Suining Formation

Geologic formation in China From Wikipedia, the free encyclopedia

The Suining Formation (simplified Chinese: 遂宁组; traditional Chinese: 遂寧組; pinyin: Suìníng Zǔ) is a geological formation in China whose strata likely date back to the Late Jurassic.[3] Dinosaur remains are among the fossils that have been recovered from the formation.[4]

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Suining Formation
Stratigraphic range: ?Late Jurassic, ~145? Ma[1]
TypeGeological formation
Unit ofSichuan Basin
UnderliesPenglaizhen Formation
OverliesUpper Shaximiao Formation
ThicknessSeveral hundred meters
Lithology
PrimaryMudstone
OtherSandstone, siltstone
Location
RegionAsia
CountryChina
Type section
Named byLee & Chen (1939)[2]
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History

The Suining Formation was identified in 1939. The formation was initially dated to the Tithonian (Late Jurassic).[2][4][5] A 2019 publication described zircons from the Suining Formation that implied a younger age, the average age being around 115.5–113.3 million years ago (Early Cretaceous, upper Aptian age).[6] Later research suggested that a Late Jurassic age is more likely based on reinterpretations of the previous zircon-based ages and comparisons of the dinosaur and pollen fossils with other more confidently-dated formations.[3][1]

Paleobiota

Dinosaurs

Sauropods

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Genus Species Presence Materials Notes Images

Mamenchisaurus[7]

M. anyuensis[7]

Geographically located in Sichuan, China.[7]

A mamenchisaurid

Qijianglong[8]

Q. guokr

A partial skeleton including cranial bones, most of the neck and tail, and other associated elements. A mamenchisaurid
Tongnanlong[3] T. zhimingi Tongnan District in the Sichuan Basin A holotype specimen, TNM 0254, consists of three dorsal and six caudal vertebrae, left shoulder girdle (scapula and coracoid), and hindlimb elements (partial tibia, fibula, three metatarsals, and two unguals). One of the largest known mamenchisaurids
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Fish

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Beiduyu[9]

B. qijiangensis

Ceratodus[3] C. szechuanensis
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Turtles

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Plesiochelys[3] P. tatsuensis
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See also

References

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