Sinosauropteryx (meaning "Chinese reptilian wing") is an extinct genus of coelurosaurian theropod dinosaurs. Described in 1996, it was the first dinosaur taxon outside of Avialae (birds and their immediate relatives) to be found with evidence of feathers. It was covered with a coat of very simple filament-like feathers. Structures that indicate the colour pattern have also been preserved in some of its feathers, which show that Sinosauropteryx had a countershading pattern in its body with a banded tail. The reddish brown colouration previously inferred for Sinosauropteryx is based on the melanosomes preserved in the specimen of a separate genus, Huadanosaurus. Some contention has arisen with an alternative interpretation of the filamentous impression as remains of collagen fibres, but this has not been widely accepted. Sinosauropteryx was a small theropod with an unusually long tail and short arms. The longest known specimen reaches up to 1.07 metres (3.51 feet) in length, with an estimated weight of 0.55 kilograms (1.21 pounds). It was considered a close relative of the similar but older genus Compsognathus, with both genera belonging to the family Compsognathidae, though subsequent analyses did not recover this family to be monophyletic and placed Sinosauropteryx within its own family, Sinosauropterygidae. Two species of Sinosauropteryx have been named. The first, S. prima, is known from three specimens, named "first" in reference to its status as the first feathered non-avian dinosaur species discovered. The third specimen previously assigned to Sinosauropteryx most likely represents a tyrannosauroid unrelated to this genus. The second, S. lingyuanensis, is known from a single specimen, named after its type locality. Sinosauropteryx lived in what is now northeastern China during the early Cretaceous period. It was among the first dinosaurs discovered from the Yixian Formation in Liaoning Province, and was a member of the Jehol Biota. Well-preserved fossils of this genus illustrate many aspects of its biology, such as its diet and reproduction.
History of discovery
The first fossil specimen of the dinosaur later named Sinosauropteryx prima was uncovered in August 1996 by Li Yumin. Yumin was a farmer and part-time fossil hunter who often prospected around Liaoning Province to acquire fossils to sell to individuals and museums. Yumin recognized the unique quality of the specimen, which was separated into two slabs, and sold the slabs to two separate museums in China: the National Geological Museum in Beijing, and the Nanjing Institute of Geology and Paleontology. The director of the Beijing museum, Ji Qiang, recognized the importance of the find, as did visiting Canadian palaeontologist Phil Currie and artist Michael Skrepnick, who became aware of the fossil by chance as they explored the Beijing museum's collections after leading a fossil tour of the area during the first week of October, 1996. Currie recognized the significance of the fossil immediately. As The New York Times quoted him, "When I saw this slab of siltstone mixed with volcanic ash in which the creature is embedded, I was bowled over." When originally described, the authors named Sinosauropteryx, meaning "Chinese Reptilian Wing". Chinese authorities initially barred photographs of the specimen from publication. However, Currie brought a photograph to the 1996 meeting of the Society of Vertebrate Paleontology at the American Museum of Natural History in New York, causing crowds of palaeontologists to gather and discuss the new discovery. The news reportedly left palaeontologist John Ostrom, who in the 1970s had pioneered the theory that birds evolved from dinosaurs, "in a state of shock." Ostrom later joined an international team of researchers who gathered in Beijing to examine the fossils; other team members included feather expert Alan Brush, fossil bird expert Larry Martin, and Peter Wellnhofer, an expert on the early bird Archaeopteryx. Three specimens have been assigned to Sinosauropteryx prima: the holotype GMV 2123 (and its counter slab [opposite face], NIGP 127586), NIGP 127587, and D 2141. Another specimen, IVPP V14202, was originally assigned to the genus in 2010, but was later designated as the holotype of a separate genus Huadanosaurus. The assignment of an additional larger specimen to S. prima, GMV 2124 (also known as NGMC 2124), was later found to be in error, and most likely belongs to Tyrannosauroidea. All of the fossils were found in the Jianshangou or Dawangzhangzi Beds of the Yixian Formation in the Beipiao and Lingyuan regions of Liaoning, China. These fossil beds have been dated to 124.6–122 million years ago, during the early Aptian stage of the Early Cretaceous.
In 2025, Rui Qiu and colleagues named and described a second species of Sinosauropteryx: S. lingyuanensis. The assigned holotype is IVPP V 12415, which comprises a near complete skeleton of a potential juvenile which also preserves traces of feather integument. The specimen was collected around 2010 from the Lower Cretaceous Yixian Formation of Dawangzhangzi (Lingyuan, Western Liaoning, China), and though it is of juvenile nature it represents the largest reported Sinosauropteryx individual. The species name, lingyuanensis, refers to Lingyuan which is the city where the holotype specimen was discovered.
Identity of filaments Controversy regarding the identity of the filaments preserved in the first Sinosauropteryx specimen began almost immediately, as the team of scientists spent three days in Beijing examining the specimen under a microscope. The results of their studies (reported during a press conference at the Philadelphia Academy of Natural Sciences on Thursday, April 24, 1997) were inconclusive; the team agreed that the structures preserved on Sinosauropteryx were not modern feathers, but suggested further research was required to discover their exact nature. Palaeontologist Alan Feduccia, who had not yet examined the specimen, wrote in Audubon Magazine that the structures of Sinosauropteryx (which he considered at the time to be a synonym of Compsognathus, as Compsognathus prima) were stiffening structures from a frill running along the back, and that dinosaur palaeontologists were engaging in wishful thinking when equating the structures with feathers. Subsequent publications saw some of the team members disagreeing over the identity of the structures.
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