2024 in archosaur paleontology

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List of years in archosaur paleontology
In reptile paleontology
2021
2022
2023
2024
2025
2026
2027
In paleontology
2021
2022
2023
2024
2025
2026
2027
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This article records new taxa of every kind of fossil archosaur that are scheduled to be described during 2024, as well as other significant discoveries and events related to the paleontology of archosaurs that will be published in 2024.

Contents

Pseudosuchians

New pseudosuchian taxa

NameNoveltyStatusAuthorsAgeType localityCountryNotesImages

Ahdeskatanka [1]

Gen. et sp. nov

Cossette & Tarailo

Wasatchian

Golden Valley Formation

Flag of the United States.svg  United States
(Flag of North Dakota.svg  North Dakota)

A member of the family Alligatoridae belonging to the subfamily Alligatorinae. The type species is A. russlanddeutsche.

Ahdeskatanka russlanddeutsche.jpg

Aphaurosuchus kaiju [2]

Sp. nov

In press

Martins et al.

Late Cretaceous

Adamantina Formation

Flag of Brazil.svg  Brazil

A baurusuchid. Announced in 2023; the final article version was published in 2024.

Araripesuchus manzanensis [3]

Sp. nov

Valid

Fernández Dumont et al.

Late Cretaceous (Cenomanian)

Candeleros Formation

Flag of Argentina.svg  Argentina

Asiatosuchus oenotriensis [4]

Sp. nov

Narváez et al.

Eocene (Lutetian)

Flag of Spain.svg  Spain

A basal member of Crocodyloidea.

Benggwigwishingasuchus [5] Gen. et sp. novValidSmith et al.Middle Triassic (Anisian) Favret Formation Flag of the United States.svg  United States
(Flag of Nevada.svg  Nevada)
A member of Paracrocodylomorpha, probably belonging to the group Poposauroidea. The type species is B. eremicarminis. Benggwigwishingasuchus.jpg

Caipirasuchus catanduvensis [6]

Sp. nov

Iori et al.

Late Cretaceous

Adamantina Formation

Flag of Brazil.svg  Brazil

Enalioetes [7]

Gen. et sp. nov

Valid

Sachs et al.

Early Cretaceous (Valanginian)

Stadthagen Formation

Flag of Germany.svg  Germany

A metriorhynchid. The type species is E. schroederi.

Skull of Enalioetes schroederi.jpg

Epoidesuchus [8]

Gen. et sp. nov

Ruiz et al.

Late Cretaceous (Campanian–Maastrichtian)

Adamantina Formation

Flag of Brazil.svg  Brazil

A peirosaurid notosuchian. The type species is E. tavaresae.

Garzapelta [9]

Gen. et sp. nov

Valid

Reyes, Martz & Small

Late Triassic (Norian)

Cooper Canyon Formation

Flag of the United States.svg  United States
(Flag of Texas.svg  Texas)

An aetosaur. The type species is G. muelleri.

Ophiussasuchus [10]

Gen. et sp. nov

Valid

López-Rojas et al.

Late Jurassic (Kimmeridgian–Tithonian)

Lourinhã Formation

Flag of Portugal.svg  Portugal

A goniopholidid crocodylomorph. The type species is O. paimogonectes.

Paranacaiman [11] Gen. et sp. novBona et al.Miocene Ituzaingó Formation Flag of Argentina.svg  Argentina A caiman. The type species is P. bravardi. Fossils of this genus were previously referred to Caiman lutescens . Caiman-lutescens-MACN-PV-13551-skull-in-A-dorsal-view-and-B-dorsolateral-view.jpg
Paranasuchus [11] Gen. et comb. novBona et al.MioceneItuzaingó FormationFlag of Argentina.svg  Argentina A caiman. The type species is "Caiman" gasparinae.
Parvosuchus [12] Gen. et sp. novMüllerTriassic (Ladinian–Carnian) Pinheiros-Chiniquá Sequence of the Santa Maria Supersequence Flag of Brazil.svg  Brazil A gracilisuchid pseudosuchian. The type species is P. aurelioi. Parvosuchus skull.png

Schultzsuchus [13]

Gen. et comb. nov

Desojo & Rauhut

Triassic (Ladinian–Carnian)

Pinheiros-Chiniquá Sequence of the Santa Maria Supersequence

Flag of Brazil.svg  Brazil

A member of Paracrocodylomorpha, probably belonging to the group Poposauroidea. The type species is "Prestosuchus" loricatus von Huene (1938).

Sutekhsuchus [14]

Gen. et comb. nov

Valid

Burke et al.

Miocene

Moghra Formation

Flag of Egypt.svg  Egypt
Flag of Libya.svg  Libya

A member of the family Gavialidae belonging to the subfamily Gavialinae. The type species is "Tomistoma" dowsoni Fourtau (1920).

Sutekhsuchus lateral view.jpg

Varanosuchus [15]

Gen et sp. nov

In press

Pochat-Cottilloux et al.

Early Cretaceous

Sao Khua Formation

Flag of Thailand.svg  Thailand

An atoposaurid. The type species is V. sakonnakhonensis.

General pseudosuchian research

Aetosaur research

Crocodylomorph research

Non-avian dinosaurs

New dinosaur taxa

NameNoveltyStatusAuthorsAgeType localityCountryNotesImages

Alpkarakush [57]

Gen. et sp. nov

Valid

Rauhut et al.

Middle Jurassic (Callovian)

Balabansai Formation

Flag of Kyrgyzstan.svg  Kyrgyzstan

A metriacanthosaurid theropod. The type species is A. kyrgyzicus.

Alpkarakush kyrgyzicus.png
Ardetosaurus [58] Gen. et sp. novvan der Linden et al.Late Jurassic (Kimmeridgian) Morrison Formation Flag of the United States.svg  United States
(Flag of Wyoming.svg  Wyoming)
A diplodocine sauropod. The type species is A. viator. Ardetosaurus viator.png

Asiatyrannus [59]

Gen. et sp. nov

Valid

Zheng et al.

Late Cretaceous (Maastrichtian)

Nanxiong Formation

Flag of the People's Republic of China.svg  China

A tyrannosaurine theropod. The type species is A. xui.

Asiatyrannus xui.png

Baiyinosaurus [60]

Gen. et sp. nov

Valid

Ning et al.

Middle Jurassic (Bathonian)

Wangjiashan Formation

Flag of the People's Republic of China.svg  China

A basal stegosaurian. The type species is B. baojiensis.

Baiyinosaurus baojiensis.png

Caletodraco [61]

Gen. et sp. nov

Valid

Buffetaut et. al

Late Cretaceous (Cenomanian)

Chalk of the Pays de Caux

Flag of France.svg  France

An abelisaurid theropod. The type species is C. cottardi.

Caletodraco cottardi.png

Campananeyen [62]

Gen. et sp. nov

Lerzo et al.

Late Cretaceous (Cenomanian)

Candeleros Formation

Flag of Argentina.svg  Argentina

An rebbachisaurid sauropod. The type species is C. fragilissimus.

Campananeyen fragilissimus.png

Chakisaurus [63]

Gen. et sp. nov

Alvarez Nogueira et al.

Late Cretaceous (Cenomanian–Turonian)

Huincul Formation

Flag of Argentina.svg  Argentina

An elasmarian ornithopod. The type species is C. nekul.

Chakisaurus UDL.png
Coahuilasaurus [64] Gen. et sp. novValidLongrich et al.Late Cretaceous (Campanian) Cerro del Pueblo Formation Flag of Mexico.svg  Mexico A saurolophine hadrosaurid belonging to the tribe Kritosaurini. The type species is C. lipani. Coahuilasaurus lipani.png
Comptonatus [65] Gen. et sp. novLockwood et al.Early Cretaceous (Barremian) Wessex Formation Flag of the United Kingdom.svg  United Kingdom An iguanodontid ornithopod. The type species is C. chasei. Comptonatus chasei.png

Datai [66]

Gen. et sp. nov

Valid

Xing et al.

Late Cretaceous (Turonian–Early Coniacian)

Zhoutian Formation

Flag of the People's Republic of China.svg  China

An ankylosaurid. The type species is D. yingliangis.

Datai yingliangis.png

Diuqin [67]

Gen. et sp. nov

Valid

Porfiri et al.

Late Cretaceous (Santonian)

Bajo de la Carpa Formation

Flag of Argentina.svg  Argentina

A unenlagiine theropod. The type species is D. lechiguanae.

Diuqin lechiguanae.png

Dornraptor [68]

Gen. et sp. nov

Valid

Baron

Early Jurassic (Hettangian–Sinemurian)

Blue Lias Formation

Flag of the United Kingdom.svg  United Kingdom

An averostran theropod. The type species is D. normani.

Dornraptor normani.png

Emiliasaura [69]

Gen. et sp. nov

Coria et al.

Early Cretaceous (Valanginian)

Mulichinco Formation

Flag of Argentina.svg  Argentina

An ornithopod belonging to the group Rhabdodontomorpha. The type species is E. alessandrii.

Emiliasaura alessandrii.png

Eoneophron [70]

Gen. et sp. nov

Atkins-Weltman et al.

Late Cretaceous (Maastrichtian)

Hell Creek Formation

Flag of the United States.svg  United States
(Flag of South Dakota.svg  South Dakota)

A caenagnathid theropod. The type species is E. infernalis.

Eoneophron infernalis.png
Fona [71] Gen. et sp. novAvrahami et al.Late Cretaceous (Cenomanian) Cedar Mountain Formation Flag of the United States.svg  United States
(Flag of Utah.svg  Utah)
A thescelosaurid ornithischian. The type species is F. herzogae. Fona herzogae.png

Gandititan [72]

Gen. et sp. nov

Valid

Han et al.

Late Cretaceous (Cenomanian–Turonian)

Zhoutian Formation

Flag of the People's Republic of China.svg  China

A titanosaur sauropod. The type species is G. cavocaudatus.

Gandititan UDL.png

Harenadraco [73]

Gen. et sp. nov

Lee et al.

Late Cretaceous

Barun Goyot Formation

Flag of Mongolia.svg  Mongolia

A troodontid theropod. The type species is H. prima.

Harenadraco prima.png

Hesperonyx [74]

Gen. et sp. nov

Valid

Rotatori et al.

Late Jurassic

Lourinhã Formation

Flag of Portugal.svg  Portugal

An early diverging iguanodontian ornithopod, possibly a dryomorphan. The type species is H. martinhotomasorum.

Hesperonyx martinhotomasorum.png
Huaxiazhoulong [75] Gen. et sp. novZhu et al.Late Cretaceous (Campanian) Tangbian Formation Flag of the People's Republic of China.svg  China An ankylosaurid. The type species is H. shouwen. Huaxiazhoulong shouwen.png

Hypnovenator [76]

Gen. et sp. nov

Valid

Kubota, Kobayashi & Ikeda

Early Cretaceous (Albian)

Ohyamashimo Formation

Flag of Japan.svg  Japan

A troodontid theropod. The type species is H. matsubaraetoheorum.

Hypnovenator matsubaraetoheorum.png

Inawentu [77]

Gen. et sp. nov

Valid

Filippi et al.

Late Cretaceous (Santonian)

Bajo de la Carpa Formation

Flag of Argentina.svg  Argentina

A titanosaur sauropod. The type species is I. oslatus. Announced in 2023; the final article version was published in 2024.

Inawentu oslatus.png

Jingiella [78]

Gen. et sp. nov

Ren et al.

Late Jurassic

Dongxing Formation

Flag of the People's Republic of China.svg  China

A mamenchisaurid sauropod. The type species is J. dongxingensis. The initially proposed name is preoccupied by Jingia Chen, 1983. [79] The replacement name was published in an addendum. [80]

Jingiella UDL.png

Kiyacursor [81]

Gen. et sp. nov

Averianov et al.

Early Cretaceous (Aptian)

Ilek Formation

Flag of Russia.svg  Russia
(Flag of Kemerovo Oblast.svg  Kemerovo Oblast)

A noasaurid theropod. The type species is K. longipes.

Kiyacursor longipes.png

Koleken [82]

Gen. et sp. nov

Pol et al.

Late Cretaceous (Campanian–Maastrichtian)

La Colonia Formation

Flag of Argentina.svg  Argentina

An abelisaurid theropod. The type species is K. inakayali.

Koleken inakayali.png

Labocania aguillonae [83]

Sp. nov

Valid

Rivera-Sylva & Longrich

Late Cretaceous (Campanian)

Cerro del Pueblo Formation

Flag of Mexico.svg  Mexico

A teratophonein tyrannosaurine; a species of Labocania .

Labocania aguillonae (skeletal reconstruction).jpg

Lokiceratops [84]

Gen. et sp. nov

Valid

Loewen et al.

Late Cretaceous (Campanian)

Judith River Formation

Flag of the United States.svg  United States
(Flag of Montana.svg  Montana)

A centrosaurine ceratopsian. The type species is L. rangiformis.

Lokiceratops rangiformis.png

Minqaria [85]

Gen. et sp. nov

Longrich et al.

Late Cretaceous (Maastrichtian)

Ouled Abdoun Basin

Flag of Morocco.svg  Morocco

A lambeosaurine hadrosaurid belonging to the tribe Arenysaurini. The type species is M. bata.

Minqaria bata.png
Musankwa [86] Gen. et sp. novBarrett et al. Late Triassic (Norian) Pebbly Arkose Formation Flag of Zimbabwe.svg  Zimbabwe A massopodan sauropodomorph. The type species is M. sanyatiensis. Musankwa sanyatiensis.png
Qianjiangsaurus [87] Gen. et sp. novDai et al.Late Cretaceous Zhengyang Formation Flag of the People's Republic of China.svg  China An early-diverging hadrosauromorph. The type species is Q. changshengi. Qianjiangsaurus changshengi.png

Qunkasaura [88]

Gen. et sp. nov

Valid

Mocho et al.

Late Cretaceous (Campanian-Maastrichtian)

Villalba de la Sierra Formation

Flag of Spain.svg  Spain

A saltasauroid titanosaur. The type species is Q. pintiquiniestra.

Qunkasaura pintiquiniestra.png

Riojavenatrix [89]

Gen. et sp. nov

Isasmendi et al.

Early Cretaceous (Barremian–Aptian)

Enciso Group

Flag of Spain.svg  Spain

A spinosaurid theropod. The type species is R. lacustris.

Riojavenatrix lacustris.png
Sasayamagnomus [90] Gen. et sp. nov.ValidTanaka et al.Early Cretaceous (Albian) Ohyamashimo Formation Flag of Japan.svg  Japan A basal member of Neoceratopsia. The type species is S. saeguesai. Sasayamagnomus saegusai.png

Sidersaura [91]

Gen. et sp. nov

Valid

Lerzo et al.

Late Cretaceous (Cenomanian–Turonian)

Huincul Formation

Flag of Argentina.svg  Argentina

A rebbachisaurid sauropod. The type species is S. marae.

Sidersaura UDL.png

Thyreosaurus [92]

Gen. et sp. nov

Zafaty et al.

Middle Jurassic

El Mers Group

Flag of Morocco.svg  Morocco

A stegosaurian. The type species is T. atlasicus.

Thyreosaurus Skeletal.svg

Tiamat [93]

Gen. et sp. nov

Pereira et al.

Cretaceous (Albian–Cenomanian)

Açu Formation

Flag of Brazil.svg  Brazil

A basal titanosaur sauropod. The type species is T. valdecii.

Tiamat Skeletal.svg
Tietasaura [94] Gen. et sp. novBandeira et al.Early Cretaceous (ValanginianHauterivian) Marfim Formation Flag of Brazil.svg  Brazil An elasmarian ornithopod. The type species is T. derbyiana. Tietasaura Skeletal.svg

Titanomachya [95]

Gen. et sp. nov

Pérez-Moreno et al.

Late Cretaceous (Campanian–Maastrichtian)

La Colonia Formation

Flag of Argentina.svg  Argentina

A titanosaur sauropod. The type species is T. gimenezi.

Titanomachya UDL.png

Tyrannosaurus mcraeensis [96]

Sp. nov

Valid

Dalman et al.

Late Cretaceous (Campanian–Maastrichtian)

Hall Lake Formation

Flag of the United States.svg  United States
(Flag of New Mexico.svg  New Mexico)

A tyrannosaurine; a species of Tyrannosaurus .

Tyrannosaurus mcraeensis (skull reconstruction).png

Udelartitan [97]

Gen. et sp. nov

Valid

Soto et al.

Late Cretaceous

Guichón Formation

Flag of Uruguay.svg  Uruguay

A titanosaur sauropod belonging to the group Saltasauroidea. The type species is U. celeste.

Udelartitan UDL.png

Urbacodon norelli [98]

Sp. nov

Wang et al.

Late Cretaceous

Iren Dabasu Formation

Flag of the People's Republic of China.svg  China

A troodontid theropod; a species of Urbacodon .

Vectidromeus [99]

Gen. et sp. nov

Valid

Longrich et al.

Early Cretaceous (Barremian)

Wessex Formation

Flag of the United Kingdom.svg  United Kingdom

A hypsilophodontid. The type species is V. insularis. Announced in 2023; the final article version was published in 2024.

Vectidromeus UDL.png

Yanbeilong [100]

Gen. et sp. nov

Valid

Jia et al.

Early Cretaceous (Albian)

Zuoyun Formation

Flag of the People's Republic of China.svg  China

A stegosaurian. The type species is Y. ultimus.

Yanbeilong ultimus.png

Yuanyanglong [101]

Gen. et sp. nov

Hao et al.

Early Cretaceous

Miaogou Formation

Flag of the People's Republic of China.svg  China

An oviraptorosaur theropod. The type species is Y. bainian.

Yuanyanglong bainian.png

General non-avian dinosaur research

Saurischian research

Theropod research

  • Manafzadeh et al. (2024) argue that the knees of early theropod dinosaurs were restricted to hinge-like motion, and that the reduction of the fibula during the theropod evolution had significant biomechanical consequences for theropod locomotion, freeing the fibula from the ankle joint and ultimately enabling extreme knee long-axis rotation of extant birds. [125]
  • A study on the femoral shape variation in theropods, providing evidence of evolution of similar adaptations to gigantism in large-bodied theropods regardless of their phylogenetic affinities, is published by Pintore et al. (2024). [126]
  • Dridi et al. (2024) describe tracks of medium to large-sized theropods from the Lower Cretaceous (HauterivianBarremian) strata from the Jebel Kebar locality (Bouhedma Formation, Tunisia), extending known geographic range of non-avian theropods to higher latitudes within Gondwana. [127]
  • A study on the affinities of shed tooth crowns of theropods from the Turonian-Coniacian Portezuelo Formation (Argentina), providing evidence of a previously undocumented diversity of theropods from this formation, is published by Meso et al. (2024). [128]
  • Isasmendi et al. (2024) describe new and revise known theropod teeth from the Maastrichtian strata from the South Pyrenean Basin (Spain), expanding known diversity of theropods from this basin and reporting evidence of theropod turnover during the Maastrichtian. [129]
  • A partial egg clutch including the smallest non-avian theropod eggs reported to date is described from the Upper Cretaceous Tangbian Formation (China) by Wu et al. (2024), who name a new ovaloolithid ootaxon Minioolithus ganzhouensis . [130]
  • McLarty & Esperante (2024) describe theropod tracks from the Maastrichtian strata from the Carreras Pampa tracksite (Bolivia) interpreted as likely preserving evidence of the trackmakers pausing during movement, bypassing an obstacle and crouching. [131]
  • Bugos & McDavid (2024) describe skulls of immature specimens of Coelophysis bauri from the Coelophysis Quarry at Ghost Ranch (New Mexico, United States). [132]
  • Marsh et al. (2024) describe post-cranial material from the Lower Jurassic Kayenta Formation (Utah, United States) and interpret it as belonging to an intermediate theropod. [133]
  • Liang, Falkingham & Xing (2024) present a digital skeleton model of Sinosaurus , based on data from a new, well-preserved specimen, and provide new body mass estimates for this theropod. [134]
  • Mohabey et al. (2024) review and redescribe Laevisuchus indicus , Jubbulpuria tenuis and Compsosuchus solus , and describe a new noasaurid dentary from central India with procumbent dentition similar to the one present in Masiakasaurus . [135]
  • A study on the affinities of isolated theropod teeth from the Kem Kem Group (Morocco) is published by Hendrickx et al. (2024), who identify teeth of abelisaurids, spinosaurines, carcharodontosaurids and a non-abelisauroid ceratosaur or a megaraptoran. [136]
  • A probable ceratosaurid dentary is described from the Toarcian Cañadón Asfalto Formation (Argentina) by Pradelli, Pol & Ezcurra (2024), expanding known theropod diversity from this formation. [137]
  • A study on the affinities of isolated theropod teeth from the Bauru Basin (Brazil) is published by Delcourt et al. (2024), who argue that the geographical distribution of abelisaurids in South America was influenced by climatic conditions. [138]
  • Ribeiro et al. (2024) identify a theropod tooth from the Upper Jurassic-Lower Cretaceous Missão Velha Formation (Brazil) as the oldest abelisaurid record in the South America reported to date. [139]
  • A study in the bone histology of a mid-sized abelisaurid from the Upper Cretaceous Serra da Galga Formation (Brazil) is published by Aureliano et al. (2024), who report that, despite living in a semiarid tropical environment, the studied specimen had a growth rate similar to those of the Patagonian abelisaurids. [140]
  • Candeiro et al. (2024) describe abelisaurid teeth from the strata of the Marília Formation in the State of Goiás (Brazil), representing the northernmost abelisaurid record in the Bauru Basin reported to date. [141]
  • A study on the skeletal pathologies affecting known specimens of brachyrostran abelisaurids is published by Baiano et al. (2024), who diagnose the fusion of two caudal vertebrae of the holotype specimen of Aucasaurus garridoi as congenital malformation and diagnose partial fusion of five caudal vertebrae of the holotype of Elemgasem nubilus as spondyloraptropathy, in both cases representing the first occurrences of the diagnosed pathologies among non-tetanuran theropods. [142]
  • Cerroni, Otero & Novas (2024) present the reconstruction of the pelvic and hindlimb musculature of Skorpiovenator bustingorryi . [143]
  • A study on the microarchitecture of bones of the axial skeleton of Majungasaurus and Rahonavis , providing evidence of increase of pneumatic complexity in early paravians compared to members of Ceratosauria, is published by Aureliano et al. (2024). [144]
  • Cau (2024) reinterprets "compsognathid" theropod specimens as juveniles of members of non-maniraptoriform tetanuran groups. [145]
  • Montealegre, Castillo-Visa & Sellés (2024) describe previously unpublished fossil material of theropods (cf. Protathlitis and a carcharodontosaurid which might be distinct from Concavenator ) from the Barremian Arcillas de Morella Formation (Spain). [146]
  • Lacerda et al. (2024) describe new fossil material of spinosaurids (including a cervical vertebra of Sigilmassasaurus ) and partial ischium of an indeterminate carcharodontosaurid from the Kem Kem Group (Morocco). [147]
  • Yun (2024) identifies convergent similarities in craniodental anatomy between spinosaurs and phytosaurs. [148]
  • D'Amore et al. (2024) study the morphology of the skull and teeth of spinosaurids, and find no evidence that the diets of spinosaurids were restricted to fish or small aquatic prey. [149]
  • A study on the diversity of spinosaurid teeth from the Camarillas Formation (Spain) is published by Cabrera-Argudo, García-Cobeña & Cobos (2024), who report possible evidence of the presence of at least one baryonychine and one spinosaurine in the eastern Iberian Peninsula during the early Barremian. [150]
  • The purported abelisaur ilium from the Upper Cretaceous Kem Kem Group (Morocco) described by Zitouni et al. (2019) [151] is interpreted as a bone of a spinosaurine spinosaurid different from the ilium of the Spinosaurus aegyptiacus neotype by Samathi (2024), who considers the studied fossil to be likely evidence of the presence of two morphotypes of spinosaurines in the Kem Kem Group. [152]
  • Myhrvold et al. (2024) use statistical analyses to reconsider previous descriptions by Fabbri et al. (2022) of spinosaurs such as Spinosaurus as subaqueous foragers, [153] and provide evidence that Spinosaurus was likely not an aquatic pursuit predator. [154]
  • Evidence from the study of patterns in skull shape, interpreted as indicating that Spinosaurus fed on aquatic prey and likely used the "stand-and-wait" predation strategy, is presented by Smart & Sakamoto (2024). [155]
  • Buffetaut & Tong (2024) reinterpret a purported ichthyosaur tooth from the Sao Khua Formation collected in 1962 and described in 1963 as a spinosaurid tooth and the first finding of a non-avian dinosaur fossil reported from Thailand. [156]
  • Evidence of large ranges of extension and flexion of manual joints and limited range of motion of the shoulder joints of Allosaurus fragilis is presented by Liang et al. (2024). [157]
  • A dorsal vertebra of an indeterminate carcharodontosaurid with similarities to the vertebrae of Acrocanthosaurus is described from the Turonian Bissekty Formation (Uzbekistan) by Averianov & Sues (2024). [158]
  • Rolando et al. (2024) describe a second specimen of Taurovenator violantei , expanding on the known anatomy of this genus. [159]
  • Rowe & Rayfield (2024) study the biomechanical capabilities of the skulls of tyrannosauroid theropods with different body size and skull morphology, and find that larger tyrannosauroids experienced higher absolute stresses in their skulls during feeding compared to their small-bodied relatives, and that wide skulls of tyrannosaurids enabled them to better accommodate high stresses during feeding. [160]
  • A study on tooth replacement pattern of Guanlong wucaii is published by Ke, Pei & Xu (2024). [161]
  • Teeth of a probable basal tyrannosauroid are described from the Upper Jurassic Phu Kradung Formation (Thailand) by Chowchuvech et al. (2024). [162]
  • Xing et al. (2024) describe large tyrannosauroid teeth from the Maastrichtian Dalangshan Formation, representing the southernmost record of tyrannosauroids in China reported to date. [163]
  • LeBlanc et al. (2024) report that extant Komodo dragons maintain cutting edges of their teeth through iron-enriched coatings on their tooth serrations and tips, argue that iron sequestration is probably widespread in reptile enamels, but also find no evidence of iron coatings along theropod dinosaur tooth serrations, report that tyrannosaurids had specialized, wavy enamel along their tooth serrations that likely supported the cutting edges of the teeth, and interpret these findings as either indicative of different feeding strategies of tyrannosaurids and Komodo dragons, or indicating that only large theropods had tooth enamel that was thick enough to significantly influence the mechanical wear of the tooth serrations. [164]
  • Słowiak, Brusatte & Szczygielski (2024) reevaluate the fossil material attributed to Bagaraatan ostromi , interpreting the holotype as an indeterminate juvenile tyrannosaurid, and reporting that some of the fossils originally attributed to B. ostromi are actually caenagnathid bones. [165]
  • Yun (2024) estimates mandibular force profiles of Alioramus altai and Qianzhousaurus sinensis , interpreting the mandibles of the studied theropods as likely unsuited for delivering powerful bites and enduring high stresses caused by capturing, holding and dismembering large prey. [166]
  • Evidence from the study of skull bones of immature specimens of Daspletosaurus from the Dinosaur Park Formation (Alberta, Canada), indicating that skull material of Daspletosaurus and Gorgosaurus can be confidently identified regardless of ontogenetic stage of the specimens, is presented by Coppock et al. (2024). [167]
  • A study on the affinities of tyrannosaurines is published by Warshaw, Barrera Guevara & Fowler (2024), who contest the conclusions of the study of Scherer & Voiculescu-Holvad (2023), [168] recovering recognized Daspletosaurus species as representing a single anagenetic lineage ancestral to Tyrannosaurus-line tyrannosaurines. [169]
  • Longrich & Saitta (2024) review the taxonomic status of Nanotyrannus and argue that multiple lines of evidence support it as a distinct, small-bodied, possibly non-tyrannosaurid taxon, rather than an immature form of Tyrannosaurus . [170]
  • Mallon & Hone (2024) estimate that past sampling efforts likely resulted in sampling even the 99th percentile of body mass reached by Tyrannosaurus rex, and that the very largest members of the species might have been up to 70% larger than the largest currently known specimens, reaching approximately 15,000 (± 3750) kg of body mass. [171]
  • A study on the phylogenetic relationships of Kinnareemimus khonkaenensis is published by Samathi (2024). [172]
  • Gianechini et al. (2024) describe and indeterminate alvarezsaurian femur from the Plottier Formation (Argentina), filling a temporal gap (between Coniacian and Santonian) in the fossil record of Late Cretaceous Patagonian alvarezsaurians. [173]
  • Description of the skeletal anatomy of Nothronychus graffami and N. mckinleyi, providing evidence of the presence of traits convergent with extant birds, ornithischian dinosaurs and titanosaur sauropods, is published by Smith & Gillette (2024). [174]
  • Park et al. (2024) propose that early pennaraptorans might have used their pennaceous feathers to flush hiding insects and to generate lift or drag during the pursuit of the flushed insects, and propose that such use of the pennaceous feathers might have contributed to the evolution of larger and stiffer feathers. [175]
  • A characterization of how number and shape of flight feathers correlate with locomotory style in extant birds is published by Kiat & O'Connor (2024). Extrapolating these patterns to Mesozoic pennaraptorans, the authors suggest that Caudipteryx and anchiornithines may have been secondarily flightless. [176]
  • A study on the evolution of the pectoral girdle of pennaraptorans is published by Wu et al. (2024), who report evidence of modifications changing the range of motion of the forelimb that preceded the origin of flight in paravians, as well as evidence of subsequent flight adaptive modifications in avialans. [177]
  • Meade et al. (2024) report evidence indicating that the ability of the skull to resist large mechanical stresses appeared early in oviraptorosaur evolution, before the appearance of the highly modified oviraptorid cranial architecture. [178]
  • The first caenagnathid fossil material from the upper Campanian De-na-zin Member of the Kirtland Formation (New Mexico, United States) is described by Funston, Williamson & Brusatte (2024). [179]
  • Qiu et al. (2024) describe the skeletal anatomy of the wrist of Heyuannia huangi , providing evidence of a specialized wrist morphology that was functionally convergent with the wrist morphology of extant birds. [180]
  • Description of the skeletal anatomy of Oksoko avarsan is published by Funston (2024). [181]
  • Zhu, Wang & Wang (2024) study the microstructural variation of elongatoolithid eggs from China, and interpret the studied variation as indicating that not all elongatoolithid eggshells can be related to oviraptorosaurs. [182]
  • A study on the skull shape and bite mechanics of dromaeosaurids is published by Tse, Miller & Pittman (2024), who interpret Deinonychus antirrhopus as adapted to taking large vertebrate prey, and interpret Halszkaraptor escuilliei as unlikely to feed on fish, and more likely to have a feeding ecology similar to those of extant waterfowl. [183]
  • Possible dromaeosaurid eggs are described from the Upper Cretaceous Lianhe Formation (China) by Wu et al. (2024), who name a new ootaxon Gannanoolithus yingliangi , and interpret the discovery of paired eggs of Gannanoolithus as possible evidence that dromaeosaurids had paired functional oviducts. [184]
  • Motta et al. (2024) interpret Imperobator antarcticus as a member of Unenlagiidae. [185]
  • Gianechini, Colli & Makovicky (2024) present a reconstruction of the pelvic and hindlimb musculature of Buitreraptor gonzalezorum . [186]
  • Dececchi et al. (2024) interpret two-toed theropod trackway from the Cretaceous Jinju Formation (South Korea) produced by a small microraptorine moving at high speed as evidence of wing-assisted movement of a non-avian theropod. [187]
  • A juvenile specimen of Microraptor , representing the smallest dromaeosaurid specimen from the Jehol Biota reported to date and preserving anatomical details that are poorly preserved in the other specimens of Microraptor, is described from the Jiufotang Formation (China) by Wang & Pei (2024), who also introduce the name Serraraptoria for the most inclusive clade containing Microraptor zhaoianus and Velociraptor mongoliensis but not Mahakala omnogovae , Halszkaraptor escuilliei and Unenlagia comahuensis . [188]
  • Based on comparisons to extant birds, joint poses in the foot of Deinonychus during its walk cycle are reconstructed by Manafzadeh, Gatesy & Bhullar (2024). [189]
  • Description of the braincase and cranial endocast of Sinovenator changii , interpreted as morphologically intermediate between basal theropods and extant birds, is published by Yu et al. (2024). [190]
  • Xing et al. (2024) describe tracks from the Upper Cretaceous Shaxian Formation (Fujian, China) which might have been produced by a large-bodied (estimated hip height of over 1.8 m) troodontid, and name a new ichnotaxon Fujianipus yingliangi . [191]

Sauropodomorph research

  • Frauenfelder et al. (2024) reevaluate the utility of sauropodomorph tooth measurement indices as proxies for classification of the studied dinosaurs. [192]
  • Müller, Damke & Terras (2024) find that inclusion of skeletally immature individuals in the phylogenetic analyses of early Late Triassic sauropodomorphs results in the artificial grouping of the immature specimens in the phylogenetic trees. [193]
  • Silva et al. (2024) describe fossil material of a member or a relative of the group Bagualosauria from the Vila Botucaraí site (Candelária Sequence of the Santa Maria Supersequence, Brazil), representing the first sauropodomorph reported from this site. [194]
  • Evidence of variability of the pneumacity patterns of the cervical and dorsal vertebrae in Plateosaurus is presented by Regalado Fernández (2024). [195]
  • Redescription of the holotype and a study on the affinities of Plateosaurus trossingensis is published by Schaeffer (2024). [196]
  • Schaeffer et al. (2024) describe pathologies in the chevrons of the tail in two specimens of Plateosaurus trossingensis from the Obere Mühle locality in Trossingen (Germany), report pathologies in the tail chevrons in further specimens indicating that chevrons were a vulnerable part of the tail, and interpret the affected individuals as able to recover without too many complications as long as there was no severe functional damage inflicted. [197]
  • Zhao et al (2024) describe a new juvenile–subadult massospondylid specimen from the Lower Jurassic Lufeng Formation (Yunnan, China), increasing known diversity of massospondylids from Asia. [198]
  • "Gyposaurus" sinensis is interpreted as a probable junior synonym of Lufengosaurus huenei by Wang, Zhao & You (2024). [199]
  • Reisz et al. (2024) report that bone development in the femora of Lufengosaurus is closer to that of altricial pigeons than precocious chickens, and argue that Lufengosaurus hatchlings were likely altricial. [200]
  • Barrett & Choiniere (2024) redescribe the skeletal anatomy of Melanorosaurus readi and designate the lectotype of this species. [201]
  • Kareem, Chakraborty & Wilson Mantilla (2024) report evidence of the presence of tail clubs in Kotasaurus yamanpalliensis , sharing morphological similarities with tail clubs of Omeisaurus tianfuensis and Shunosaurus lii . [202]
  • Redescription of the skull anatomy of Bagualia alba is published by Gomez, Carballido & Pol (2024). [203]
  • Using Spinophorosaurus as an example, Vidal (2024) explains how virtual 3D models of sauropods have enabled an understanding of their biomechanics. [204]
  • Agustí, Alcalá & Santos-Cubedo (2024) propose that sauropod gigantism was an adaptation that increased the ability of sauropods to travel great distances, necessitated by pronounced seasonal changes. [205]
  • Butler et al. (2024) describe an assemblage of tracks produced by large-bodied sauropods passing through coastal lagoonal environment from the earliest Cretaceous strata of the Durlston Formation (Dorset, United Kingdom), representing the largest dinosaur track site accessible within the Purbeck Group reported to date. [206]
  • Boisvert et al. (2024) describe a new specimen of Haplocanthosaurus sp. from the Dry Mesa Dinosaur Quarry (Colorado, United States), extending known range of the genus into the true Brushy Basin Member of the Morrison Formation, and likely representing the geologically youngest occurrence of Haplocanthosaurus on the Colorado Plateau. [207]
  • King et al. (2024) report evidence of a previously unknown form of pneumaticity in a rib of a member of the genus Apatosaurus , and propose that rib pneumaticity among apatosaurines is individually variable. [208]
  • Windholz et al. (2024) describe a new rebbachisaurid caudal vertebra from the Cenomanian Candeleros Formation (Argentina), providing new information on the caudal anatomy and pneumaticity in rebbachisaurids. [209]
  • A study on the morphology of teeth of Europasaurus holgeri is published by Régent et al. (2024), who report evidence interpreted as indicative of the presence of a strong connective tissue that partially covered the teeth, and argue that such structure might have been present in other members of Eusauropoda. [210]
  • Gomes et al. (2024) describe a well-preserved trackway of a large sauropod (probably a titanosauriform with a mosaic of basal and derived features) with a unique set of characteristics from the Lower Cretaceous Sousa Formation (Brazil), and name a new ichnotaxon Sousatitanosauripus robsoni . [211]
  • A trackway produced by an early juvenile titanosauriform sauropod is described from the Cenomanian Jindong Formation (South Korea) by Yoon et al. (2024), who compare this trackway with other sauropod trackways from the Jindong Formation, and report evidence that trackway gauges got narrower as pes length increased. [212]
  • Gomez et al. (2024) describe new titanosauriform fossils from the Portezuelo Formation (Argentina), expanding known diversity of sauropods from this formation. [213]
  • A titanosauriform femur belonging to a subadult individual that reached a significantly larger size than other titanosauriform specimens with modified lamellar bone tissue at a similar growth stage is described from the Upper Cretaceous Bayan Shireh Formation (Mongolia) by Witasik, Słowiak & Szczygielski (2024), indicating that the characteristic modified laminar bone tissue of titanosauriform did not prevent those sauropods from achieving large body size. [214]
  • Beeston et al. (2024) describe new sauropod material from the Winton Formation (Australia), and interpret Australotitan cooperensis as an indeterminate diamantinasaurian that is likely a junior synonym of Diamantinasaurus matildae . [215]
  • Filippi et al. (2024) study fossil material of sauropods from the Cerro Overo – La Invernada area (Bajo de la Carpa Formation; Neuquén Province, Argentina), interpreted as suggestive of the presence of a diverse fauna of titanosauriforms coexisting in the environment during the Santonian. [216]
  • A study on the taphonomy of the fossil material of Kaijutitan maui and on its bone histology is published by Filippi, Previtera & Garrido (2024). [217]
  • A study on the tail vertebrae of Adamantisaurus mezzalirai and Baurutitan britoi is published by Vidal et al. (2024), who interpret the studied titanosaurs as keeping their tail close to the ground, with their tails likely functioning as the fifth stabilizing member of the body. [218]
  • Vidal et al. (2024) study the range of motion of the axial series of Trigonosaurus pricei , and interpret it as capable of high elevation of the neck. [219]
  • A study on the morphological variability of titanosaur femora from the Campanian-Maastrichtian Ibero-Armorican domain, providing evidence of the presence of Lirainosaurinae and sauropods with affinities with large-bodied late Maastrichtian titanosaurs, is published by Páramo, Mocho & Ortega (2024). [220]
  • A study on the extent of the postcranial pneumaticity in saltasaurines and other derived titanosaurs is published by Zurriaguz (2024). [221]
  • A description and study of the morphological variability of sauropod appendicular remains from Maastrichtian sites of the Hațeg, Transylvanian, and Rusca Montană basins (Romania) is published by Mocho, Pérez-García & Codrea (2024), who interpret the studied remains as indicative of the presence of four or five sauropod taxa on the Hațeg Island during the Maastrichtian, including a titanosaur lineage with an extremely elongated manus. [222]
  • An overview of the largest known sauropods from Argentina is published by Calvo (2024). [223]

Ornithischian research

Thyreophoran research

  • Satchell (2024) reidentified the proximal femur fragment (BELUM K3998) from the Lias Group of Northern Ireland as an indeterminate dinosaur remain, not a potential specimen of Scelidosaurus or an ornithischian. [230]
  • Castanera, Mampel & Cobos (2024) describe new stegosaur tracks from the Upper Jurassic Villar del Arzobispo Formation (Spain), providing evidence of gregarious behavior in stegosaurs. [231]
  • Sánchez-Fenollosa, Escaso & Cobos (2024) describe a new specimen of Dacentrurus armatus from the Upper Jurassic Villar del Arzobispo Formation (Spain), propose a new diagnosis for this species, and interpret Miragaia longicollum as a junior synonym of D. armatus. [232]
  • Lategano, Conti & Lozar (2024) study the stress resistance of the tail of Miragaia longicollum, interpret its tail as capable of achieving high speed and pressure, but also interpret its tail spines as less robust than those of Stegosaurus stenops , and consider their findings to be indicative of a defensive strategy that prioritized intimidation over direct physical combat. [233]
  • The first stegosaurian fossil material from Gansu (China), assigned to Stegosaurus sp., is described from the Lower Cretaceous Hekou Group by Li et al. (2024). [234]
  • Cross and Arbour (2024) describe an ankylosaur femur from the Cenomanian Dunvegan Formation (British Columbia, Canada). [235]
  • Soto Acuña, Vargas & Kaluza (2024) redescribe the holotype specimen of Antarctopelta from the Snow Hill Island Formation (Antarctica), and provide support for its phylogenetic position within the Parankylosauria. [236]
  • A study on the microstructure and probable developmental origin of small ossicles forming between osteoderms of Antarctopelta oliveroi is published by Sanchez et al. (2024). [237]

Cerapod research

  • Evidence of increase of total tooth volume and rates of tooth wear throughout the evolutionary history of ornithopod dinosaurs is presented by Ősi et al. (2024), who interpret early-diverging ornithopods as likely browsers or frugivores, and that the diets of derived ornithopods likely involved bulk feeding on more resistant, less nutritious forage. [238]
  • Alarcón-Muñoz et al. (2024) describe a vertebra of a non-hadrosauroid iguanodontian from the Lower Cretaceous Quebrada Monardes Formation (Chile), providing evidence of the presence of such ornithopods in the southwestern margin of Gondwana since at least the Early Cretaceous. [239]
  • A review of Early Cretaceous Spanish styracosterns from the Maestrat Basin published by Santos-Cubedo (2024). [240]
  • Escanero-Aguilar et al. (2024) describe skull material of a hadrosauriform ornithopod from the Lower Cretaceous Castrillo de la Reina Formation (Spain), interpreted as more derived than Iguanodon but more basal than Proa , and expanding known diversity of ornithopods from the Cameros Basin. [241]
  • Hayashi et al. (2024) report the discovery of a probable hadrosauroid vertebra from the Upper Cretaceous Hiketa Formation (Izumi Group) in Sanuki, Kagawa Prefecture, providing additional evidence of dispersal of hadrosauriforms into the area of present-day Japan by the Campanian. [242]
  • Nikolov, Dochev, & Brusatte (2024) test the ontogenetic age of small hadrosauroid bones from the Late Cretaceous (Maastrichtian) Kaylaka Formation (Bulgaria), and determine that the specimen likely belonged to a late juvenile or young subadult, rather than a dwarved adult, and suggest that large terrestrial animals were able to populate some European islands via a cyclically appearing or short-lived dispersal route. [243]
  • Van der Linden et al. (2024) describe spheroolithid eggshells from the Maastrichtian Argiles et Grès à Reptiles Formation, probably representing the first hadrosauroid eggshells reported from France, and name a new ootaxon Paraspheroolithus porcarboris . [244]
  • The first described hadrosaurid footprints from the Horseshoe Canyon Formation are described by Powers et al. (2024), who assign them to the ichnospecies Hadrosauropodus langstoni. [245]
  • A study on three bonebeds from the Upper Cretaceous Oldman Formation (Alberta, Canada) and Two Medicine Formation (Montana, United States) preserving remains of specimens of Hypacrosaurus stebingeri is published by Joubarne, Therrien & Zelenitsky (2024), who interpret the studied assemblages as indicating that H. stebingeri individuals lived in age-segregated groups until into their fourth year of life. [246]
  • Evidence from the study of a skull of a juvenile hadrosaurine from the Campanian Dinosaur Park Formation (Alberta, Canada), interpreted as indicative of differences in the dental battery development between hadrosaurid species which might have been related to dietary differences during early ontogeny, is presented by Warnock-Juteau et al. (2024). [247]
  • Sharpe et al. (2024) describe fossil material of a probable immature specimen of Edmontosaurus regalis from the Horseshoe Canyon Formation, and interpret its similarities to Ugrunaaluk kuukpikensis as supporting the referral of the Alaskan saurolophine material to Edmontosaurus cf. regalis. [248]
  • Wick & Lehman (2024) describe fossil material of a juvenile pachycephalosaur specimen belonging to the genus Stegoceras from the Campanian Aguja Formation (Texas, United States), providing new information on the ontogeny of members of this genus, and interpret the holotype of Texacephale langstoni as a probable adult individual belonging to the genus Stegoceras. [249]
  • Hu et al. (2024) reconstruct endocasts of Yinlong , Liaoceratops and Psittacosaurus , and interpret early ceratopsians as having more sensitive sense of smell and as adapted to hearing frequencies than their late-diverging relatives. [250]
  • Description of the morphology of the skull and endocranium of Psittacosaurus sibiricus, based on the study of both juvenile and adult specimens, is published by Podlesnov et al. (2024). [251]
  • A description endocranial anatomy of the Psittacosaurus lujiatunensis published by Sakagami et al. (2024). [252]
  • Yang et al. (2024) describe a well-preserved scaled skin of a specimen of Psittacosaurus from the Early Cretaceous Jehol Biota of China, providing evidence of preservation of epidermal layers, corneocytes and melanosomes, and interpret the studied specimen as indicative of co-occurrence of feathers and reptile-type skin in non-feathered regions of the skin in Psittacosaurus. [253]
  • Witton & Hing (2024) argue that there is no compelling evidence indicating that the development of the idea of the griffin was inspired by the discovery of fossils of Protoceratops . [254]
  • Barrera Guevara et al. (2024) reinterpret fossil material of Coahuilaceratops magnacuerna as derived from Cerro Huerta Formation (and representing the first dinosaur taxon described from this formation) rather than from Cerro del Pueblo Formation. [255]

Birds

New bird taxa

NameNoveltyStatusAuthorsAgeType localityCountryNotesImages

Agapornis longipes [256]

Sp. nov

In press

Pavia et al.

PlioPleistocene transition

Cradle of Humankind

Flag of South Africa.svg  South Africa

A lovebird; a species of Agapornis.

Ardenna buchananbrowni [257]

Sp. nov

Valid

Tennyson et al.

Pliocene (Waipipian)

Tangahoe Formation

Flag of New Zealand.svg  New Zealand

A species of Ardenna .

Avisaurus darwini [258]

Sp. nov

Valid

Clark et al.

Late Cretaceous (Maastrichtian)

Hell Creek Formation

Flag of the United States.svg  United States
(Flag of Montana.svg  Montana)

A member of Enantiornithes belonging to the family Avisauridae.

Avisaurus darwini fossil.png

Buteo chimborazoensis [259]

Sp. nov

Lo Coco, Agnolín & Carrión

Pleistocene

Flag of Ecuador.svg  Ecuador

A species of Buteo .

Chloephaga dabbenei [260]

Sp. nov

Valid

Agnolín, Álvarez Herrera & Tomassini

Pleistocene

Flag of Argentina.svg  Argentina

A species of Chloephaga .

Enkuria [261]

Gen. et sp. et comb. nov

Valid

Zelenkov

Pliocene and Pleistocene

Flag of Crimea.svg  Crimea

A relative of the grey partridge. The type species is E. voinstvenskyi; genus also includes "Phasianus" etuliensis Bocheński & Kurochkin (1987) from Moldova.

Eocypselus geminus [262] Sp. novIn pressMayr & Kitchener Eocene London Clay Flag of the United Kingdom.svg  United Kingdom A species of Eocypselus.
Eocypselus grandissimus [262] Sp. novIn pressMayr & Kitchener Eocene London Clay Flag of the United Kingdom.svg  United Kingdom A species of Eocypselus.
Eocypselus paulomajor [262] Sp. novIn pressMayr & Kitchener Eocene London Clay Flag of the United Kingdom.svg  United Kingdom A species of Eocypselus.
Fluvioviridavis michaeldanielsi [263] Sp. novMayr & Kitchener Eocene London Clay Flag of the United Kingdom.svg  United Kingdom A species of Fluvioviridavis.
Fluvioviridavis nazensis [263] Sp. novMayr & Kitchener Eocene London Clay Flag of the United Kingdom.svg  United Kingdom A species of Fluvioviridavis.

Imparavis [264]

Gen. et sp. nov

In press

Wang et al.

Early Cretaceous

Jiufotang Formation

Flag of the People's Republic of China.svg  China

An enantiornithine. The type species is I. attenboroughi.

Kustokazanser [265]

Gen. et comb. nov

Zelenkov

Late Eocene

Aksyir Svita

Flag of Kazakhstan.svg  Kazakhstan

An anseriform of uncertain placement; a new genus for "Cygnavus" formosus.

Lumbrerornis [266]

Gen. et sp. nov

Valid

Bertelli et al.

Eocene (Lutetian)

Lumbrera Formation

Flag of Argentina.svg  Argentina

A bird of uncertain affinities, possibly related to the families Palaeotididae and Geranoididae. The type species is L. rougieri.

Magnusavis [258]

Gen. et sp. nov

Valid

Clark et al.

Late Cretaceous (Maastrichtian)

Hell Creek Formation

Flag of the United States.svg  United States
(Flag of Montana.svg  Montana)

A member of Enantiornithes. The type species is M. ekalakaenis.

Magnusavis ekalakaenis holotype fossil.png

?Masillatrogon incertus [267]

Sp. nov

Valid

Mayr & Kitchener

Eocene

London Clay

Flag of the United Kingdom.svg  United Kingdom

A trogon.

Melanitta kirbori [268]

Sp. nov

Valid

Zelenkov

Lower Pleistocene

Taurida Cave

Flag of Crimea.svg  Crimea

A scoter; a species of Melanitta.

Miochelidon [269]

Gen. et sp. nov

Volkova

Miocene

Tagay Formation

Flag of Russia.svg  Russia

A swallow. The type species is M. eschata.

Mionetta turgaiensis [265]

Sp. nov

Zelenkov

Early Oligocene

Chelkarnura Formation

Flag of Kazakhstan.svg  Kazakhstan

A species of Mionetta.

Nasiornis [270] Gen. et sp. novIn pressMayr & Kitchener Eocene London Clay Flag of the United Kingdom.svg  United Kingdom A messelornithid. The type species is N. messelornithoides.
Navaornis [271] Gen. et sp. novValid Chiappe et al.Late Cretaceous Adamantina Formation Flag of Brazil.svg  Brazil A member of Enantiornithes. The type species is N. hestiae. Navaornis skull.webp

Paakniwatavis [272]

Gen. et sp. nov

Valid

Musser & Clarke

Eocene

Green River Formation

Flag of the United States.svg  United States
(Flag of Wyoming.svg  Wyoming)

An early member of Anseriformes. The type species is P. grandei.

Paakniwatavis (holotype slab, FMNH PA725).png

Pakudyptes [273]

Gen. et sp. nov

Ando et al.

Late Oligocene

Otekaike Limestone

Flag of New Zealand.svg  New Zealand

An early penguin. The type species is P. hakataramea.

Paralyra [274]

Gen. et comb. nov

Valid

Zelenkov

Pliocene and Pleistocene

Flag of Poland.svg  Poland

A grouse; a new genus for "Lagopus lagopus" atavus Jánossy (1974), originally described from the Rębielice Królewskie 1 locality in Poland, subsequently also described from the Taurida Cave in Crimea. [274]

?Paraortygoides argillae [275]

Sp. nov

Mayr & Kitchener

Eocene (Ypresian)

London Clay

Flag of the United Kingdom.svg  United Kingdom

A member of Galliformes, possibly belonging to the family Gallinuloididae.

? Parvirallus incertus [270] Sp. novIn pressMayr & KitchenerEoceneLondon ClayFlag of the United Kingdom.svg  United Kingdom A messelornithid; a possible species of Parvirallus.
Phalacrocorax bakonyiensis [276] Sp. novValidHorváth, Futó, & Kessler Miocene Flag of Hungary.svg  Hungary A cormorant; a species of Phalacrocorax .

Pristineanis [277]

Gen. et 2 sp. et comb. nov

Valid

Mayr & Kitchener

Eocene

London Clay

Flag of the United Kingdom.svg  United Kingdom
Flag of the United States.svg  United States

A possible member of Piciformes. The type species is P. minor; genus also includes new species P. major, as well as "Neanis" kistneri Feduccia (1973).

Prophaethon waltonensis [278]

Sp. nov

Valid

Mayr & Kitchener

Eocene

London Clay

Flag of the United Kingdom.svg  United Kingdom

A member of the family Prophaethontidae.

Pterodroma zinorum [279]

Sp. nov

Valid

Rando et al.

Quaternary

Flag of Portugal.svg  Portugal
(Flag of the Azores.svg  Azores)

A gadfly petrel.

Septencoracias simillimus [277]

Sp. nov

Valid

Mayr & Kitchener

Eocene (Ypresian)

London Clay

Flag of the United Kingdom.svg  United Kingdom

A stem group roller belonging or related to the family Primobucconidae.

Shuilingornis [280] Gen. et sp. novWang et al. Early Cretaceous Jiufotang FormationFlag of the People's Republic of China.svg  China A euornithe in the family Gansuidae. The type species is S. angelai. Shuilingornis angelai.png

Sulcitarsus [267]

Gen. et sp. nov

Valid

Mayr & Kitchener

Eocene

London Clay

Flag of the United Kingdom.svg  United Kingdom

A bird of uncertain affinities, with similarities of hindlimb elements to those of cuckoo-rollers and members of Accipitriformes. The type species is S. aenigmatus.

Torgos platycephalus [281]

Sp. nov

Valid

Gorbatcheva & Zelenkov

Pleistocene

Flag of Azerbaijan.svg  Azerbaijan

A vulture, a species of Torgos .

Ukugyps [259]

Gen. et sp. nov

Lo Coco, Agnolín & Carrión

Pleistocene

Flag of Ecuador.svg  Ecuador

A condor. The type species is U. orcesi.

Uyrekura [265]

Gen. et sp. nov

Zelenkov

Early Oligocene

Chelkarnura Formation

Flag of Kazakhstan.svg  Kazakhstan

An anatid of uncertain placement. The type species is U. chalkarica.

Walbeckornis waltonensis [270] Sp. novIn pressMayr & KitchenerEoceneLondon ClayFlag of the United Kingdom.svg  United Kingdom A species of Walbeckornis .

Waltonirrisor [277]

Gen. et sp. nov

Valid

Mayr & Kitchener

Eocene (Ypresian)

London Clay

Flag of the United Kingdom.svg  United Kingdom

A member of Upupiformes. The type species is W. tendringensis.

Waltonortyx [275]

Gen. et sp. nov

Mayr & Kitchener

Eocene (Ypresian)

London Clay

Flag of the United Kingdom.svg  United Kingdom

A member of Galliformes, the type genus of the new family Waltonortygidae. The type species is W. bumbanipodiides.

Wunketru [282]

Gen. et comb. nov

Valid

De Mendoza, Degrange & Tambussi

Eocene

Las Flores Formation

Flag of Argentina.svg  Argentina

A member of Anseriformes of uncertain affinites; a new genus for "Telmabates" howardae.

Xenavicula [267]

Gen. et sp. nov

Valid

Mayr & Kitchener

Eocene

London Clay

Flag of the United Kingdom.svg  United Kingdom

A bird of uncertain affinities, with similarities to members of Telluraves, the type genus of the new family Xenaviculidae. The type species is X. pamelae.

Avian research

Pterosaurs

New pterosaur taxa

NameNoveltyStatusAuthorsAgeType localityCountryNotesImages

Akharhynchus [342]

Gen. et sp. nov

Jacobs, Smith & Zouhri

Cretaceous (Albian-Cenomanian)

Ifezouane Formation

Flag of Morocco.svg  Morocco

A member of the family Ornithocheiridae. The type species is A. martilli.

Akharhynchus (holotype rostrum).jpg
Ceoptera [343] Gen. et sp. novValidMartin-Silverstone et al. Middle Jurassic Kilmaluag Formation Flag of the United Kingdom.svg  United Kingdom A darwinopteran. The type species is C. evansae.

Haliskia [344]

Gen. et sp. nov

Valid

Pentland et al.

Early Cretaceous (Albian)

Toolebuc Formation

Flag of Australia (converted).svg  Australia

A member of Anhangueria. The type species is H. peterseni.

Haliskia Life Restoration.png

Inabtanin [345]

Gen. et sp. nov

Rosenbach et al.

Late Cretaceous (Maastrichtian)

Muwaqqar Chalk Marl Formation

Flag of Jordan.svg  Jordan

A member of Azhdarchoidea. The type species is I. alarabia.

Inabtanin Skeletal.svg

Nipponopterus [346]

Gen. et sp. nov

Zhou et al.

Late Cretaceous

Mifune Group

Flag of Japan.svg  Japan

A member of the family Azhdarchidae. The type species is N. mifunensis.

Nipponopterus Skeletal.svg

Propterodactylus [347]

Gen. et sp. nov

Valid

Spindler

Late Jurassic

Painten Formation Flag of Germany.svg  Germany A transitional monofenestratan. The type species is P. frankerlae.

Propterodactylus frankerlae (holotype).jpg

Skiphosoura [348] Gen. et sp. novHone et al. Late Jurassic Mörnsheim Formation Flag of Germany.svg  Germany A transitional pterodactyliform. The type species is S. bavarica.
Torukjara [349] Gen. et sp. novValidPêgas Early Cretaceous Caiuá Group Flag of Brazil.svg  Brazil A tapejarid. The type species is T. bandeirae. Torukjara CP.V 8175.png

Pterosaur research

Other archosaurs

Other new archosaur taxa

NameNoveltyStatusAuthorsAgeType localityCountryNotesImages

Gondwanax [370]

Gen. et sp. nov

In press

Müller

Middle–Late Triassic (Ladinian–early Carnian)

Pinheiros-Chiniquá Sequence of the Santa Maria Supersequence

Flag of Brazil.svg  Brazil

A sulcimentisaurian member of the possibly paraphyletic family Silesauridae. The type species is G. paraisensis.

Gondwanax paraisensis.png

Other archosaur research

General research

Related Research Articles

<i>Aucasaurus</i> Extinct genus of dinosaurs

Aucasaurus is a genus of medium-sized abelisaurid theropod dinosaur from Argentina that lived during the Late Cretaceous of the Anacleto Formation. It was smaller than the related Carnotaurus, although more derived in some ways, such as its extremely reduced arms and almost total lack of fingers. The type skeleton is complete to the thirteenth caudal vertebra, and so is relatively well understood, and is the most complete abelisaurid yet described. However, the skull is damaged, causing some paleontologists to speculate that it was involved in a fight prior to death.

<i>Megaraptor</i> Extinct genus of dinosaurs

Megaraptor is a genus of large theropod dinosaur that lived in the ages of the Late Cretaceous. Its fossils have been discovered in the Patagonian Portezuelo Formation of Argentina, South America. Initially thought to have been a giant dromaeosaur-like coelurosaur, it was classified as a neovenatorid allosauroid in previous phylogenies, but more recent phylogeny and discoveries of related megaraptoran genera has placed it as either a basal tyrannosauroid or a basal coelurosaur with some studies still considering it a neovenatorid.

<span class="mw-page-title-main">Winton Formation</span> Geological formation in Australia

The Winton Formation is a Cretaceous geological formation in central-western Queensland, Australia. It is late Albian to early Turonian in age. The formation blankets large areas of central-western Queensland. It consists of sedimentary rocks such as sandstone, siltstone and claystone. The sediments that make up these rocks represent the remnants of the river plains that filled the basin left by the Eromanga Sea - an inland sea that covered large parts of Queensland and central Australia at least four times during the Early Cretaceous. Great meandering rivers, forest pools and swamps, creeks, lakes and coastal estuaries all left behind different types of sediment.

<span class="mw-page-title-main">Kem Kem Group</span> Geological group in eastern Morocco

The Kem Kem Group is a geological group in the Kem Kem region of eastern Morocco, whose strata date back to the Cenomanian stage of the Late Cretaceous. Its strata are subdivided into two geological formations, with the lower Ifezouane Formation and the upper Aoufous Formation used for the strata on the eastern side of the Atlas Mountains (Tinghir), with the Gara Sbaa Formation and Douira Formation used in the southern Tafilalt region. It is exposed on an escarpment along the Algeria–Morocco border.

The Haman Formation is an Early Cretaceous geological formation in South Korea. It has been dated to the Albian, with an estimated maximum depositional age of 105.4 ± 0.4 Ma. The deposit is known for its tracks, including those of dinosaurs, pterosaurs and birds. It overlies the Silla Conglomerate which overlies the Chilgok Formation. It is laterally equivalent to the Sagog Formation.

<i>Australovenator</i> Extinct genus of dinosaurs

Australovenator is a genus of megaraptoran theropod dinosaur from Cenomanian -age Winton Formation of Australia. Some specimens from the Albian-aged Eumeralla Formation may belong to Australovenator. It is known from partial cranial and postcranial remains which were described in 2009 by Scott Hocknull and colleagues, although additional descriptions and analyses continue to be published. It is the most complete predatory dinosaur discovered in Australia. It has been suggested that Australovenator is a sister taxon to Fukuiraptor, although some phylogenetic analyses find it to be a more derived member of the Megaraptora, possibly being part of the main Megaraptoridae family itself.

<i>Wintonotitan</i> Extinct genus of dinosaurs

Wintonotitan is a genus of titanosauriform dinosaur from Cenomanian -age Winton Formation of Australia. It is known from partial postcranial remains.

The Nanxiong Formation is a Late Cretaceous geologic formation in Guangdong Province. Dinosaur remains are among the fossils that have been recovered from the formation.

The year 2012 in Archosaur paleontology was eventful. Archosaurs include the only living dinosaur group — birds — and the reptile crocodilians, plus all extinct dinosaurs, extinct crocodilian relatives, and pterosaurs. Archosaur palaeontology is the scientific study of those animals, especially as they existed before the Holocene Epoch began about 11,700 years ago. The year 2012 in paleontology included various significant developments regarding archosaurs.

The year 2017 in archosaur paleontology was eventful. Archosaurs include the only living dinosaur group — birds — and the reptile crocodilians, plus all extinct dinosaurs, extinct crocodilian relatives, and pterosaurs. Archosaur palaeontology is the scientific study of those animals, especially as they existed before the Holocene Epoch began about 11,700 years ago. The year 2017 in paleontology included various significant developments regarding archosaurs.

The year 2018 in archosaur paleontology was eventful. Archosaurs include the only living dinosaur group — birds — and the reptile crocodilians, plus all extinct dinosaurs, extinct crocodilian relatives, and pterosaurs. Archosaur palaeontology is the scientific study of those animals, especially as they existed before the Holocene Epoch began about 11,700 years ago. The year 2018 in paleontology included various significant developments regarding archosaurs.

This article records new taxa of fossil archosaurs of every kind that are scheduled described during the year 2019, as well as other significant discoveries and events related to paleontology of archosaurs that are scheduled to occur in the year 2019.

This archosaur paleontology list records new fossil archosauriform taxa that were described during the year 2016, as well as notes other significant Archosaur paleontology discoveries and events which occurred during the year.

This article records new taxa of trace fossils of every kind that are scheduled to be described during the year 2019, as well as other significant discoveries and events related to trace fossil paleontology that are scheduled to occur in the year 2019.

This article records new taxa of fossil archosaurs of every kind that are scheduled described during the year 2020, as well as other significant discoveries and events related to paleontology of archosaurs that are scheduled to occur in the year 2020.

This article records new taxa of fossil archosaurs of every kind that are scheduled described during the year 2021, as well as other significant discoveries and events related to paleontology of archosaurs that are scheduled to occur in the year 2021.

The year 2018 in non-avian dinosaur paleontology was eventful. Archosaurs include the only living dinosaur group — birds — and the reptile crocodilians, plus all extinct dinosaurs, extinct crocodilian relatives, and pterosaurs. Archosaur palaeontology is the scientific study of those animals, especially as they existed before the Holocene Epoch began about 11,700 years ago. This article records new taxa of fossil archosaurs of the non-avian variety that have been described during the year 2018, as well as other significant discoveries and events related to paleontology of archosaurs that occurred in the year 2018.

This article records new taxa of fossil archosaurs of every kind that are scheduled described during the year 2022, as well as other significant discoveries and events related to paleontology of archosaurs that are scheduled to occur in the year 2022.

This article records new taxa of fossil archosaurs of every kind that are scheduled described during the year 2014, as well as other significant discoveries and events related to paleontology of archosaurs that are scheduled to occur in the year 2014.

This article records new taxa of every kind of fossil archosaur that were scheduled to be described during 2023, as well as other significant discoveries and events related to the paleontology of archosaurs that were published in 2023.

References

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