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Chine

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82 image(s) · 38 Actualités

Galerie d'images

Changmiania liaoningensis, an ornithopod dinosaur from the Lower Cretaceous of Lujiatun (Liaoning Province, China).
(A) Holotype PMOL AD00114 in dorsal view; (B) anterior part of the holotype PMOL AD00114 in caudolateral view; (C) referred specimen PMOL LFV022 in dorsal view. Red arrows indicate the emplacement of the gastrolith clusters.
Taxons Changmiania

Changmiania liaoningensis, an ornithopod dinosaur from the Lower Cretaceous of Lujiatun (Liaoning Province, China). (A) Holotype PMOL AD00114 in dorsal view; (B) anterior part of the holotype PMOL AD00114 in caudolateral view; (C) referred specimen PMOL LFV022 in dorsal view. Red arrows indicate the emplacement of the gastrolith clusters.

Chine Crétacé holotype spécimen +2
Life restoration of the Triassic ichthyosaur Callawayia neoscapularis. Three specimens of this ichthyosaur are known, the holotype, ROM 41993, and two referred specimens, TMP 94.380.11 and 94.382.2. The skull is primarily based on ROM 41993, cross-checked against TMP 94.380.11 and TMP 94.382.2. The vertebral column is based primarily on TMP 94.382.2 as it is the most complete of these specimens, while the ribs were based on ROM 41993. The forelimbs were mainly based on those of ROM 41993, with TMP 94.380.11 used to determine their breadth. The hindlimbs were based on TMP 94.380.11, especially the more complete right hindlimb.
ROM 41993 was cross-scaled with TMP 94.380.11 by the dimensions of the forelimb epipodials, which produced similar vertebral dimensions. The two TMP specimens were cross-scaled based on femoral length, also producing similar vertebral dimensions. Nicholls & Manabe (2001) stated that no wedge-shaped caudal centra supporting a tailbend were found and that there was no evidence of a bend being present, though considered that they might have existed in the gap in the preserved caudals. Since various other Triassic ichthyosaurs have since been found to have tail bends, one was illustrated here. A modest downturn of roughly 15° was illustrated, comparable to that in Guanlingsaurus, and the location of the bend within the gap in the preserved vertebrae matches well with the location of the bend in Guizhouichthyosaurus.

References
McGowan, C. (1994). "A new species of Shastasaurus (Reptilia: Ichthyosauria) from the Triassic of British Columbia: The most complete exemplar of the genus". Journal of Vertebrate Paleontology 14 (2): 168–179. DOI:10.1080/02724634.1994.10011550.
Nicholls, E. L.; Manabe, M. (2001). "A new genus of ichthyosaur from the Late Triassic Pardonet Formation of British Columbia: Bridging the Triassic-Jurassic gap". Canadian Journal of Earth Sciences 38 (6): 983–1002.
Ji, C.; Jiang, D.Y.; Hao, W.; Sun, Y. (2011). "True tailbend occurred in the Late Triassic: Evidence from ichthyosaur skeletons of South China". Acta Scientiarum Naturalium Universitatis Pekinensis 47 (2): 309–314.
Shang, Q. H.; Li, C. (2009). "On the occurrence of the ichthyosaur Shastasaurus in the Guanling biota (Late Triassic), Guizhou, China". Vertebrata PalAsiatica 47 (3): 178–193.
Taxons Guanlingsaurus

Life restoration of the Triassic ichthyosaur Callawayia neoscapularis. Three specimens of this ichthyosaur are known, the holotype, ROM 41993, and two referred specimens, TMP 94.380.11 and 94.382.2. The skull is primarily based on ROM 41993, cross-checked against TMP 94.380.11 and TMP 94.382.2. The vertebral column is based primarily on TMP 94.382.2 as it is the most complete of these specimens, while the ribs were based on ROM 41993. The forelimbs were mainly based on those of ROM 41993, with TMP 94.380.11 used to determine their breadth. The hindlimbs were based on TMP 94.380.11, especially the more complete right hindlimb. ROM 41993 was cross-scaled with TMP 94.380.11 by the dimensions of the forelimb epipodials, which produced similar vertebral dimensions. The two TMP specimens were cross-scaled based on femoral length, also producing similar vertebral dimensions. Nicholls & Manabe (2001) stated that no wedge-shaped caudal centra supporting a tailbend were found and that there was no evidence of a bend being present, though considered that they might have existed in the gap in the preserved caudals. Since various other Triassic ichthyosaurs have since been found to have tail bends, one was illustrated here. A modest downturn of roughly 15° was illustrated, comparable to that in Guanlingsaurus, and the location of the bend within the gap in the preserved vertebrae matches well with the location of the bend in Guizhouichthyosaurus. References McGowan, C. (1994). "A new species of Shastasaurus (Reptilia: Ichthyosauria) from the Triassic of British Columbia: The most complete exemplar of the genus". Journal of Vertebrate Paleontology 14 (2): 168–179. DOI:10.1080/02724634.1994.10011550. Nicholls, E. L.; Manabe, M. (2001). "A new genus of ichthyosaur from the Late Triassic Pardonet Formation of British Columbia: Bridging the Triassic-Jurassic gap". Canadian Journal of Earth Sciences 38 (6): 983–1002. Ji, C.; Jiang, D.Y.; Hao, W.; Sun, Y. (2011). "True tailbend occurred in the Late Triassic: Evidence from ichthyosaur skeletons of South China". Acta Scientiarum Naturalium Universitatis Pekinensis 47 (2): 309–314. Shang, Q. H.; Li, C. (2009). "On the occurrence of the ichthyosaur Shastasaurus in the Guanling biota (Late Triassic), Guizhou, China". Vertebrata PalAsiatica 47 (3): 178–193.

Chine Jurassique Trias supérieur Trias +12
Prismatoolithus tiantaiensis eggs (IVPP V16515) on display at the Paleozoological Museum of China.
Taxons Prismatoolithidae

Prismatoolithus tiantaiensis eggs (IVPP V16515) on display at the Paleozoological Museum of China.

musée Chine Prismatoolithidae Prismatoolithus
Prismatoolithus tiantaiensis eggs (IVPP V16515) on display at the Paleozoological Museum of China.
Taxons Prismatoolithus

Prismatoolithus tiantaiensis eggs (IVPP V16515) on display at the Paleozoological Museum of China.

musée Chine Prismatoolithidae Prismatoolithus
Prismatoolithus tiantaiensis eggs (IVPP V16515) on display at the Paleozoological Museum of China.
Taxons Prismatoolithus

Prismatoolithus tiantaiensis eggs (IVPP V16515) on display at the Paleozoological Museum of China.

musée Chine Prismatoolithidae Prismatoolithus
Elangatoolithidae fossil dinosaur eggs, from China. Exhibit in the Academy of Natural Sciences, 1900 Benjamin Franklin Parkway, Philadelphia, Pennsylvania, USA. Photography was permitted in this area of the museum without restrictions.
Taxons Elongatoolithidae

Elangatoolithidae fossil dinosaur eggs, from China. Exhibit in the Academy of Natural Sciences, 1900 Benjamin Franklin Parkway, Philadelphia, Pennsylvania, USA. Photography was permitted in this area of the museum without restrictions.

musée Chine États-Unis fossile +2
Earth during the Middle Ordivician Period @ 460 Ma. Gondwana is seen above the equator (Australia & South China) and bellow the equator (North China, Kazakh terranes, Tarim, Antartica, India, Madagascar, Africa and South America). Laurentia, Baltica & Sibera are seperate continents, with Avalonia on its way to collide Baltica to form the Calledonian Orogeny, and Acadia on its way to collide Laurentia to form the Acadian Orogeny.
Legend:

Dark blue = ocean
Light blue = shallow seas
Tan = landmass
Black outlines = modern day coastlines showing their respective positions
Intervalles Darriwilian

Earth during the Middle Ordivician Period @ 460 Ma. Gondwana is seen above the equator (Australia & South China) and bellow the equator (North China, Kazakh terranes, Tarim, Antartica, India, Madagascar, Africa and South America). Laurentia, Baltica & Sibera are seperate continents, with Avalonia on its way to collide Baltica to form the Calledonian Orogeny, and Acadia on its way to collide Laurentia to form the Acadian Orogeny. Legend: Dark blue = ocean Light blue = shallow seas Tan = landmass Black outlines = modern day coastlines showing their respective positions

Australie Chine Inde Madagascar +1
West of Chilton Chine The coastline west of the chine is accessible at lowish tides.  The various rock strata in the Wealden Beds can be seen, with the chalk of Highdown Cliffs SZ3285 beyond.
Formations Wessex

West of Chilton Chine The coastline west of the chine is accessible at lowish tides. The various rock strata in the Wealden Beds can be seen, with the chalk of Highdown Cliffs SZ3285 beyond.

Chine
Fossil of Mei long (holotype), on temporary display at the Shanghai Natural History Museum as part of the exhibition "China's Dinosaur World". Shot on July 22, 2025.
Taxons Mei

Fossil of Mei long (holotype), on temporary display at the Shanghai Natural History Museum as part of the exhibition "China's Dinosaur World". Shot on July 22, 2025.

musée Chine fossile holotype +1
Fossil specimen (IVPP V17903) of Corpulentapus lilasia on display at the Paleozoological Museum of China.
Taxons Corpulentapus

Fossil specimen (IVPP V17903) of Corpulentapus lilasia on display at the Paleozoological Museum of China.

musée Chine fossile spécimen +1
Holotype of Ikrandraco avatar on display at the Paleozoological Museum of China.
Taxons Ikrandraco

Holotype of Ikrandraco avatar on display at the Paleozoological Museum of China.

musée Chine holotype Ikrandraco +1
Holotype specimen (GMV2128) of Dendrorhynchoides curvidentatus on display at the Geological Museum of China.
Taxons Dendrorhynchoides

Holotype specimen (GMV2128) of Dendrorhynchoides curvidentatus on display at the Geological Museum of China.

musée Chine holotype spécimen +1
Holotype skeleton of Jianchangnathus robustus on display at the Paleozoological Museum of China.
Taxons Jianchangnathus

Holotype skeleton of Jianchangnathus robustus on display at the Paleozoological Museum of China.

musée Chine holotype Jianchangnathus +1
Holotype skeleton (AGB 6257) of Cartorhynchus lenticarpus on display at the Geological Museum of China.

Holotype skeleton (AGB 6257) of Cartorhynchus lenticarpus on display at the Geological Museum of China.

musée Chine holotype squelette
Reconstruction of skeleton; Lower Cretaceous (120 mio. Years); Jungar Basin, China.
Taxons Dsungaripteridae

Reconstruction of skeleton; Lower Cretaceous (120 mio. Years); Jungar Basin, China.

Chine Crétacé Dsungaripteridae Dsungaripterus +1
Reconstruction of skeleton; Lower Cretaceous (120 mio. Years); Jungar Basin, China.
Taxons Dsungaripterus

Reconstruction of skeleton; Lower Cretaceous (120 mio. Years); Jungar Basin, China.

Chine Crétacé Dsungaripteridae Dsungaripterus +1
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Actualités

520-Million-Year-Old Fossil from China Fills Gap in Evolutionary History of Cephalopods
Un fossile chinois vieux de 520 millions d’années comble une lacune dans l’histoire évolutive des céphalopodes
Chine Cambrien fossile évolution
Les paléontologues ont identifié le plus ancien céphalopode connu équipé d'un siphoncle - une extension tubulaire du manteau trouvée chez les céphalopodes à coquille - remontant les archives fossiles de cette caractéristique clé de l'évolution au Cambrien inférieur, il y a environ 520 millions d'années. L'article Un fossile chinois vieux de 520 millions d'années comble une lacune dans l'histoire évolutive des céphalopodes est apparu en premier sur Sci.News : Breaking Science News.
30/07/2026 sci-news ⚙ Traduction automatique
C’est une découverte exceptionnelle : cet ambre est si vieux qu'il a été fabriqué avant que le moindre animal ne marche sur la Terre ferme !
C’est une découverte exceptionnelle : cet ambre est si vieux qu'il a été fabriqué avant que le moindre animal ne marche sur la Terre ferme !
Chine découverte
Ils cherchaient du charbon et ont découvert un trésor bien plus ancien : de minuscules fragments d’ambre vieux de 385 millions d’années. Cette trouvaille inattendue en Chine repousse de plusieurs dizaines de millions d’années l’apparition connue de la résine fossilisée et révèle que les plantes...
21/07/2026 futura-terre
L’ADN ancien révèle un secret effrayant dans la ville chinoise de Shimao, vieille de 4 000 ans
ADN Chine génétique
L’ADN ancien de la vaste colonie chinoise de Shimao, vieille de 4 000 ans, révèle comment a été organisée l’une des premières sociétés complexes d’Asie de l’Est. Les chercheurs ont découvert que ses habitants descendaient en grande partie des communautés agricoles locales du fleuve Jaune, mais qu'ils avaient également des liens génétiques avec des populations éloignées du sud et des steppes, ce qui indique des contacts préhistoriques étendus.
21/07/2026 sciencedaily-paleo ⚙ Traduction automatique
385-Million-Year-Old Amber Found in China
De l'ambre vieux de 385 millions d'années découvert en Chine
Chine Dévonien Dévonien Dévonien moyen géologie
Des paléontologues chinois ont découvert ce qu'ils disent être les premiers morceaux d'ambre confirmés jamais découverts, une résine fossilisée vieille d'environ 385 millions d'années (époque du Dévonien moyen) qui est antérieure d'environ 65 millions d'années au précédent détenteur du record. L'article Ambre vieux de 385 millions d'années découvert en Chine est apparu en premier sur Sci.News : Breaking Science News.
17/07/2026 sci-news ⚙ Traduction automatique
New Jurassic Fossil Reveals How Birds Lost Their Dinosaur Tails
Un nouveau fossile jurassique révèle comment les oiseaux ont perdu leur queue de dinosaure
Chine Jurassique fossile Dinosauria Zhengheornis oiseau
Des paléontologues chinois ont décrit un petit oiseau jurassique jusqu'alors inconnu dont la queue courte offre de nouvelles preuves de la façon dont les premiers oiseaux ont troqué leur longue queue semblable à celle d'un dinosaure contre le coccyx compact qui aide les oiseaux vivants à voler. L'article Un nouveau fossile du Jurassique révèle comment les oiseaux ont perdu leurs queues de dinosaures est apparu en premier sur Sci.News : Breaking Science News.
07/07/2026 sci-news ⚙ Traduction automatique
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