Showing posts with label Coelurosaurs. Show all posts
Showing posts with label Coelurosaurs. Show all posts

Sunday, 9 June 2019

Phuwiangvenator yaemniyomi & Vayuraptor nongbualamphuensis: Two new species of Coelurosaur from the Early Cretaceous of Thailand.

The Coelurosaurs were a diverse group of Therapod Dinosaurs, including the Tyrannosaurs, Compsognathids, Ornithomimids and Maniraptors (the group that includes the modern Birds). They are thought to have appeared and diversified in the Mid-to-Late Jurassic, though fossils from this early are rare, and usually fragmentary, often comprising only isolated teeth. The Megaraptors are a poorly understood group of Theropod Dinosaurs, currently thought to be basal members of the Coelurosauria (i.e. they are an early group that diverged from the main Coelurosaur lineange before the appearance of Tyrannosaurs and Maniraptors. They appear to have been medium sized Theropods with long claws, broad bodies and highly pneumatised skeletons, though they are known only from incomplete skeletons, making their true nature and affinities hard to judge.

In a paper published in the journal Acta Palaeontologica Polonica on 27 May 2019, Adun Samathi of the Division of Paleontology at the Rheinische Friedrich-Wilhelms Universität Bonn, Phornphen Chanthasit of the Sirindhorn Museum, and Martin Sander, also of the Division of Paleontology at the Rheinische Friedrich-Wilhelms Universität Bonn, describe two new species of Coelurosaurs from the Early Cretaceous Sao Khua Formation of northeastern Thailand, one of which is considered to be a Megaraptor, and one of which could possibly be.

The first Dinosaur bones discovered in Thailand cane from the red clays of the Sao Khua Formation on Phu Wiang Mountain in the 1970s and 80s, since when the site has been extensively worked, producing a range of fossils including Ornithischians, Sauropods, and Theropods, as well as freshwater Hybodont Sharks, Actinopterygian Fish, Turtles, and Crocodilians. These deposits were originally thought to be Jurassic in age, but are now considered to be Early Cretaceous.

The first new species described is named Phuwiangvenator yaemniyomi, where 'Phuwiangvenator' derives from Phu Wiang Mountain in Khon Kaen Province, Thailand, where the specimen was found, plus '-venator' Latin for 'hunter', making 'hunter of Phu Wiang', and 'yaemniyomi' honours Sudham Yaemniyom, the geologist who found the first ever Dinosaur bone on Phu Wiang Mountain in 1976. The specimen comprises a disarticulated partial skeleton consisting of a dorsal vertebra, three fused sacral vertebrae, the right second metacarpal, plus the right phalanges and unguals, both tibias, the left left astragalocalcaneum, the left first metatarsal, the right second to fourth metatarsals, and the right pedal phalanges and unguals. This specimen is reconstructed as a Megaraptor about 6 m in length.

Coelurosaurian Theropod Phuwiangvenator yaemniyomi from the Early Cretaceous Sao Khua Formation of Phu Wiang, Khon Kaen Province, Thailand. (A) Right tibia in anterior (A₁), lateral (A₂), posterior (A₃), medial (A₄), proximal (A₅), and distal (A₆) views. (B) Proximal left tibia in lateral view. Arrow indicates vertical ridge on the tibia. Samathi et al. (2019).

The second new species is named Vayuraptor nongbualamphuensis, where 'Vayuraptor' derives from 'Voyu' Sanskrit for the God of Wind and '-raptor', to give 'wind-raptor', in reference to the long, slim tibia of the specimen, which suggests a fast running animal. The species is described from the tibia mentioned, plus some coracoids, a fragment of fibula, a rib, a probable fragment of the pubis, a manual phalanx, and a probable pedal phalanx. It is interpreted as a small Theropod 4-4.5 m in length, with body proportions similar to those of the Magaraptor Fukuiraptor kitadaniensis.

Coelurosaurian Theropod Vayuraptor nongbualamphuensis from the Early Cretaceous Sao Khua Formation of Phu Wat, Nong Bua Lamphu Province, Thailand. Left tibia with associated astragalocalcaneum in anterior (A₁), lateral (A₂), posterior (A₃), medial (A₄), proximal (A₅), and distal (A₆) view. Arrow indicates vertical ridge on the tibia. Samathi et al. (2019).

See also...

https://sciencythoughts.blogspot.com/2019/04/moros-intrepidus-small-tyrannosauroid.htmlhttps://sciencythoughts.blogspot.com/2019/04/small-theropod-tracks-preserved-in.html
https://sciencythoughts.blogspot.com/2019/04/evidence-of-large-tyranosauroid.htmlhttps://sciencythoughts.blogspot.com/2019/04/the-partial-ilium-of-abelisaurid.html
https://sciencythoughts.blogspot.com/2018/12/anomalipes-zhaoi-new-species-of.htmlhttps://sciencythoughts.blogspot.com/2018/11/archaeopteryx-albersdoerferi-phantom.html
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Monday, 1 July 2013

A juvenile Coelurosaur from the Middle Jurassic of Xinjiang Province, China.

The Coelurosaurs were a diverse group of Therapod Dinosaurs, including the Tyrannosaurs, Compsognathids, Ornithomimids and Maniraptors (the group that includes the modern Birds). They are thought to have appeared and diversified in the Mid-to-Late Jurassic, though fossils from this early are rare, and usually fragmentary, often comprising only isolated teeth.

In a paper published in the Journal of Systematic Palaeontology on 3 May 2013, a team of scientists led by Jonah Choiniere of the Division of Paleontology and Richard Gilder Graduate School at the American Museum of Natural History and the Department of Biological Sciences at George Washington University, describe juvenile Coelurosaur, at most a year old, from the latest Middle Jurassic (i.e. about 161.5 million years old) of northern Xinjiang Province, China.

The new specimen is named Aorun zhaoi, after Ao Run, the Dragon King of the West in the Chinese epic Journey to the West, which featured the pilgrimage of the Buddhist monk Xuanzang (sometimes known as Tripitaka) and his companions, and Zhao Xi-jin, a distinguished Chinese palaeontologist. Aorun zhaoi is described from a partial skeleton comprising most of a skull, several vertebrae, the left ulna (one of the bones in the forearm) and manus (hand),and part of the hip and legs.

The skull of Aorun zhaoi. (A) Right lateral view; (B) line drawing of right lateral view; (C) left lateral view; (D) line drawing of left lateral view. Abbreviations: a, articular; aof, antorbital fenestra; aofo, antorbital fossa; dg, dentary groove; emf, external mandibular fenestra; en, external naris; hy, hyoid; itf, infratemporal fenestra; jg, jugal; lac, lacrimal; lang, left angular; ld, left dentary; lfp, left frontal and parietal; lmr, lateral maxillary ridge; lpa, left prearticular; lpal, left palatine; lsa, left surangular; lspl, left splenial; max, maxilla; mf, maxillary fenestra; mhf, mylohyoid foramen; na, nasal; o, orbit; pf, prefrontal; pmx, premaxilla; po, postorbital; prq, pterygoid ramus of the quadrate; q, quadrate; qj, quadratojugal; qjc, quadratojugal contact; rang, right angular; rd, right dentary; rls, right laterosphenoid; rpal, right palatine; rpt, right pterygoid; rq, right quadrate; rsa, right surangular; saf, surangular foramen; scl, sclerotic ring; sq, squamosal; v, vomer. Scale bar is 1 cm. Choiniere et al. (2013).

Overview of partially prepared block containing Aorun zhaoi. The skull was removed prior to this photograph and its approximate position is indicated by the dashed black line with white fill. The dashed line with arrows indicates the approximate position of the histological section taken for analysis. (A) Photograph of block; (B) line drawing. Abbreviations: sk, skull; rfib, right fibula; lcarp, left carpus; lmc, leftmetacarpus; ltib, left tibia; rpes, right pes; rtib, right tibia; lman, left manus; pub, pubis; rmt, right metatarsus; lpes, left pes; lmt, left metatarsus; ldt, left distal tarsals. Scale bar equals 2 cm. Choiniere et al. (2013).


Describing species from juvenile specimens is problematic, and it is usually considered preferable to use mature specimens to avoid giving different names to different growth stages of the same animal. On this occasion Choiniere et al. have concluded that the available material is distinctive enough to exclude the possibility of it being the juvenile of a previously described species of Coelurosaur, of which there are a limited supply in this time period. 

The attempt was also made to assign systematic position to Aorun zhaoi. A cladistic analysis suggests a position after the Tyrannosaurs but before the divergence of the other groups, but Choiniere et al. caution this may be a product of the young age of the specimen, and that features that would lead to it being placed within a more developed group might have developed later in its development.

Strict consensus tree showing phylogenetic position of Aorun zhaoi. Choiniere et al. (2013).

Map showing the location where Aorun zhoi was found. Choiniere et al. (2013).


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