Showing posts with label PaleoIchthyology. Show all posts
Showing posts with label PaleoIchthyology. Show all posts

Saturday, October 17, 2026

[PaleoIchthyology • 2022] Dianodipterus huizeensis • A New dipnoan Genus (Sarcopterygii: Dipnoi) from the Middle Devonian of Huize, Yunnan, China


Dianodipterus huizeensis
Luo, Cui, Qiao & Zhu, 2022

 
Abstract
A new genus and species of tooth-plated lungfishes, Dianodipterus huizeensis gen. et sp. nov., is described from the Qujing Formation (late Eifelian, Middle Devonian) of Huize County, Qujing, north-eastern Yunnan, China. It differs from other lungfishes in the small proportion of the tooth-bearing part on the pterygoid (less than one-quarter), the extensively developed anteromedial edentulous portion of the pterygoid, and tooth rows few in number (only four). Phylogenetic analysis reveals that Dianodipterus is more plesiomorphic than Dipterus, yet crownward of Melanognathus. As the ninth Devonian lungfish genus from China, the new taxon displays a novel schema of lungfish dentition and increases the diversity of early lungfishes.

Keywords: Dipnoi, Middle Devonian, dentition, vomer, phylogeny, China


Dianodipterus huizeensis gen. et sp. nov.



Yanchao Luo, Xindong Cui, Tuo Qiao and Min Zhu. 2022. A New dipnoan Genus from the Middle Devonian of Huize, Yunnan, China. Journal of Systematic Palaeontology. 19(18); 1303-1315 DOI: doi.org/0.1080/14772019.2022.2042409 [29 Mar 2022]
x.com/ChinaScience/status/1514136308083412994

Friday, October 16, 2026

[PaleoIchthyology • 2026] Talentichthys kuragh • A new Devonian lungfish (Dipnoi: Holodontidae) from the western Karakoram of northern Pakistan


Talentichthys kuragh 
Young & Lu, 2026


Abstract
A well-preserved sarcopterygian fish skull from the Famennian (Upper Devonian) Shogrãm Formation, of the Chitral region, northern Pakistan, is described. Collected as a calcareous nodule by J.A. Talent and colleagues, it has been investigated using high-resolution computed tomography to reveal the internal cranial architecture. It represents a new genus and species of tooth-plated, cosmine-covered dipnoan (lungfish), Talentichthys kuragh n. gen. n. sp., distinguished from all previously described Devonian dipnoans by its deep nasal notches, elongate narrow subnasal ridge, and uniquely shaped olfactory cavities. Additional specimens from the type locality, showing additional aspects of morphology, will be necessary to clarify the phylogenetic position of the new form within the Dipnoi.

Keywords: Devonian lungfish; Dipnoi; Talentichthys; Famennian; northern Pakistan

ANU V3736, holotype of Talentichthys kuragh n. gen. n. sp., the anterior portion of a lungfish skull preserved in calcareous matrix.
(A) Dorsal view. (B) Ventral view. (C) Anterior view.
ioc, infraorbital sensory canal; ri, dentine ridge; ?ri, broken possible lateral dentine ridge; snr, subnasal ridge; soc, supraorbital sensory canal; t, tooth; TP, tooth-plate.

Systematic palaeontology
Class Osteichthyes Huxley, 1880
Subclass Sarcopterygii Romer, 1955

Superdivision Dipnomorpha Ahlberg, 1991
Division Dipnoi Müller, 1845
Family Holodontidae Gorizdro-Kulczyzka, 1950

Genus Talentichthys n. gen.

Etymology: The generic name commemorates Professor John Talent, with -ichthys (Gk) for fish.
 
Diagnosis: A tooth-plated, cosmine-covered dipnoan with deep notches for the anterior (incurrent) nares, elongate subnasal ridges, and the nasal cavity subdivided dorsally into a posteromesial reniform recess, and an anterolateral subdivision elongated rostrocaudally that extends as a groove to the nasal notch.

Remarks: The new taxon is represented by only one incomplete anterior skull portion, which displays nasal notches in the upper mouth margin, a long and deep nasal groove, prominent subnasal ridge and a pterygoid tooth plate. These features demonstrate dipnoan affinity, and are not consistent with porolepiforms, the other major dipnomorph subgroup, in which cosmine-covered forms are predominantly of Early Devonian age. We provisionally refer Talentichthys n. gen. to the family Holodontidae, based on the updated diagnosis and comprehensive review of the family provided by Long (2010). Although very incomplete, our new taxon displays features not shown in any previously described dipnoan. Further material from the Karakoram type area (currently inaccessible) will clarify the relationships of the new taxon.

Talentichthys kuragh n. gen. n. sp.

Etymology: The specific epithet is the local term ‘Kurãgh’ from the name of the stratigraphic section of Talent et al. (1999) which produced the specimen.
 
Locality and horizon: Collected from about 63 m above the base of the Kurãgh Spur stratigraphic section of Talent et al. (1999), about 55 km northeast of Chitral, northern Pakistan (Fig. 1), within the Upper Devonian (Famennian) Shogrãm Formation.

Holotype: ANU V3736, the only known specimen (ANU Department of Materials Physics, Research School of Physics, Canberra).


 Gavin C. Young and Jing Lu. 2026. A new Devonian lungfish from the western Karakoram of northern Pakistan. Palaeoworld. 35(5): 201130. DOI: doi.org/10.1016/j.palwor.2026.201130  [2026-10-09]

“喜马拉雅化石骗局”的回响——西喀喇昆仑泥盆纪肺鱼新知

Wednesday, October 14, 2026

[PaleoIchthyology • 2026] Yipetalichthys maxiongensis • A New quasipetalichthyid placoderm from the Middle Devonian of China

 

 Yipetalichthys maxiongensis
 Pan, Dupret, Ahlberg, Zhao, Wang, Wang & Zhu, 2026


Abstract
We describe Yipetalichthys maxiongensis gen. et sp. nov., a quasipetalichthyid placoderm from the Eifelian Shangshuanghe Formation (Qujing, Yunnan, China). High-resolution micro-CT reveals an endocranium bearing cranial nerve grooves and inner ear structures. The dermal neck joint permits a quantitative character, the angle between the ventral laminar ridge (v.l.r) and the skull-roof midline. Current specimens yield two non-overlapping bins (state 0: ≤15°; state 1: ≥28°), separating Macropetalichthyidae and Quasipetalichthyidae; the 15–28° interval is unsampled and the threshold remains testable with new material. Expanded parsimony analysis, adding Yipetalichthys and six additional ptyctodont taxa, recovers Petalichthyida as sister to Ptyctodontida and places Yipetalichthys within Quasipetalichthyidae. The diagnosis includes large unenclosed elliptical orbits, slender unbifid postorbital processes, an elongate occipital region, and a shallow posterolateral vagus canal. Yipetalichthys shows a high v.l.r angle, supporting its quasipetalichthyid placement and providing a reproducible metric for future comparisons across articulated specimens. Our analysis of the neck joint helps to clarify petalichthyid phylogeny and identifies distinct, recurring architectures among major placoderm groups: in Antiarcha, a reverse sliding joint; in Petalichthyida, an elaborate sliding joint guided by the ventral laminar ridge with laminar cranial articular facets forming a longitudinal sliding track opposing the articular flanges of the anterior dorsolateral plate (ADL); in Ptyctodontida, a sliding joint with spoon-shaped cranial articular facets opposing ADL articular flanges; in Actinolepidoidei, a simple sliding condition; in Brachythoraci, a ginglymoid joint. These distinct neck joint architectures demonstrate the high evolutionary plasticity of this structure and its multiple, independent pathways toward cranial mobility in placoderms.


Yipetalichthys maxiongensis gen. et sp. nov.




 
Zhaohui Pan, Vincent Dupret, Per E. Ahlberg, Wenjin Zhao, Jianhua Wang, Mengjun Wang and Min Zhu. 2026. A New quasipetalichthyid placoderm from the Middle Devonian of China. Papers in Palaeontology. DOI: doi.org/10.1002/spp2.70124 [24 September 2026] 

DeepBone团队发现瓣甲鱼新属种,揭示颈胸关节演化新线索


Thursday, September 3, 2026

[PaleoIchthyology • 2026] Nazaria limnica • A New deep bodied ray-finned fish (Osteichthyes: Actinopterygii) from the Permian Pedra do Fogo Formation (Northeastern Brazil) and its phylogenetic and paleogeographic affinities


Nazaria limnica
Richter, Cisneros, Kammerer, Pardo, Marsicano, Fröbisch, Smith & Angielczyk, 2026

Artwork by Juan C. Cisneros & Martha Richter

ABSTRACT
A deep bodied ray-finned fish is reported from Cisuralian lacustrine deposits of the Parnaíba Basin. Its ecological niche and systematic affinities are discussed, considering the paleogeographic distribution of selected Permo-Carboniferous deep bodied fishes from several separate sedimentary successions of western Gondwana. The occurrence of deep bodied fishes in the Parnaíba Basin mirrors the presence of a similarly shaped but less derived and distantly related taxon, Paranaichthys longianalis from the late Permian of the Paraná Basin of southern Brazil. The new taxon’s unique combination of characters includes an elongated pectoral fin; posteriorly inclined suspensorium; deep flank scales ornamented with fine vertical striae, tiny mandibular teeth and palatal crushing dental plates. It shares with Guildayichthys and Discoserra two preopercular bones, a supraorbital, and marginal teeth on the lower jaw. Phylogenetic analyses were performed based on two datasets. Dataset 1 included 53 characters coded for 26 deep bodied and fusiform fish fossils from Brazil, North America, China, South Africa, and Australia, with results indicating that is most closely related to the North American order Guildayichthyformes, known from marine rocks of Pennsylvanian age. Dataset 2 included 119 taxa coded for 293 characters. The two analyses place the new taxon as the sister group of a clade comprised of Blourugia and Paranaichthys. However, the results of the study of both datasets show a high degree of uncertainty about the interrelationships between the new taxon and other deep bodied Paleozoic fish species.

SYSTEMATIC PALEONTOLOGY
OSTEICHTHYES Huxley, 1880
ACTINOPTERYGII Cope, 1887

NAZARIA, gen. nov.
 
Etymology—Named after the municipality of Nazária in the State of Piauí, where the fossils were collected.

NAZARIA LIMNICA, gen. et sp. nov.

Etymology—Derives from the Greek epithet limne (‘lake’) a reference to the lacustrine paleoenvironment where the fishes lived.

Nazaria limnica, MAP PV1029 (holotype).
A, part; B, counterpart (reversed). The caudal and anal fins are not preserved in the holotype.
Abbreviations: vrs, ventral ridge scales.

Nazaria limnica, MAP PV1029 (holotype).
A, skull and anterior part of the trunk (dorsal crest not figured here); B, identification of skull bones as preserved in A and, augmented drawing of one of the anteriormost trunk scales, showing its vertical ornamental ridges and dorsal of the peg-and-socket articulation system. The hatched lines indicate uncertain bone boundaries.
Abbreviations: An, angular; a.In, anterior infraorbital; br, branchiostegal rays; Cl, cleithrum; Cla, clavicle; De, dentary; Dro, dorsal rostral; Dsp, dermosphenotic; Ent?, impression of an entopterygoid?; Ex, extrascapulars; Fr, frontal; Ju, jugal; mt, mandibular teeth; Mx, maxilla; Na, nasal; Op, operculum; Pa, parietal; Pmx-ant, premaxilla-antorbital; Pop1, preoperculum 1; Pop2, preoperculum 2; Psp, post-spiracular; Sco, scapulocoracoid; So, suborbitals; Sop, suboperculum; St, supratemporal; Su, supraorbital; Vo, vomer; VRo, ventral rostral.

 Nazaria limnica, MAP PV1029 (holotype).
A, detail of the mouth and surrounding region; B, details of the dentition.
 Abbreviations: maxt?, possible maxillary crushing teeth; mt, mandibular marginal teeth; Mx, maxilla; Vo, vomer (vomerine tooth plate).

Tentative reconstruction of the skull pattern and anteriormost flank scales of Nazaria limnica, based on MAP PV1029 (holotype), after rearrangement of some taphonomically dislocated bones (jugal, lachrymal and ventral preopercular). Short, dotted lines represent inferred bone limits (preoperculum, suboperculum, and ventral limit of the suprachleithrum). The inset features the skull sensorial line pattern.
Abbreviations: An, angular; a.In, anterior infraorbital; app, anterior process of parasphenoid; asp, posterior ascending process of parasphenoid; br, branchiostegal rays; Cl, cleithrum; Cla, clavicle; Dro, dorsal rostral; Dsp, dermosphenotic; Ent?, impression of an entopterygoid?; Ex, extrascapulars; Fr, frontal; Ju, jugal; Mx, maxilla; Na, nasal; Op, operculum; P1, pectoral fin; Pa, parietal; Par, parasphenoid; Pmx-ant, premaxilla-antorbital; Pop1, preoperculum 1; Pop2, preoperculum 2; Psp, post-spiracular; Sco, scapulocoracoid; So, suborbitals; Sop, suboperculum; sr, sclerotic ring; St, supratemporal; Su, supraorbital; Vo, vomer; Vro, ventral rostral.


Life reconstruction of Nazaria limnica, based on a composite rendering of characters observed on either the holotype, the paratype or both.
Art by Juan C. Cisneros based on Martha Richter reconstruction.

 
Martha Richter, Juan C. Cisneros, Christian F. Kammerer, Jason D. Pardo, Claudia A. Marsicano, Jörg Fröbisch, Roger M. H. Smith and Kenneth D. Angielczyk. 2026. A New deep bodied ray-finned fish (Osteichthyes/Actinopterygii) from the Permian Pedra do Fogo Formation (Northeastern Brazil) and its phylogenetic and paleogeographic affinities. Journal of Vertebrate Paleontology. e2697805. DOI: doi.org/10.1080/02724634.2026.2697805 [26 Aug 2026]

Tuesday, August 18, 2026

[PaleoIchthyology • 2026] Bataspis crux • A galeaspid (jawless stem gnathostome) from the Lochkovian of Yunnan with a batwing-shaped head adapted for hydrodynamic efficiency

 

Bataspis crux
Meng, Ferrón, Pisani, Gai & Donoghue, 2026 

Life restoration by Dinghua Yang.

Abstract
Galeaspids are an extinct group of jawless fishes from the Silurian–Devonian of China and northern Vietnam that are key to understanding the origin of vertebrate anatomical innovations. A new eugaleaspid, Bataspis crux gen. et sp. nov., is described based on fossil material from the Lochkovian (Early Devonian) Xishancun Formation of Qujing, Yunnan, China. Bataspis crux possesses a suite of unusual features, especially its bat-wing-like cornual processes that are seamlessly integrated with a brim-like rostral margin without a rostral process, constituting a unique morphology for galeaspids. Maximum parsimony, maximum likelihood and Bayesian phylogenetic inference all support membership in the family Tridensaspidae. We employed computational fluid dynamics to infer the hydrodynamic properties of the headshield of B. crux. Our analysis reveals that this species achieves an exceptionally high lift-to-drag ratio; the highest recorded among known galeaspids. This remarkable efficiency stems from its low drag across various angles of attack, coupled with passive lift generation through the exploitation of the Bernoulli effect by the airfoil cross-section of the cornual processes. This suggests that the species was an effective gliding cruiser, outperforming not only galeaspids but also other stem gnathostomes, such as osteostracans and pteraspidomorphs. These results provide new insights into our understanding of the evolution of Tridensaspidae, the ecological habits of stem gnathostomes and convergence in the evolutionary assembly of the gnathostome bodyplan.

Keywords: galeaspid, phylogenetic analysis, hydrodynamic analysis, lift-to-drag ratio, convergence, morphological function

Bataspis crux, holotype, IVPP V30969: A, internal mould in dorsal view; B, external mould in ventral view.
Abbreviations: c, cornual process; dcm, dorsal commissure; ic, inner cornual process; ifc, infraorbital canal; ldc, lateral dorsal canal; ltc, lateral transverse canal; mdc, median dorsal canal; md.o, median dorsal opening; orb, orbital opening; pi, pineal opening; se, serrated edge; soc2, posterior supraorbital canal; v.mtc, vestige of the median transverse canal; vr, ventral rim.
 All scale bars represent 1 cm.


SYSTEMATIC PALAEONTOLOGY

Subphylum VERTEBRATA-CRANIATA Linnaeus 1758
Infraphylum GNATHOSTOMATA Cope 1889
Subclass GALEASPIDA Tarlo 1967

Order EUGALEASPIFORMES (Liu 1965) Liu 1980

Family TRIDENSASPIDAE Liu 1986

Genus Bataspis nov.
 
Derivation of name: Bat from English, the shape of the cornual processes of Bataspis is similar to the membranous wings in bats.

Type species: Bataspis crux sp. nov.

Differential diagnosis: Bataspis is assigned to Eugaleaspiformes because it exhibits a suite of diagnostic features in morphology: subtriangular headshield with cornual and inner cornual processes, slit-like median dorsal opening, and typical eugaleaspid-type sensory canals. Although Bataspis lacks a rostral angle or process, its diagnostic specialized laterally-projecting processes suggest it differs from the members of Shuyuidae, Sinogaleaspidae, and Eugaleaspidae and can be assigned to Tridensaspidae. Compared with other members of Tridensaspidae, the absence of the rostral angle and the presence of vestiges of the median transverse canal distinguish Bataspis and Falxcornus; the lack of the rostral process constitute a diagnostic difference between Bataspis and the sister group including Pterogonaspis and Tridensaspis. Additionally, Bataspis contains serrations along with the margin connecting the cornual and inner cornual processes and the lateral margins of the median dorsal opening that differ from Falxcornus.


Bataspis crux sp. nov.
 
Derivation of name: The verb ‘to cruise’, in the sense of ‘to move from one side to the other’, is derived (via Norse and Old English) from the Latin crux (cross).

Holotype: A nearly complete headshield and its counterpart, IVPP V30969 (Fig. 1A–B).

Locality & horizon: Near the Qujing Maternal and Child Health Care Hospital Qilin District, Qujing City, Yunnan Province, Xishancun Formation, Cuifengshan Group, Lochkovian, Early Devonian.

Diagnosis: Medium-sized tridensaspid fish; subtriangular headshield; arcuate rostral margin without rostral angle and process; cornual process spine-like, projecting posterolaterally; lobular inner cornual process projecting posteriorly, slightly stronger than cornual process; the angle between the cornual and inner cornual processes exceeding 90° (sickle-like); margin of the headshield connecting the cornual and inner cornual processes serrated; median dorsal opening slit-like (length/width >6) with nearly parallel lateral serrated margins, the posterior margin almost level with the centra of the orbital openings, and its middle part convex forward; orbital opening large, round, and dorsally positioned; pineal opening small, round, beyond the posterior margin of the orbital opening; sensory canal system typical eugaleaspid-type, with three pairs of lateral transverse canals and vestiges of the median transverse canal.

Artistic life restoration of Bataspis crux.
Artwork by Dinghua Yang.

CONCLUSION: 
We describe Bataspis crux, a new species of galeaspid from Xishancun Formation in the Early Devonian (Lochkovian age) of Yunnan, China. Our phylogenetic analyses ally the new genus to the family Tridensaspidae, sister to the clade of Pterogonaspis and Tridensaspis, and sharing with Falxcornus the status as the oldest known tridensaspids. The results of probabilistic phylogenetic methods indicate that more data are needed to clarify the phylogenetic relationships of galeaspids such as the family Shuyuidae. Bataspis crux extends beyond the range of phenotypic variation known previously for galeaspids. The unique morphological features of this bat-like jawless fish result in a high lift-to-drag ratio when at low angles of attack. Our results reveal the breadth of locomotor capabilities available to galeaspids and other jawless stem-gnathostomes, demonstrating that an absence of flexible paired fins was not an impediment to ecological diversity.


Xinyuan Meng, Humberto G. Ferrón, Davide Pisani, Zhikun Gai and Philip C. J. Donoghue. 2026. Bataspis crux, a galeaspid (jawless stem gnathostome) from the Lochkovian of Yunnan with a batwing-shaped head adapted for hydrodynamic efficiency. Palaeontology.  DOI: doi.org/10.1111/pala.70081 [04 August 2026]


Friday, August 14, 2026

[PaleoIchthyology • 2026] Parastylephorus anatoides • A New fossil from the Eocene of Iran provides new insights regarding the evolution of the morphologically bizarre tube-eye fish

 

Parastylephorus anatoides 
Ridolfi, Schrøder, Bahrami, Yazdi, Roa-Varón, Marramà & Carnevale, 2026
 
Artwork by Lucrezia Bonardo

Abstract
Stylephoriformes are a morphologically bizarre lineage of deep-sea fishes, currently represented by a single extant species, Stylephorus chordatus, the so-called tube-eye fish. The phylogenetic relationships of the Stylephoriformes were extensively debated until recent genomic studies proposed a sister-group relationship with the Gadiformes. The tube-eye fish exhibits a suite of highly derived features, including extreme cranial kinesis, a pipette-like oral apparatus specialized for suction feeding, and an elongate, naked ribbon-like body lacking scales. The evolutionary origin of these unique traits is largely unknown, in part due to the complete absence of a fossil record. Here, we describe the first-known fossil of the order Stylephoriformes, from Bartonian (c. 40 Ma) sediments of the Pabdeh Formation, Iran. On the basis of several unique morphological features (edentulous premaxillae and dentary, moderately enlarged pterygoid elements, reduced opercle, elongate ribbon-like body comprising more than 63 vertebrae, eight pectoral-fin rays, absence of basipterygia, and the presence of a complete series of well-developed lateral-line scales) the specimen is assigned to a new genus and species: Parastylephorus anatoides. The fossil exhibits a body physiognomy, oral apparatus and cranial architecture remarkably similar to those of the extant tube-eye, with the most derived features already present and closely comparable in morphology. This suggests that the new fossil represents a good example of long-term morphological stasis among marine teleosts, documenting the persistence of a highly specialized body plan for more than 40 myr.

Keywords: Parastylephorus anatoides, Bartonian, Iran, Pabdeh Formation, Paracanthopterygii

Parastylephorus anatoides gen. et sp. nov., holotype, IUGM 100897, from the Eocene of Babaheydar (Iran). Scale bar represents 10 mm.


SYSTEMATIC PALAEONTOLOGY

Order STYLEPHORIFORMES sensu Miya et al. 2007
Family STYLEPHORIDAE Swainson 1839

Genus Parastylephorus nov.
 
Derivation of name: The genus name is derived from the Greek prefix para- (παρά), meaning ‘near’, combined with Stylephorus, the name of the only currently recognized stylephoriform genus. The name reflects the shared morphological characteristics with Stylephorus.
 
Remarks: As discussed above, the Stylephoriformes are a lineage currently represented by a single extant species, Stylephorus chordatus, which possesses a number of highly derived anatomical features, including a strongly modified buccal apparatus, extremely reduced first two vertebral centra, and a continuous dorsal fin along the entire dorsal margin of the body. The body plan of Parastylephorus gen. nov. closely resembles that of Stylephorus, although it has a set of distinctive traits. These include the maxilla with a well-developed posterior process, the expanded metapterygoid and ectopterygoid, and the reduced size of the opercular bones. In addition, Parastylephorus gen. nov. possesses body squamation, consisting of thin and delicate lateral-line scales, which are completely absent in Stylephorus.


Parastylephorus anatoides sp. nov.
 
Derivation of name: The name is derived from the Latin word Anas, meaning ‘duck’, and the Greek suffix -oides (-οειδής) meaning ‘resembling’ or ‘having the form of’.

Holotype: IUGM 100897 a partially preserved specimen on a single plate 
 
Artistic reconstruction of Parastylephorus anatoides gen. et sp. nov. 
Note that the tubular eyes are based on the condition characteristic of the extant Stylephorus chordatus. 
Artwork by Lucrezia Bonardo.


Lorenzo Ridolfi, Ane Elise Schrøder, Ali Bahrami, Mehdi Yazdi, Adela Roa-Varón, Giuseppe Marramà and Giorgio Carnevale. 2026. A New fossil from the Eocene of Iran provides new insights regarding the evolution of the morphologically bizarre tube-eye fish. Papers in Palaeontology. DOI: doi.org/10.1002/spp2.70114 [11 August 2026]


Saturday, July 11, 2026

[PaleoIchthyology • 2026] The Oldest Shark Face—Anatomy of the Devonian elasmobranch Phoebodus


Phoebodus saidselachus Frey, Coates, Ginter, Hairapetian, Rücklin, Jerjen & Klug, 2019

in Klug, Greif, Pohle, Ginter, Coates, Haouz, Lagnaoui, Pople et Frey, 2026. 

Phoebodus was recognized as the earliest elasmobranch known from articulated remains, a group which constitutes most modern cartilaginous fish comprising sharks, skates and rays. Its elongate body, the presence of two dorsal fins with fin spines, and the elongate head had already been described. Based on spectacularly well-preserved fossils, we add new anatomical information on its exact body proportions, the paired and caudal fins, the dermal denticles, the skull morphology, the endocast, and the gill skeleton. These new skeletons from the Famennian (Upper Devonian) of Morocco (c. 367 Ma) permit a much-improved reconstruction of the anatomy of Phoebodus. The new materials comprise the oldest elasmobranch specimens preserving the complete head in three dimensions. Additionally, the new materials yield information about growth and diet and thus position in the trophic network. Despite the newly coded characters, the phylogenetic position of the genus Phoebodus with the oldest teeth dating to the early Givetian remains that of the oldest stem-elasmobranch in the Bayesian analyses.

Key words: Chondrichthyes, Elasmobranchii, Famennian, ontogeny, exceptional preservation, Fossillagerstätten

Phoebodontiform elasmobranch Phoebodus saidselachus Frey et al., 2019a, middle Famennian, Upper Devonian, southern Maïder, Anti-Atlas, Morocco. A. PIMUZ A/I 5751, prep. T. Imhof, largest individual, nearly complete. B. PIMUZ A/I 5752, prep. T. Imhof, second largest individual, only caudal region missing; for details of the skull see Fig. 2. C. PIMUZ A/I 5753, prep. M. Greif, anterior half, excellent integument, fins and brachial region. D. PIMUZ A/I 5754, prep. R. Roth, two superimposed chondrichthyans; the skull in the middle is Maghriboselache mohamezanei with further remains; the straight, complete skeleton belongs to Phoebodus; the latter preserves the caudal fin. E. PIMUZ A/I 4712, holotype, smallest skeleton, nearly complete, modified after Frey et al. (2019a).

Skeletal reconstruction of the phoebodontiform elasmobranch Phoebodus saidselachus Frey et al., 2019a, middle Famennian, Upper Devonian, southern Maïder, Anti-Atlas, Morocco. A. PIMUZ A/I 5754, caudalis. B, C. PIMUZ A/I 4712, posterior and anterior dorsal fins. D. PIMUZ A/I 5752, anterior dorsal fin. E. PIMUZ A/I 5751, caudalis. F, G. PIMUZ A/I 5753, pectoral fin and branchial basket. H. PIMUZ A/I 5752, head. The photos are not to scale. The scale refers only to the drawing.

Systematic palaeontology 
Chondrichthyes Huxley, 1880 
Elasmobranchii Bonaparte, 1838 
Phoebodontiformes Ginter et al., 2010 

Genus Phoebodus St. John & Worthen, 1875


Reconstructions of an adult female and juvenile male of the phoebodontiform elasmobranch Phoebodus saidselachus Frey et al., 2019a, middle Famennian, Upper Devonian, southern Maïder, Anti-Atlas, Morocco. We incorporated the new anatomical details particularly in the proportions and the fin shapes. The juvenile is reconstructed after the holotype.

  
Christian Klug, Merle Greif, Alexander Pohle, Michał Ginter, Michael I. Coates, Wahiba Bel Haouz, Abdelouahed Lagnaoui, Jonathan Pople, and Linda Frey. 2026. The Oldest Shark Face—Anatomy of the Devonian elasmobranch Phoebodus. Acta Palaeontologica Polonica. 71 (2), 2026: 399-430 DOI:10.4202/app.01290.2025  https://www.app.pan.pl/article/item/app012902025.html

Linda Frey, Michael Coates, Michał Ginter, Vachik Hairapetian, Martin Rücklin, Iwan Jerjen, Christian Klug. 2019. The early elasmobranch Phoebodus: phylogenetic relationships, ecomorphology and a new time-scale for shark evolution. Proc Biol Sci. 286 (1912): 20191336. DOI: doi.org/10.1098/rspb.2019.1336

Thursday, June 18, 2026

[PaleoIchthyology • 2026] Asioaspis brachyotus • A New Genus of Polybranchiaspiformes (Galeaspida: stem-Gnathostomes) from the Lower Devonian of Yunnan, China

 

Asioaspis brachyotus
 R.-R. Zhang, N. Zhang, Li, Zhu & Gai, 2026
 
VERTEBRATA ALASIATICA. 64(2);   
 
A new genus and species, Asioaspis brachyotus gen. et sp. nov. of Polybranchiaspiformes, is described from the Lower Devonian Lochkovian Xishancun Formation near Miandian Reservoir, Qujing City, Yunnan Province, China. The new genus is characterized by an elongated ovoid headshield with serrated lateral margins, a small subcircular median dorsal opening, short and laterally projecting cornual processes, an exceptionally broad ventral rim, 12 pairs of branchial fossae, and coarse granular tubercles (~3/mm²). It displays a mosaic of characters of the most primitive polybranchiaspiform (Platylomaspis), derived Polybranchiaspiformes, and even the basal members of the galeaspid family Dayongaspidae. Phylogenetic analysis resolves A. brachyotus as an intermediate taxon between the most primitive Gumuaspidae and other derived Polybranchiaspiformes. Although A. brachyotus also shares the broad ham-brim-like ventral rim with the Gumuaspidae, its other characters are more like other derived Polybranchiaspiformes. In particular, its median dorsal opening and paired orbital openings are not highly close-set on the top of the headshield as in the Gumuaspidae, but rather significantly separated from each other and close to the margin of the ventral rim as in the Pentathyraspidae, Duyunolepididae, and Polybranchiaspidae. These proportions indicate that it was unlikely to have lived a semi-infaunal lifestyle and are more consistent with the epibenthic habit typical of most galeaspids, representing an evolutionary transition from the semi-infaunal benthic to epibenthic lifestyle within Polybranchiaspiformes.

Photograph of Asioaspis brachyotus gen. et sp. nov. from Lower Devonian Xishancun Formation, Qujing, Yunnan in ventral view
A. an incomplete headshield, paratype, IVPP V26676. 2; B. a nearly complete dorsal headshield, holotype, V26676. 1
A. an incomplete dorsal headshield, IVPP V26676.5; B. an incomplete dorsal headshield, V26676.4b

Subclass Galeaspida Tarlo, 1967 
Supraorder Polybranchiaspidida Janvier, 1996 
Order Polybranchiaspiformes Liu, 1965 

Family Asioaspidae fam. nov. 
Type genus Asioaspis gen. nov. 

Differential diagnosis: The Asioaspidae is distinguished from other families of Polybranchiaspiformes by its short, ear-like, and laterally projecting cornual processes. It resembles the Gumuaspidae in having a broad ventral rim, but differs in lacking a rostral process. It differs from the Duyunolepididae, Pentathyraspidae, and Polybranchiaspidae by the presence of a broad ventral rim and further differs from the Duyunolepididae by bearing a pair of broad inner cornual processes. Therefore, a new family, the Asioaspidae fam. nov., is herein established.

Genus Asioaspis gen. nov.  
Type species Asioaspis brachyotus gen. et sp. nov. 

Etymology: Asioaspis is derived from Asio (referring to owls of the genus Asio characterized by prominent ear tufts) plus aspis (Greek shield). 

Diagnosis: Medium-sized polybranchiaspiform characterized by an ovoid headshield with serrated lateral margins; the rostral margin arcuate, but lacking a rostral process; the cornual processes short and projecting laterally; the inner cornual processes large and broad leaf-shaped; median dorsal opening small and subcircular in shape; orbital opening large, round, and dorsally positioned; the sensory canals are well developed, V-shaped posterior supraorbitals and four pairs of lateral transverse canals issuing from the lateral dorsal canal; ventral rim of headshield remarkably broad, 13.5–14.1 mm in width on each side (approximately one half of the width of the entire headshield); a large dome-shaped oralobranchial chamber (a composite chamber with both oral and branchial functions) with 12 pairs of branchial fossae; and ornamentation consists of coarse tubercles (~3/mm²)

 Asioaspis brachyotus gen. et sp. nov. 

Etymology: The brachyotus means short-eared, which is in reference to its short and laterally projecting cornual processes that resemble a pair of short ears on the headshield, as in Asio.

Type locality and horizon: Miandian Reservoir in the Triathlon Sports Park, Qilin District, Qujing City, Yunnan Province, China; Xishancun Formation, lower Lochkovian, Lower Devonian.

Morphological comparison of Polybranchiaspiformes, Dayongaspidida, and Huananaspidiformes
A. Asioaspis; B. Dayongaspis (Zhang et al., 2024); C. Foxaspis (Gai et al., 2023); D. Platylomaspis (redrawn after Gai et al., 2018); E. Rhegmaspis (Gai et al., 2015); F. Rhegmaspis (Gai et al., 2015); G. Nanningaspis (redrawn after Gai et al., 2018)
A–E, G. in dorsal views; F. in ventral view.  

Phylogenetic diagram of Dayongaspidida, Polybranchiaspiformes, and Huananaspidiformes
Dayongaspis (Zhang et al., 2024); Platylomaspis (redrawn after Gai et al., 2018); Nanningaspis (redrawn after Gai et al., 2018); Polybranchiaspis (Liu, 1965); Foxaspis (Gai et al., 2023); Rhegmaspis (Gai et al., 2015).
No scaled

 Life restoration of Asioaspis brachyotus gen. et sp. nov. 


ZHANG Rui-Rui, ZHANG Ning, LI Qiang, ZHU Min and GAI Zhi-Kun. 2026. Asioaspis, A New Genus of Polybranchiaspiformes (Galeaspida, stem-Gnathostomes) from the Lower Devonian of Yunnan, China.  VERTEBRATA PALASIATICA. 64(2); 137-150.  DOI: 10.19615/j.cnki.2096-9899.260113 [20 April 2026] 


Sunday, April 26, 2026

[PaleoIchthyology • 2026] New Data on the sarcopterygian Koharalepis jarviki (Tetrapodomorpha: Canowindridae) from the Late Devonian of Antarctica, revealed via Synchrotron and Neutron Tomography

 

Koharalepis jarviki Young & Ritchie, 1992  
3D rendering of Koharalepis jarviki (AMF 54325) from neutron tomographic data.

  in Mensforth, Long, Bevitt et Clement, 2026. 
Artwork: Thomas Turner

Abstract
Introduction: The ‘osteolepiforms’ are an extinct order of lobe-finned fishes that had a cosmopolitan distribution, which are often considered for their proximity to the vertebrate water-to-land transition. The canowindrids are an East Gondwanan clade of tetrapodomorph fishes that exhibit a high level of endemism. However, due to the rarity of canowindrid material and their taphonomy, there is only a single representative preserved wholly in 3D and thus suitable for investigation via modern non-invasive tomography.

Methods: Here we present an updated description of the holotype of Koharalepis jarviki, a canowindrid collected from the Late Devonian Aztec Siltstone formation in Mt Crean, Antarctica, elucidated via a combination of synchrotron and neutron tomography.

Results and discussion: New elements of the braincase, palate, mandible and axial skeleton are revealed for the first time, and previously reported anatomy including the dermal skull and position of the orbits are confirmed. A partial braincase and endocast has been reconstructed, enabling rare insight into the neural anatomy of Koharalepis. Phylogenetic analysis confirms Koharalepis as a member of the Canowindridae with Harajicadectes zhumini recovered as sister taxon. The canowindrids occupy a region of the phylogenetic tree with ‘osteolepidid’ taxa and megalichthyids, crownward of rhizodonts but below tristichopterids and elpistostegalids. This work provides greater support for the taxonomic characters and phylogenetic position of the enigmatic canowindrid family, and the 3D preservation of this material has enabled us to infer some behavioural and ecological insight.

Keywords: 3D modelling, canowindrid, Devonian, endocast, neutron tomography, phylogenetic analysis, Sarcopterygii, tetrapodomorph

3D rendering of Koharalepis jarviki (AMF 54325) from neutron tomographic data in (A) dorsal view, (B) ventral view, (C) anterior view, (D) left lateral view and (E) posterior view.
Et, extra temporal; Ju, jugal; L.Ex, lateral extrascapular; M.Ex, median extrascapular; Op, operculum; Par, parietal; Po, postorbital; PP, postparietal; Sclm, supracleithrum; Sq, squamosal.

Life reconstruction of the Devonian tetrapodomorph fish Koharalepis jarviki.
Artwork: Thomas Turner/Flinders University

 Koharalepis jarviki Young & Ritchie, 1992


Corinne L. Mensforth, John A. Long, Joseph J. Bevitt and Alice M. Clement. 2026. New Data on the sarcopterygian Koharalepis jarviki (Tetrapodomorpha; Canowindridae) from the Late Devonian of Antarctica, revealed via Synchrotron and Neutron Tomography. Front. Ecol. Evol. (14); DOI: doi.org/10.3389/fevo.2026.1765271 [16 April 2026]

Thursday, March 5, 2026

[PaleoIchthyology • 2026] Eosteus chongqingensis • The Oldest articulated Bony Fish from the early Silurian period

 

 Eosteus chongqingensis
Y.-A. Zhu, Chen, Li, Zhao, Zhou, Jia, Y.-L. Yu, H.-X. Yu, Wei, Ahlberg, Lu & M. Zhu, 2026

Life reconstruction by NICE PaleoVislab, IVPP

Abstract
Osteichthyans, comprising sarcopterygians and actinopterygians, dominate modern vertebrate biodiversity, yet their pre-Devonian fossil record remains scarce and fragmentary. The oldest articulated sarcopterygian and stem osteichthyan date to the late Silurian, whereas undisputed actinopterygian fossils in articulation appear only in the Middle Devonian. Here we report an articulated, near-complete osteichthyan from the early Silurian Chongqing Lagerstätte (approximately 436 million years ago), representing the oldest osteichthyan occurrence including microfossils. This tiny fish exhibits a fusiform, generalized osteichthyan body outline, with plesiomorphic osteichthyan characters, including the lack of lepidotrichia and the presence of serial median dorsal plates, pectoral and dorsal fin spines and an anal fin spine reported previously exclusively in stem chondrichthyans and one placoderm. It also displays features, such as a single dorsal fin and caudal fulcra, seen commonly in actinopterygians. Bayesian inference and the 50% majority rule consensus of the maximum-parsimony analysis place the new fish on the osteichthyan stem, whereas the strict consensus leaves its position unresolved within osteichthyans. This discovery increases Silurian osteichthyan diversity and further populates the osteichthyan stem group. The morphological disparity among early osteichthyans implies a more extensive Silurian to Early Devonian radiation of bony fishes than previous lines of evidence suggested.

Morphological evolution of early jawed vertebrates, showing the position of Eosteus and Megamastax among stem bony fishes. 


Eosteus chongqingensis

Life reconstruction of the oldest osteichthyan Eosteus chongqingensis.
 Credit: NICE PaleoVislab, IVPP



Life reconstruction of the biggest Silurian vertebrate Megamastax amblyodus.
Credit: Image by NICE PaleoVislab, IVPP

 
You-An Zhu, Yang Chen, Qiang Li, Wen-Jin Zhao, Zheng-Da Zhou, Lian-Tao Jia, Yi-Lun Yu, Han-Xin Yu, Guang-Biao Wei, Per E. Ahlberg, Jing Lu and Min Zhu. 2026. The Oldest articulated Bony Fish from the early Silurian period. Nature. 651; 128–134. DOI: doi.org/10.1038/s41586-026-10125-2 [04 March 2026]