Zhiluo Formation

Geological formation in China From Wikipedia, the free encyclopedia

The Zhiluo Formation is a geological formation in China, it is also alternatively considered a geological group under the name Zhiluo Group (formerly known as the Chiloo Group). It dates to the Middle Jurassic. It consists of sandstone, mudstone and siltstone of varying colours. It has received scientific attention for its uranium ore bodies present in the lower part of the formation.[1] Fossil theropod tracks have been reported from the formation.[2] These were described from two footprints found in Jiaoping Coal Mine by C. C. Young in 1966 as Shensipus tungchuanensis. These were in 2015 suggested to belong to Anomoepus.[3] The dicraeosaurid sauropod dinosaur Lingwulong is known from the formation, previously having been erroneously attributed to the underlying Yanan Formation.[4]

Sub-unitsLower, Upper units
UnderliesLower Cretaceous Dongsheng Formation
Quick facts Type, Sub-units ...
Zhiluo Formation
Stratigraphic range: Middle to Late Jurassic, Bathonian–Oxfordian
TypeGeological formation
Sub-unitsLower, Upper units
UnderliesLower Cretaceous Dongsheng Formation
OverliesYanan Formation
Thickness100-200 metres
Lithology
PrimarySandstone, siltstone mudstone
Location
RegionShaanxi
CountryChina
ExtentOrdos Basin
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Fossil content

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Dinosaurs

Sauropods

More information Sauropods of the Zhiluo Formation, Genus ...
Sauropods of the Zhiluo Formation
Genus Species Location Stratigraphic position Material Notes Images
Lingwulong[5] L. shenqi A dicraeosaurid sauropod
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Insects

More information Insects of the Zhiluo Formation, Genus ...
Insects of the Zhiluo Formation
Genus Species Location Stratigraphic position Material Notes Images
Orthophlebia O. quadrimacula A orthophlebiid scorpionfly
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See also

Footnotes

References

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