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Kulindadromeus zabaikalicus
Jurassic Herbivore

Kulindadromeus

Kulindadromeus zabaikalicus

"Kulinda runner from Transbaikalia"

Period
Jurassic · Batoniano
Lived
168–166 Ma
Length
up to 1.5 m
Estimated weight
2 kg
Country of origin
Rússia
Described in
2014 by Godefroit, P., Sinitsa, S.M., Dhouailly, D., Bolotsky, Y.L., Sizov, A.V., McNamara, M.E., Benton, M.J., Spagna, P.

Kulindadromeus zabaikalicus is a basal neornithischian from the Middle Jurassic (Bathonian, about 168 to 166 million years ago according to Cincotta et al. 2019) Ukureyskaya Formation, also spelled Ukurey, at the Kulinda locality in the Olov Depression, Chernyshevsky District, Zabaikalsky Krai, southeastern Siberia, Russia. A small bipedal herbivore about 1.5 m long with an estimated mass of 2 kg, it became famous as the first ornithischian with clearly documented complex integumentary cover, a find that unsettled the consensus that feathers were an exclusive trait of coelurosaurian theropods. Godefroit and colleagues, in 2014 in Science, described three types of feather-like filaments at Kulinda: monofilament fuzz covering head and trunk, with simple fibres of constant width comparable to the earliest generation of feather-like structures in Sinosauropteryx; compound tufts of 6 to 7 filaments arising from hexagonal base plates on arms and legs, a previously unknown morphology without exact parallel in theropods; and ribbon-like structures on thigh and tibia, broad, flattened and lacking a defined rachis. Added to these filaments are three scale types: imbricated hexagonal scales on the shins, small rounded scales on hands and feet, and arched rectangular scales on the tail. The simultaneous presence of filaments and scales in the same individual shows that the integumentary morphology of basal dinosaurs was mosaic and suggests that feather-like integument may be plesiomorphic for Dinosauria as a whole rather than restricted to Coelurosauria, radically changing the classical reading that confined feathers to carnivorous theropods. The find overturned the precedent that only Tianyulong and Psittacosaurus bore filamentous structures in Ornithischia, extending the condition to a much older basal ornithischian and geographically anchoring the record in Siberia, outside the Chinese Jehol stage that had dominated feathered fossils. U-Pb dating on detrital zircons and monazites combined with palynology by Cincotta et al. (2019) refined the original age of Godefroit et al. (2014), which pointed to a Bajocian to Tithonian interval (169 to 144 Ma), to Bathonian (168.3 ± 1.3 to 166.1 ± 1.2 Ma), making Kulindadromeus the oldest known dinosaur with unequivocal 'feather-like' structures. The same study synonymised Kulindapteryx ukureica, Daurosaurus olovus and Lepidocheirosaurus natalis, taxa erected by Alifanov and Saveliev in 2014 and 2015 on material from the same bone beds, as nomina dubia likely junior synonyms of Kulindadromeus, simplifying the site's systematics to a single dominant ornithischian taxon. The holotype INREC K3/109, a partial skull with mandibles, is housed at the Institute of Natural Resources, Ecology and Cryology SB RAS in Chita, with referred material distributed across INREC, the Institute of Earth's Crust SB RAS in Irkutsk and the Royal Belgian Institute of Natural Sciences in Brussels, where Paul Spagna prepared the blocks bearing integument. Together, the type skull and the hundreds of disarticulated elements from three bone beds allowed Godefroit and colleagues to reconstruct the animal's nearly complete anatomy and to document the richest record of body cover in a basal ornithischian of the Mesozoic.

Ukureyskaya Formation (or Ukurey), lower part, Olov Depression, Chernyshevsky District, Zabaikalsky Krai, about 220 km east of Chita city, southeastern Siberia, Russia. It is a volcanosedimentary succession with sandstones, siltstones, shales and tuffites deposited in shallow lakes under a recurrent volcanic regime. The original dating in Godefroit et al. (2014) suggested a Bajocian to Tithonian age (169 to 144 Ma). The U-Pb dating on detrital zircons and monazites combined with palynological analysis in Cincotta et al. (2019) refined the age to Bathonian (Middle Jurassic, 168.3 ± 1.3 to 166.1 ± 1.2 Ma), making Kulindadromeus zabaikalicus the oldest known dinosaur with structures clearly interpretable as 'feather-like'. The bone beds are distributed across three fossil horizons rich in ornithischian material, excavated between 2010 and 2013.

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Habitat

Volcanosedimentary lacustrine system on the inner plains of the Siberian continent during the Middle Jurassic. The Ukureyskaya Formation preserves tuffaceous shales, sandstones and siltstones deposited in shallow lakes periodically buried by volcanic ash, under a humid temperate climate. Flora included conifers, ginkgoaleans, ferns and horsetails; associated fauna included insects, crustaceans, fish and other indeterminate small dinosaurs. Recurrent volcanic ash produced Konservat-Lagerstätten responsible for the exceptional preservation of soft tissues.

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Feeding

Small herbivore. The small skull with simple leaf-shaped teeth, short snout with aligned premaxillae, maxillae and dentaries indicates a diet of soft vegetation, leaves, shoots and possibly ginkgoalean and fern fruits. The absence of complex dental batteries places Kulindadromeus among basal neornithischians in terms of feeding specialisation.

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Behavior and senses

Small agile biped, with long hindlimbs adapted for fast running and tail used as a counterweight. The heterogeneous filamentous integument, including compound tufts and ribbon-like structures, supports roles in visual display and intraspecific signalling, plus a possible thermal function in an environment with recurrent ash falls.

Physiology and growth

The extensive filamentous cover on head, neck and trunk suggests at least facultative endothermy. The coexistence with scales (hexagonal on shins, rounded on hands and feet, rectangular on the tail) shows that integumentary morphology was mosaic, consistent with what is observed in living neornithine birds and with the ancestral integument in Dinosauria as a whole.

Continental configuration

Mapa paleogeográfico do Jurassic (~90 Ma)

Ron Blakey · CC BY 3.0 · Jurassic, ~90 Ma

During the Batoniano (~168–166 Ma), Kulindadromeus zabaikalicus inhabited the fragmenting Pangea. North America and Europe were still close, and the North Atlantic was just beginning to open. Climate was warm and humid globally, with no polar ice caps.

Estimated completeness 75%

The genus is known from holotype INREC K3/109 (partial skull with mandibles) and hundreds of disarticulated elements from three main bone beds at Kulinda, including blocks with preserved soft tissues (filament and scale impressions). Taken together, the material allows near-complete skeletal reconstruction from skull to feet and unprecedented documentation of integument in basal ornithischians. Material distributed across INREC SB RAS (Chita), Institute of Earth's Crust SB RAS (Irkutsk) and RBINS (Brussels).

Found (15)
Inferred (3)
Esqueleto de dinossauro — ornithopod
Wikimédia Commons CC BY-SA

Found elements

crânio parcial com mandíbulas (holótipo INREC K3/109)seis crânios referidos adicionaiscentenas de elementos pós-cranianos desarticuladosvértebras cervicais, dorsais, sacrais e caudaiscintura escapular e úmerorádio, ulna e elementos da mãopelve com ílio, ísquio e púbisfêmur, tíbia e fíbulametatarsos e falanges pedaisimpressões de filamentos monofilamentares (tipo 1) em cabeça e troncoimpressões de tufos compostos (tipo 2) de 6 a 7 filamentos em braços e pernasimpressões de estruturas em fita (tipo 3) na coxa e tíbiaescamas hexagonais sobrepostas (tipo 1) nas canelasescamas arredondadas pequenas (tipo 2) nas mãos e pésescamas arqueadas retangulares (tipo 3) na cauda

Inferred elements

porções distais de algumas falangeselementos pequenos da cintura pélvica em alguns indivíduos parciaiscauda completa em comprimento (inferido por extrapolação de vértebras articuladas)

15 papers in chronological order — from the original description to recent research.

2002

Bristle-like integumentary structures at the tail of the horned dinosaur Psittacosaurus

Mayr, G., Peters, D.S., Plodowski, G. e Vogel, O. · Naturwissenschaften 89(8), 361-365

First report of bristle-like integumentary structures in an ornithischian, preserved on the tail of Psittacosaurus specimen SMF R 4970 (Early Cretaceous of China). It set the anatomical precedent for filamentous structures outside Theropoda and became the comparative reference for Kulindadromeus more than a decade later.

Psittacosaurus specimen SMF R 4970, the focus of Mayr et al.'s (2002) description of tail bristles. The fossil offers the closest anatomical parallel for ornithischian integumentary filaments prior to Kulindadromeus.

Psittacosaurus specimen SMF R 4970, the focus of Mayr et al.'s (2002) description of tail bristles. The fossil offers the closest anatomical parallel for ornithischian integumentary filaments prior to Kulindadromeus.

Psittacosaurus skeletal reconstruction showing tail bristles. Mayr et al. (2002) positioned the ornithischian as a precedent of filamentous integument later revisited in Kulindadromeus.

Psittacosaurus skeletal reconstruction showing tail bristles. Mayr et al. (2002) positioned the ornithischian as a precedent of filamentous integument later revisited in Kulindadromeus.

2009

An Early Cretaceous heterodontosaurid dinosaur with filamentous integumentary structures

Zheng, X.-T., You, H.-L., Xu, X. e Dong, Z.-M. · Nature 458(7236), 333-336

Description of Tianyulong confuciusi, a heterodontosaurid from the Tiaojishan Formation (Late Jurassic of China, about 159 Ma), bearing long single filaments along back, neck and tail. It provided the first unequivocal evidence of filamentous structures in Ornithischia and anticipated the reading of Kulindadromeus as ancestral dinosaur integument.

Holotype of Tianyulong confuciusi (STMN 26-3), basis of Zheng, You, Xu and Dong (2009, Nature 458:333). The dorsal filaments are the direct precedent for the filamentous integument later described in Kulindadromeus.

Holotype of Tianyulong confuciusi (STMN 26-3), basis of Zheng, You, Xu and Dong (2009, Nature 458:333). The dorsal filaments are the direct precedent for the filamentous integument later described in Kulindadromeus.

Life reconstruction of Tianyulong with long filaments along the back. The Chinese ornithischian is the closest parallel to Kulindadromeus in the debate on the ancestral origin of feather-like integument.

Life reconstruction of Tianyulong with long filaments along the back. The Chinese ornithischian is the closest parallel to Kulindadromeus in the debate on the ancestral origin of feather-like integument.

Figure 1: New heterodontosaurid ornithischian dinosaur T. confuciusi .

Figure 1: New heterodontosaurid ornithischian dinosaur T. confuciusi .

Figure 2: Integumentary structures of T. confuciusi holotype (STMN 26-3) and others for comparison.

Figure 2: Integumentary structures of T. confuciusi holotype (STMN 26-3) and others for comparison.

Figure 3: Phylogenetic relationships of T. confuciusi and Heterodontosauridae.

Figure 3: Phylogenetic relationships of T. confuciusi and Heterodontosauridae.

2012

A gigantic feathered dinosaur from the Lower Cretaceous of China

Xu, X., Wang, K., Zhang, K., Ma, Q., Xing, L., Sullivan, C., Hu, D., Cheng, S. e Wang, S. · Nature 484(7392), 92-95

Description of Yutyrannus huali, a 9 m tyrannosauroid from the Yixian Formation, with 15 to 20 cm filaments covering much of the body. It expanded the size envelope in which filamentous cover occurs in theropods and established the broad comparative context in which Kulindadromeus was interpreted two years later.

Life reconstruction of Yutyrannus huali, the large feathered tyrannosauroid from the Yixian Formation described by Xu et al. (2012, Nature 484:92), a key component of the scenario in which feather-like cover extends beyond Maniraptora.

Life reconstruction of Yutyrannus huali, the large feathered tyrannosauroid from the Yixian Formation described by Xu et al. (2012, Nature 484:92), a key component of the scenario in which feather-like cover extends beyond Maniraptora.

Lateral view of Yutyrannus huali. The size and climatic setting (cool Yixian) outlined in Xu et al. (2012) widened the debate on the thermal function of feather-like structures, central to the interpretation of Kulindadromeus.

Lateral view of Yutyrannus huali. The size and climatic setting (cool Yixian) outlined in Xu et al. (2012) widened the debate on the thermal function of feather-like structures, central to the interpretation of Kulindadromeus.

Figure 1: Yutyrannus huali (ZCDM V5000 and ZCDM V5001).

Figure 1: Yutyrannus huali (ZCDM V5000 and ZCDM V5001).

Figure 2: Selected elements of Y. huali (ZCDM V5000, ZCDM V5001 and ELDM V1001).

Figure 2: Selected elements of Y. huali (ZCDM V5000, ZCDM V5001 and ELDM V1001).

Figure 3: A simplified cladogram showing the systematic position of Y. huali among the Tyrannosauroidea.

Figure 3: A simplified cladogram showing the systematic position of Y. huali among the Tyrannosauroidea.

2012

Exceptionally preserved juvenile megalosauroid theropod dinosaur with filamentous integument from the Late Jurassic of Germany

Rauhut, O.W.M., Foth, C., Tischlinger, H. e Norell, M.A. · Proceedings of the National Academy of Sciences (PNAS) 109(29), 11746-11751

Description of the juvenile Sciurumimus albersdoerferi, a Late Jurassic megalosauroid from Solnhofen (Germany) with preserved integumentary filaments. It pushed the record of feather-like integument outside Coelurosauria, a condition later consolidated by the discovery of Kulindadromeus in Ornithischia.

Life reconstruction of Sciurumimus albersdoerferi, a juvenile megalosauroid with filaments described by Rauhut et al. (2012, PNAS 109:11746). The taxon anticipated the spread of feather-like integument beyond Coelurosauria, later extended to Kulindadromeus.

Life reconstruction of Sciurumimus albersdoerferi, a juvenile megalosauroid with filaments described by Rauhut et al. (2012, PNAS 109:11746). The taxon anticipated the spread of feather-like integument beyond Coelurosauria, later extended to Kulindadromeus.

Tail detail of Sciurumimus, with preserved pigmentation pattern. Rauhut et al. (2012) used these impressions to argue that filaments were a basal trait in theropods, later converging with the ornithischian reading of Kulindadromeus.

Tail detail of Sciurumimus, with preserved pigmentation pattern. Rauhut et al. (2012) used these impressions to argue that filaments were a basal trait in theropods, later converging with the ornithischian reading of Kulindadromeus.

2014

A Jurassic ornithischian dinosaur from Siberia with both feathers and scales

Godefroit, P., Sinitsa, S.M., Dhouailly, D., Bolotsky, Y.L., Sizov, A.V., McNamara, M.E., Benton, M.J. e Spagna, P. · Science 345(6195), 451-455

Original description of Kulindadromeus zabaikalicus based on holotype INREC K3/109 and on hundreds of disarticulated elements from Kulinda (Ukureyskaya Formation). Documents three filament types (monofilament fuzz, compound tufts, ribbon-like structures) and three scale types, suggesting that feather-like integument may be plesiomorphic for Dinosauria.

Mounted partial skeleton of Kulindadromeus zabaikalicus, the type of material that underpinned the original description by Godefroit et al. (2014, Science 345:451).

Mounted partial skeleton of Kulindadromeus zabaikalicus, the type of material that underpinned the original description by Godefroit et al. (2014, Science 345:451).

Composite figure of Kulindadromeus skeleton and integument (reproduced in Cincotta et al. 2019, PeerJ). Type material INREC K3/109 and referred elements described by Godefroit et al. (2014, Science 345:451) show the distribution of filaments and scales on the body.

Composite figure of Kulindadromeus skeleton and integument (reproduced in Cincotta et al. 2019, PeerJ). Type material INREC K3/109 and referred elements described by Godefroit et al. (2014, Science 345:451) show the distribution of filaments and scales on the body.

2014

Comment on "A Jurassic ornithischian dinosaur from Siberia with both feathers and scales"

Lingham-Soliar, T. · Science 346(6208), 434

Critical comment questioning the interpretation of Kulindadromeus filaments as protofeathers, proposing instead that the compound structures around humerus and femur are support fibres of degraded scales. It framed the main debate on the homology of feather-like integument in ornithischians.

Skeletal elements of Kulindadromeus used in comparative figures. Critical works like Lingham-Soliar (2014) drew on this kind of material to discuss the taphonomy and nature of the filamentous structures.

Skeletal elements of Kulindadromeus used in comparative figures. Critical works like Lingham-Soliar (2014) drew on this kind of material to discuss the taphonomy and nature of the filamentous structures.

Life-size Psittacosaurus model with countershading pattern (figure from Vinther et al. 2016). The contrast between caudal filaments and scales is central to the debate Lingham-Soliar (2014) opened about Kulindadromeus.

Life-size Psittacosaurus model with countershading pattern (figure from Vinther et al. 2016). The contrast between caudal filaments and scales is central to the debate Lingham-Soliar (2014) opened about Kulindadromeus.

2014

Response to Comment on "A Jurassic ornithischian dinosaur from Siberia with both feathers and scales"

Godefroit, P., McNamara, M.E., Dhouailly, D. e Benton, M.J. · Science 346(6208), 434

Formal response of the original authors to Lingham-Soliar's critique. They reaffirm, based on electron microscopy and experimental decay, that Kulindadromeus filaments have constant width, keratinous behaviour and are incompatible with collagen fibres, supporting homology with basal feathers.

Monofilament type-1 filaments of Kulindadromeus under microscopy (figure from Cincotta et al. 2019, PeerJ). Godefroit et al. (2014b) used images of this type to argue against the collagen interpretation.

Monofilament type-1 filaments of Kulindadromeus under microscopy (figure from Cincotta et al. 2019, PeerJ). Godefroit et al. (2014b) used images of this type to argue against the collagen interpretation.

Microstructural details of Kulindadromeus filaments. Godefroit et al. (2014b) highlighted the constant width and keratinous behaviour, incompatible with collagen fibres.

Microstructural details of Kulindadromeus filaments. Godefroit et al. (2014b) highlighted the constant width and keratinous behaviour, incompatible with collagen fibres.

2014

Two new ornithischian dinosaurs (Hypsilophodontia, Ornithopoda) from the Late Jurassic of Russia

Alifanov, V.R. e Saveliev, S.V. · Paleontological Journal 48(4), 414-425

Description of Kulindapteryx ukureica and Daurosaurus olovus based on material collected at Kulinda, interpreted as distinct ornithopods. Subsequent studies (Cincotta et al. 2019) concluded they are likely junior synonyms of Kulindadromeus and should be treated as nomina dubia.

Hypsilophodontid evolutionary tree of the kind used in discussions following Alifanov and Saveliev (2014), which sought to place the putative new Kulinda taxa within the group.

Hypsilophodontid evolutionary tree of the kind used in discussions following Alifanov and Saveliev (2014), which sought to place the putative new Kulinda taxa within the group.

Cladogram of heterodontosaurids and basal ornithopods (Sereno 2012) used in discussions of the phylogenetic position of Kulindapteryx and Daurosaurus, later reunified with Kulindadromeus.

Cladogram of heterodontosaurids and basal ornithopods (Sereno 2012) used in discussions of the phylogenetic position of Kulindapteryx and Daurosaurus, later reunified with Kulindadromeus.

2015

The systematic relationships and biogeographic history of ornithischian dinosaurs

Boyd, C.A. · PeerJ 3, e1523

Phylogenetic analysis with 255 characters and 65 terminal taxa, the largest at the time for basal ornithischians. It provides the framework in which Kulindadromeus fits as a non-cerapodan neornithischian, and confirms that old 'Hypsilophodontidae' are paraphyletic.

Figure 1 of Boyd (2015, PeerJ): recent phylogenetic hypotheses for Ornithischia compared. The framework underpins the basal position of neornithischians such as Kulindadromeus, outside Cerapoda.

Figure 1 of Boyd (2015, PeerJ): recent phylogenetic hypotheses for Ornithischia compared. The framework underpins the basal position of neornithischians such as Kulindadromeus, outside Cerapoda.

Figure 2 of Boyd (2015, PeerJ): strict consensus tree of basal ornithischians, with 'hypsilophodontids' treated as a paraphyletic group. This is the scenario in which Kulindadromeus fits as a pre-cerapodan neornithischian.

Figure 2 of Boyd (2015, PeerJ): strict consensus tree of basal ornithischians, with 'hypsilophodontids' treated as a paraphyletic group. This is the scenario in which Kulindadromeus fits as a pre-cerapodan neornithischian.

2014

New specimen of Archaeopteryx provides insights into the evolution of pennaceous feathers

Foth, C., Tischlinger, H. e Rauhut, O.W.M. · Nature 511(7507), 79-82

Description of the 11th Archaeopteryx specimen, with pennaceous feather pattern on limbs and tail. It provides the avian context contemporary to Kulindadromeus within a broader feather evolution scenario, clearly distinguishing pennaceous from filamentous morphotypes.

Life reconstruction of Anchiornis huxleyi, a feathered paravian from the Chinese Jurassic. The comparative context introduced by Foth et al. (2014) highlights how pennaceous forms differ from the Kulindadromeus filaments.

Life reconstruction of Anchiornis huxleyi, a feathered paravian from the Chinese Jurassic. The comparative context introduced by Foth et al. (2014) highlights how pennaceous forms differ from the Kulindadromeus filaments.

Anchiornis huxleyi in detail, a representative of feathered paravians. The evolutionary scenario articulated by Foth et al. (2014) places Kulindadromeus at the base of the same integumentary system in a plesiomorphic version.

Anchiornis huxleyi in detail, a representative of feathered paravians. The evolutionary scenario articulated by Foth et al. (2014) places Kulindadromeus at the base of the same integumentary system in a plesiomorphic version.

2015

A new psittacosaurid dinosaur (Psittacosauridae, Ornithischia) from the Late Jurassic of Transbaikalia

Alifanov, V.R. e Saveliev, S.V. · Paleontological Journal 49(5), 517-526

Description of Lepidocheirosaurus natalis, a putative Jurassic psittacosaurid from Kulinda. The detailed analysis of Cincotta et al. (2019) considers the material indistinguishable from Kulindadromeus and treats the taxon as a junior synonym and nomen dubium.

Size comparison among heterodontosaurids. Discussions after Alifanov and Saveliev (2015) use this kind of reference to contrast the putative psittacosaurid Lepidocheirosaurus with the Siberian Kulindadromeus.

Size comparison among heterodontosaurids. Discussions after Alifanov and Saveliev (2015) use this kind of reference to contrast the putative psittacosaurid Lepidocheirosaurus with the Siberian Kulindadromeus.

Transparent version of the Kulindadromeus reconstruction (Nobu Tamura), used for direct comparisons with the putative taxa Kulindapteryx, Daurosaurus and Lepidocheirosaurus, now synonymised.

Transparent version of the Kulindadromeus reconstruction (Nobu Tamura), used for direct comparisons with the putative taxa Kulindapteryx, Daurosaurus and Lepidocheirosaurus, now synonymised.

2016

3D camouflage in an ornithischian dinosaur

Vinther, J., Nicholls, R., Lautenschlager, S., Pittman, M., Kaye, T.G., Rayfield, E., Mayr, G. e Cuthill, I.C. · Current Biology 26(18), 2456-2462

3D reconstruction of Psittacosaurus SMF R 4970 pigmentation based on preserved melanosomes, revealing pronounced countershading. The work demonstrates how much integumentary information can be recovered from Cretaceous ornithischians, and acts as a counterpoint to Kulindadromeus, the older and more basal feathered ornithischian.

Figure 1 of Vinther et al. (2016, Current Biology): Psittacosaurus specimen SMF R 4970 in overall view, basis of the 3D pigment reconstruction complementary to the filamentous integument described in Kulindadromeus.

Figure 1 of Vinther et al. (2016, Current Biology): Psittacosaurus specimen SMF R 4970 in overall view, basis of the 3D pigment reconstruction complementary to the filamentous integument described in Kulindadromeus.

Figure 2 of Vinther et al. (2016, Current Biology): regional distribution of melanosomes in Psittacosaurus. The method provides the Cretaceous pigmentary counterpart to the Jurassic integument of Kulindadromeus.

Figure 2 of Vinther et al. (2016, Current Biology): regional distribution of melanosomes in Psittacosaurus. The method provides the Cretaceous pigmentary counterpart to the Jurassic integument of Kulindadromeus.

2019

The rise of feathered dinosaurs: Kulindadromeus zabaikalicus, the oldest dinosaur with "feather-like" structures

Cincotta, A., Pestchevitskaya, E.B., Sinitsa, S.M., Markevich, V.S., Debaille, V., Reshetova, S.A., Mashchuk, I.M., Frolov, A.O., Gerdes, A., Yans, J. e Godefroit, P. · PeerJ 7, e6239

Comprehensive redescription of Kulindadromeus integument and U-Pb dating of detrital zircons and monazites, combined with palynological analysis. It concludes a Bathonian age (168.3 ± 1.3 to 166.1 ± 1.2 Ma) and synonymises Kulindapteryx, Daurosaurus and Lepidocheirosaurus with Kulindadromeus. It makes the taxon the oldest dinosaur with unequivocal 'feather-like' structures.

Figure 3 of Cincotta et al. (2019, PeerJ): compound type-2 structures and type-3 ribbon-like structures of Kulindadromeus, the core of the argument against Lingham-Soliar's collagen interpretation.

Figure 3 of Cincotta et al. (2019, PeerJ): compound type-2 structures and type-3 ribbon-like structures of Kulindadromeus, the core of the argument against Lingham-Soliar's collagen interpretation.

Figure 5 of Cincotta et al. (2019, PeerJ): type-1 imbricated hexagonal scales and type-2 small rounded scales of Kulindadromeus, a key diagnostic for the coexistence of scales and filaments in the same organism.

Figure 5 of Cincotta et al. (2019, PeerJ): type-1 imbricated hexagonal scales and type-2 small rounded scales of Kulindadromeus, a key diagnostic for the coexistence of scales and filaments in the same organism.

Figure 1: Location of the studied area. (A) Position of Kulinda locality with respect to the Mongol-Okhotsk suture (modified with permission from Tomurtogoo et al., 2005 ). (B) Geological map of the Kulinda region (redrawn with permission from Kozlov, Zaikov & Karasev, 1998 ). According to the map, Kulinda is situated in the Upper Jurassic of the Ukurey Formation. Download full-size image DOI: 10.7717/peerj.6239/fig-1

Figure 1: Location of the studied area. (A) Position of Kulinda locality with respect to the Mongol-Okhotsk suture (modified with permission from Tomurtogoo et al., 2005 ). (B) Geological map of the Kulinda region (redrawn with permission from Kozlov, Zaikov & Karasev, 1998 ). According to the map, Kulinda is situated in the Upper Jurassic of the Ukurey Formation. Download full-size image DOI: 10.7717/peerj.6239/fig-1

Figure 2: Lithological section of the Kulinda dinosaur locality in the Ukurey Formation. (A) Composite stratigraphic log of the three trenches and the position of the bone beds. (B) Schematic location of the trenches excavated on the hillslope. (C) Photograph showing the location of the three parallel trenches on site (photo credit: A. Cincotta). The locations of the detrital samples used for dating are marked by an arrow. Download full-size image DOI: 10.7717/peerj.6239/fig-2

Figure 2: Lithological section of the Kulinda dinosaur locality in the Ukurey Formation. (A) Composite stratigraphic log of the three trenches and the position of the bone beds. (B) Schematic location of the trenches excavated on the hillslope. (C) Photograph showing the location of the three parallel trenches on site (photo credit: A. Cincotta). The locations of the detrital samples used for dating are marked by an arrow. Download full-size image DOI: 10.7717/peerj.6239/fig-2

Figure 3: Probability curve based on the LA-ICP-MS data performed on zircons and monazites. Two age populations (i.e., peaks) can be discriminated from this curve. Download full-size image DOI: 10.7717/peerj.6239/fig-3

Figure 3: Probability curve based on the LA-ICP-MS data performed on zircons and monazites. Two age populations (i.e., peaks) can be discriminated from this curve. Download full-size image DOI: 10.7717/peerj.6239/fig-3

Figure 4: Concordia diagrams for the three samples collected at Kulinda. (A) Zircons and monazites collected from the granite. (B) Zircons collected from a sample situated above bone bed 3 in trench 3. (C) Zircons collected from a sample situated below bone bed 4 in trench 4. Download full-size image DOI: 10.7717/peerj.6239/fig-4

Figure 4: Concordia diagrams for the three samples collected at Kulinda. (A) Zircons and monazites collected from the granite. (B) Zircons collected from a sample situated above bone bed 3 in trench 3. (C) Zircons collected from a sample situated below bone bed 4 in trench 4. Download full-size image DOI: 10.7717/peerj.6239/fig-4

2022

The exquisitely preserved integument of Psittacosaurus and the scaly skin of ceratopsian dinosaurs

Bell, P.R., Hendrickx, C., Pittman, M., Kaye, T.G. e Mayr, G. · Communications Biology 5, 809

Laser-stimulated fluorescence (LSF) reanalysis of Psittacosaurus specimen SMF R 4970. It maps heterogeneous scalation by body region, cloaca, umbilicus and a keratinous sheath. It complements the repertoire of known ornithischian integument and offers a Cretaceous counterpart to the Jurassic Kulindadromeus.

Scale comparison of psittacosaurids. The integumentary diversity of these Cretaceous ornithischians, restudied by Bell et al. (2022), complements the Jurassic record of Kulindadromeus.

Scale comparison of psittacosaurids. The integumentary diversity of these Cretaceous ornithischians, restudied by Bell et al. (2022), complements the Jurassic record of Kulindadromeus.

Dinosauria phylogeny with integument mapping, of the kind used to contextualise Bell et al. (2022) and Cincotta et al. (2019). Kulindadromeus appears as an ancient node of feather-like integument in Ornithischia.

Dinosauria phylogeny with integument mapping, of the kind used to contextualise Bell et al. (2022) and Cincotta et al. (2019). Kulindadromeus appears as an ancient node of feather-like integument in Ornithischia.

Fig. 1: Psittacosaurus sp. (SMF R 4970) under laser-stimulated fluorescence (LSF) and distribution of different integumentary types.

Fig. 1: Psittacosaurus sp. (SMF R 4970) under laser-stimulated fluorescence (LSF) and distribution of different integumentary types.

Fig. 2: Integument of the head and neck of Psittacosaurus SMF R 4970 under LSF.

Fig. 2: Integument of the head and neck of Psittacosaurus SMF R 4970 under LSF.

Fig. 3: Integument of the forelimb and pectoral region of Psittacosaurus SMF R 4970 under LSF.

Fig. 3: Integument of the forelimb and pectoral region of Psittacosaurus SMF R 4970 under LSF.

Fig. 4: Abdominal skin in Psittacosaurus SMF R 4970 under LSF.

Fig. 4: Abdominal skin in Psittacosaurus SMF R 4970 under LSF.

2021

The phylogenetic nomenclature of ornithischian dinosaurs

Madzia, D., Arbour, V.M., Boyd, C.A., Farke, A.A., Cruzado-Caballero, P. e Evans, D.C. · PeerJ 9, e12362

Comprehensive review of phylogenetic definitions of Ornithischia clades, including Neornithischia, Cerapoda and Ornithopoda, in the spirit of the PhyloCode. It provides the formal framework in which Kulindadromeus is labelled as a basal non-cerapodan neornithischian.

Biogeography of heterodontosaurids used as context for Madzia et al. (2021). The nomenclatural review places Kulindadromeus outside Heterodontosauria, on a Siberian branch of basal neornithischians.

Biogeography of heterodontosaurids used as context for Madzia et al. (2021). The nomenclatural review places Kulindadromeus outside Heterodontosauria, on a Siberian branch of basal neornithischians.

Hexinlusaurus multidens, a Middle Jurassic basal neornithischian from China, close sister taxon to Kulindadromeus in several analyses. The framework of Madzia et al. (2021) supports this phylogenetic neighbourhood.

Hexinlusaurus multidens, a Middle Jurassic basal neornithischian from China, close sister taxon to Kulindadromeus in several analyses. The framework of Madzia et al. (2021) supports this phylogenetic neighbourhood.

INREC K3/109 — Institute of Natural Resources, Ecology and Cryology SB RAS, Chita

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INREC K3/109

Institute of Natural Resources, Ecology and Cryology SB RAS, Chita

Completeness: crânio parcial com maxilar
Found in: 2010
By: Sofia Sinitsa

Holotype designated by Godefroit et al. (2014, Science 345:451). Partial skull with mandibles from the lower Kulinda bone bed in the Ukureyskaya Formation, basis of the diagnosis of Kulindadromeus zabaikalicus. The associated referred material, comprising hundreds of postcranial elements and blocks with integument, is distributed across INREC (Chita), the Institute of Earth's Crust SB RAS (Irkutsk) and RBINS (Brussels), where Paul Spagna prepared the fragments bearing filaments and scales.

Dinosauria
Ornithischia
Neornithischia
Kulindadromeus
First fossil
2010
Discoverer
Sofia Sinitsa e equipe
Formal description
2014
Described by
Godefroit, P., Sinitsa, S.M., Dhouailly, D., Bolotsky, Y.L., Sizov, A.V., McNamara, M.E., Benton, M.J., Spagna, P.
Formation
Formação Ukureyskaya
Region
Zabaikalsky Krai
Country
Rússia
📄 Original description paper

Fun fact

Before Kulindadromeus, some people hoped that feathers would remain a theropod-only affair, confined to the 'carnivorous' side of the dinosaur tree. In 2014, Pascal Godefroit and colleagues published in Science a small Siberian bipedal herbivore about 1.5 m long with not one but three variants of filamentous integument, from simple fuzz to compound tufts and the strange ribbon-like structures on the legs, all in a basal ornithischian older than Archaeopteryx. In 2019, U-Pb zircon dating fixed the age as Bathonian, around 167 Ma, crowning Kulindadromeus as the oldest feathered dinosaur known to date and reinforcing the hypothesis that feather-like integument is an ancestral trait of all Dinosauria, rather than a late invention of coelurosaurs.