a terrestrial forager that could utilize sudden bursts of flight to escape into arboreal settings as a prey evasion strategy.

Illustration showing the fossil skeleton of Imparavis attenboroughi, alongside a reconstruction of the bird in life.
Artwork: Ville Sinkkonen.

Systematic paleontology
Aves Linnaeus, 1758
Pygostylia Chiappe, 2002

Ornithothoraces Chiappe, 1995
Enantiornithes Walker, 1981

Imparavis attenboroughi gen. et sp. nov.

Locality and horizon. Collected near the village of Toudaoyingzi, Jianchang County, Liaoning Province, PR China; Lower Cretaceous Jiufotang Formation, 120 Ma (Lower Aptian) (He et al., 2004; Pan et al., 2013).

Conclusions: 
Imparavis attenboroughi represents the first known edentulous enantiornithine from the Lower Cretaceous. The discovery of this taxon contributes to the multiple independent evolutionary occurrences of complete tooth loss among Mesozoic birds. The loss of teeth in enantiornithines may be linked to shifts in feeding behavior; however, as yet there is no evidence that this shift was driven by herbivory as is suggested for ornithuromorphs and non-avian dinosaurs. Rostral occlusion in Imparavis ....


Xiaoli Wang, Alexander D. Clark, Jingmai K. O'Connor, Xiangyu Zhang, Xing Wang, Xiaoting Zheng and Zhonghe Zhou. 2024. First Edentulous Enantiornithine (Aves: Ornithothoraces) from the Lower Cretaceous Jehol Avifauna. Cretaceous Research. 159, 105867. DOI: 10.1016/j.cretres.2024.105867
 

Saturday, December 23, 2023

[Paleontology • 2023] Meilifeilong youhao • A New toothless Pterosaur from the Early Cretaceous Jehol Biota with Comments on the Chaoyangopteridae


 Meilifeilong youhao  
Wang, Kellner, Jiang, Chen, Costa, Cheng, Zhang, Vila Nova, de Almeida Campos, Sayão, Rodrigues, Bantim, Saraiva & Zhou, 2023

artwork by Maurilio Oliveira

Abstract
The Chaoyangopteridae is a clade of azhdarchoid pterosaurs that stands out in China, particularly in the Jehol Biota, as a Cretaceous group of medium-sized and high-crested pterosaurs. Herein, we describe a new species, Meilifeilong youhao gen. et sp. nov., based on two specimens, one tentatively referred to this taxon. This new species represents the most complete and well-preserved chaoyangopterid recorded to date. Along with a set of characters (low premaxillary crest above the nasoantorbital fenestra extending posteriorly, posterior premaxillary process arched and curving posteriorly, a slightly convex sternal articulation surface of coracoid, and a fibular shaft close to proximal articulation strongly arched posteriorly), this species also provides new information both on the unknown palatal region of this clade, and on the rarely preserved (in place) ear portion with stapes. Moreover, M. youhao sheds light on paleoecological aspects, while also giving new information about the taxonomic diversity of this peculiar group of Jiufotang pterosaurs.

Systematic Paleontology
Pterosauria Kaup, 1834
Pterodactyloidea Plieninger, 1901

Dsungaripteroidea Young, 1964 sensu Kellner 2001, 2003
Azhdarchoidea Nessov 1984, sensu Kellner 2001, 2003

Chaoyangopteridae Lü et al. 2008

Photo (A) and line drawing (B) of the holotype (IVPP V 16059) of Meilifeilong youhao gen. et sp. nov. Arrows indicate preserved soft tissue.
 Abbreviations: at-ax, atlas-axis; cdv, caudal vertebra; cv, cervical vertebra; dca, distal syncarpal; dv, dorsal vertebrae; fe, femur; fi, fibula; gas, gastralia; hu, humerus; il, ilium; isc, ischium; man, mandible; mcI-IV, metacarpal I-IV; mt, metatarsal; obfo, obturator foramen.; paca, preaxial carpal; ph1-3d4, first to third phalanx of manual digit IV; phd 1–3, phalanx of the manual digit IIII; pphd, phalanx of the pedal digit; ppu, prepubis; prca, proximal syncarpal; ptd, pteroid; pu, pubis; ra, radius; ri, rib; sca-cor; scapulocoracoid; sk, skull; sv sacral vertebra; st, sternum; ta, tarsal; ti, tibia; ul, ulna; l, left; r, right.

 Meilifeilong youhao gen. et sp. nov.
Photo (A) and line drawing (B) of the cranial elements of the holotype (IVPP V 16059) 

Meilifeilong gen. nov.
Type species. Meilifeilong youhao.

Etymology. From the Chinese expressions meili—beautiful, fei—fly, and long—dragon, meaning beautiful flying dragon in allusion to the magnificent preservation of the holotype, IVPP V 16059.

Included species. Meilifeilong sanyainus comb. nov.

Diagnosis. Chaoyangopterid with low premaxillary crest above the nasoantorbital fenestra that extends posteriorly; posterior premaxillary process arched and curving posteriorly; humerus about 20% longer than third phalanx of the wing finger (hu/ph1d4 ~ 1.20).

Meilifeilong youhao sp. nov.

Etymology. Youhao, meaning friendship in mandarin, to celebrate the two-decade continuous collaboration between Chinese and Brazilian paleontologists in pterosaur research since 2003.

Holotype. IVPP V 16059, an almost complete skeleton housed at the Institute of Vertebrate Paleontology and Paleoanthropology (IVPP), Chinese Academy of Sciences, Beijing, China,

Horizon and locality. Xiaotaizi, Jianchang, Huludao City, western Liaoning China; Jiufotang Formation, Early Cretaceous (Barremian-Aptian).

Diagnosis. Chaoyangopterid pterosaur exhibiting the following autapomorphies: sternal articulation surface of coracoid slightly convex; fibular shaft close to proximal articulation strongly arched posteriorly. The new species can be further distinguished from Meilifeilong sanyainus by the following features: posterior premaxillary process more arched; jugal with lacrimal and postorbital processes at a narrower angle (~ 45° contra ~ 55° in Meilifeilong sanyainus); deeper mandibular symphysis; cervical vertebrae 5 slightly longer than cervical 4; rectangular sternum that is wider than long (square in Meilifeilong sanyainus); scapula comparatively longer relative to the coracoid, metatarsal III and IV proportionally shorter than metatarsals I and II.

 Meilifeilong youhao gen. et sp. nov.
artwork: Maurilio Oliveira

 
Xiaolin Wang, Alexander W. A. Kellner, Shunxing Jiang, He Chen, Fabiana R. Costa, Xin Cheng, Xinjun Zhang, Bruno C. Vila Nova, Diogenes de Almeida Campos, Juliana M. Sayão, Taissa Rodrigues, Renan A. M. Bantim, Antônio A. F. Saraiva and Zhonghe Zhou. 2023. A New toothless Pterosaur from the Early Cretaceous Jehol Biota with Comments on the Chaoyangopteridae. Scientific Reports. 3, 22642. DOI: 10.1038/s41598-023-48076-7

Thursday, June 29, 2023

[Arachnida • 2023] Pholcus xiuyan • Pholcid Spiders of the Pholcus phungiformes Species-group (Araneae: Pholcidae) from Liaoning Province, China: An Overview, with Description of A New Species

 

Pholcus xiuyan Zhao, Zheng & Yao,

in Zhao, Jiang, Yang, He, Zheng et Yao, 2023. 

Abstract
Species of the Pholcus phungiformes group exhibit high diversity in Liaoning Province of northeastern China. This paper summarizes the current knowledge on this species-group from this area. A checklist of 22 species recorded from this province is given, accompanied with a distribution map of the species. Pholcus xiuyan Zhao, Zheng & Yao, sp. nov. (♂♀) is described as new to science, and P. yuhuangshan Yao & Li, 2021 is reported from Liaoning for the first time.

Keywords: Biodiversity, daddy-long-legs spider, morphology, Northeast Asia, taxonomy


Pholcus xiuyan sp. nov., living specimens and habitat
A, B females and juveniles on rock walls C habitat, arrow indicates collecting site.

 Pholcus xiuyan Zhao, Zheng & Yao, sp. nov.
 
Remarks: This new species is assigned to the phungiformes group by the following combination of characters: the male chelicerae with frontal apophyses (arrow fa in Fig. 4D), the male palpal tibia with a prolatero-ventral projection (Fig. 3A), the procursus with dorsal spines (arrows in Fig. 3D), the uncus with a “pseudo-appendix” (arrow 2 in Fig. 4C), and the epigyne with a knob (Fig. 4A).


 Fangyu Zhao, Tian Jiang, Lan Yang, Qiaoqiao He, Guo Zheng and Zhiyuan Yao. 2023. Pholcid Spiders of the Pholcus phungiformes Species-group (Araneae, Pholcidae) from Liaoning Province, China: An Overview, with Description of A New Species. ZooKeys. 1156: 1-14. DOI:  10.3897/zookeys.1156.98331

Wednesday, June 14, 2023

[Paleontology • 2023] Wulong bohaiensis • Iridescent Plumage in A juvenile dromaeosaurid Theropod Dinosaur


Wulong bohaiensis  Poust, Gao, Varricchio, Wu & Zhang, 2020

in Croudace, Shen, Lü, Brusatte eVinther, 2023. 
Artwork by Robert Nicholls (Bob Nicholls Art).

Colour reconstructions have provided new insights into the lives of dinosaurs and other extinct animals, by predicting colouration patterns from fossilised pigment-bearing organelles called melanosomes. Although these methods have become increasingly popular, only a small number of dinosaurs have been studied using these techniques, which require exceptional preservation of fossil feathers, leaving open key questions such as whether dinosaurs changed their plumage patterns during ontogeny. Here we reconstruct the feather colouration of an approximately one-year-old individual of the Early Cretaceous dromaeosaurid theropod Wulong bohaiensis, which to our knowledge is the first unequivocal juvenile paravian for which aspects of the original colour has been predicted. Using quadratic discriminant analysis (QDA) and multinomial logistic regression (MLR) on the most comprehensive available datasets, we find strong evidence for iridescent plumage of the forelimb and hindlimb remiges and grey plumage on other portions of the body. This suggests that some juvenile paravians used shiny iridescent feathers for signalling purposes, possibly even before reaching somatic or sexual maturity, and thus we can conclude that this paravian used iridescent signalling for intraspecific communication other than sexual signalling. Finally, our results show that when analysing fossil datasets that are entirely comprised of solid and cylindrical melanosomes QDA consistently outperforms MLR, providing more accurate and higher classification probability colour predictions.

Key words: Dinosauria, Dromaeosauridae, Paraves, Wulong bohaiensis , iridescence, melanosome, palaeocolour, juvenile, colour reconstruction, Cretaceous, China.

Reconstruction of the dromaeosaurid dinosaur Wulong bohaiensis Poust, Gao, Varricchio, Wu, and Zhang, 2020 (DNHM D2933),
from Shangheshou, Chaoyang, Liaoning, China, Early Cretaceous Jiufotang Formation with a minimum age of 120.3Ma.
This illustration broadly depicts iridescent plumage on the limbs and grey feathers on the body. It should be noted that the full extent of the iridescence has been extrapolated in the creation of this illustration, based on the evidence provided by a small but significant distribution of iridescent samples across several limbs of the fossil.
Artwork by Robert Nicholls (Bob Nicholls Art).

 
Angus D. Croudace, Caizhi Shen, Junchang Lü, Stephen L. Brusatte and Jakob Vinther. 2023. Iridescent Plumage in A juvenile dromaeosaurid Theropod Dinosaur. Acta Palaeontologica Polonica.  in press. https://app.pan.pl/article/item/app010042022.html
DOI: 10.4202/app.01004.2022


Wednesday, August 10, 2022

[Paleontology • 2022] Reappraisal of the largest ctenochasmatid Moganopterus zhuiana et al. 2012 (Pterosauria: Ctenochasmatidae)


Moganopterus zhuiana Lü et al., 2012 

in Gao, Jiang, Xu, et al., 2022. 

Moganopterus zhuiana Lü et al., 2012 was erected as a member of the Boreopteridae, which was questioned by different researchers shortly after the publication. Although the new assignment to the Ctenochasmatidae is widely accepted by pterosaur researchers, some characteristics still require a detailed description. Here, the holotype of this taxon is restudied, and some ambiguous characteristics are re-identified. The diagnosis of this taxon has been revised as the following: a large ctenochasmatid pterosaur, which can be distinguished from other members of this clade by a single autapomorphy: an elongated rod-like parietal crest that extends posterodorsally, forming an angle of about 15° with the ventral margin of the skull. This taxon can be further distinguished from other ctenochasmatids on the basis of the following combination of characteristics: straight occlusal surfaces of the upper and low jaws; presence of a low premaxillary crest confined anterior to the nasoantorbital fenestra; rostrum about two thirds of the skull length; nasoantorbital fenestra occupying slightly more than 20% of the skull length; about 100 slender teeth; and a mid-cervical length/width ratio of about 7. The wingspan of M. zhuiana has been re-estimated according to a simple regression equation for wingspan versus skull length in ctenochasmatids. It confirms that M. zhuiana, although smaller than previous thought, is still the largest known ctenochasmatid. When comparing the sizes of ctenochasmatids in the Jurassic and Cretaceous, ctenochasmatids showed a rough tendency to increase their sizes.

Key words: Liaoning, Jiufotang Formation, Moganopterus zhuiana, largest ctenochasmatid


Photographs and reconstruction of the holotype of Moganopterus zhuiana (HGM 41HIII-0419) from Jianchang, Liaoning
A. slab A; B. slab B; C. the reconstruction of the upper and lower jaws.



GAO Dian-Song, JIANG Shun-Xing, XU Li, CHENG Xin, YANG Li-Li, JIA Song-Hai and WANG Xiao-Lin. 2022. Reappraisal of the largest ctenochasmatid Moganopterus zhuiana Lü et al., 2012. VERTEBRATA PALASIATICA. 60(3); 197-211. vertpala.ac.cn/EN/10.19615/j.cnki.2096-9899.220111
 DOI: 10.19615/j.cnki.2096-9899.220111
http://www.vertpala.ac.cn/EN/2096-9899/home.shtml

   

摘要:朱氏莫干翼龙(Moganopterus zhuiana)由吕君昌等于2012年建立,并将其归入北方翼龙科(Boreopteridae), 这一分类在发表后不久就受到了不同研究者的质疑。之后,尽管关于莫干翼龙归入梳颌翼龙科(Ctenochasmatidae)的观点已被大部分翼龙研究者所接受,但是很多特征还需要详细的描述。通过对朱氏莫干翼龙的正型标本进行详细观察,对一些较为模糊的特征进行了重新确认。将其鉴定特征修改为:一种大型的梳颌翼龙类成员,具有一个与其他成员不同的自有裔征——一长棍状额骨嵴向后背侧延伸,并与头骨腹面形成15°夹角。同时莫干翼龙还具有以下的特征组合可以区别于其他梳颌翼龙类成员:平直的上下颌咬合面;低矮的前上颌骨嵴位于鼻眶前孔之前;吻端约占头骨长度的2/3; 鼻眶前孔占头骨长度略大于20%; 100枚细长的牙齿;中部颈椎的长宽比约为7。依据梳颌翼龙类翼展和头骨长度的线性关系,重新推测了莫干翼龙的翼展。新的推测结果证实,虽然比最初推测的小了很多,但莫干翼龙仍然是已知的个体最大的梳颌翼龙类成员。对比侏罗纪和白垩纪的梳颌翼龙类,这一种类的体型大致存在一个增大的趋势。

关键词: 辽宁, 九佛堂组, 朱氏莫干翼龙, 最大的梳颌翼龙类

Lü Junchang; Pu Hanyong; Xu Li; Wu Yanhua; Wei Xuefang (2012). "Largest Toothed Pterosaur Skull from the Early Cretaceous Yixian Formation of Western Liaoning, China, with Comments On the Family Boreopteridae". Acta Geologica Sinica. 86 (2): 287–293. DOI: 10.1111/j.1755-6724.2012.00658.x

Saturday, December 18, 2021

[PaleoOrnithology • 2021] Brevirostruavis macrohyoideus • Novel Evolution of A Hyper-elongated Tongue in A Cretaceous Enantiornithine from China and the Evolution of the Hyolingual Apparatus and Feeding in Birds


Brevirostruavis macrohyoideus
Li, Wang, Stidham, Zhou & Clarke, 2021

 
Abstract
The globally distributed extinct clade Enantiornithes comprises the most diverse early radiation of birds in the Mesozoic with species exhibiting a wide range of body sizes, morphologies, and ecologies. The fossil of a new enantiornithine birdBrevirostruavis macrohyoideus gen. et sp. nov., from the Lower Cretaceous Jiufotang Formation in Liaoning Province, northeastern China, preserves a few important skeletal features previously unknown among early stem and extant birds, including an extremely elongate bony hyoid element (only slightly shorter than the skull), combined with a short cranial rostrum. The long hyoid provides direct evidence for the evolution of specialized feeding in this extinct species, and appears similar to the highly mobile tongue that is mobilized by the paired epibranchials present in living hummingbirds, honeyeaters, and woodpeckers. The likely linkage between food acquisition and tongue protrusion might have been a key factor in the independent evolution of particularly elongate hyobranchials in early birds.


Aves Linnaeus, 1758. 
Enantiornithes Walker, 1981. 

Photograph and line drawing of the skull of the holotype specimen of  Brevirostruavis macrohyoideus (IVPP V13266).

Brevirostruavis macrohyoideus gen. et sp. nov. 

Etymology: The genus name refers to its short rostrum (and bird), and the specific epithet refers to the particularly long hyoid apparatus

Locality and horizon: Xiaotaizi Village, Jianchang County, Liaoning Province, China; Jiufotang Formation, Lower Cretaceous. Age approximately 120 Ma (He et al., 2004).


 Brevirostruavis macrohyoideus with its mouth open to show its long tongue that was used to catch insects or obtain nectar from cone-bearing plants


Zhiheng Li, Min Wang, Thomas A. Stidham, Zhonghe Zhou and Julia Clarke. 2021. Novel Evolution of A Hyper-elongated Tongue in A Cretaceous Enantiornithine from China and the Evolution of the Hyolingual Apparatus and Feeding in Birds. Journal of Anatomy. DOI: 10.1111/joa.13588