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Xiguayuan Formation
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Xiguayuan Fm base reconstruction

Xiguayuan Fm


Period: 
Cretaceous

Age Interval: 
Early Cretaceous, (25a) K1xgy


Province: 
Hebei

Type Locality and Naming

N. Hebei. The Xiguayuan Formation was erected by the 2nd Geological Survey Team of Hebei Province in 1975. The type section locates in 3 km to the Luanping County of northern Hebei.

Synonym: In its evolution, it used to refer to the “Jiufotang Fm” (Pang Qiqing, 1984), “Huajiying Fm” (Wang Si’en, 1990).

[Figure: Type section of Xiguayuan Formation between Liying and Xigayuan, Luanping County of Hebei Province]

[Figure: Measured section of Xiguayuan Formation]


Lithology and Thickness

The Huajiying Fm (= Xiguayuan Fm in this Lexicon) mainly comprises fluvio-lacustrine and lacustrine siltstones interbedded with numerous layers of tuffs and tuffaceous clastic rocks. Key specimens of the Early Jehol Biota were preserved in great fidelity in the lacustrine shales of the Huajiying Formation.


Lithology Pattern: 
Siltstone


Relationships and Distribution

Lower contact

Shown by D.P. Xi, X.Q. Wan et al. (2019; Cretaceous chapter of China Integrated Stratigraphy and Timescale) as underlying the Nandian Fm.

Upper contact

Shown by D.P. Xi, X.Q. Wan et al. (2019; Cretaceous chapter of China Integrated Stratigraphy and Timescale) as overlying the Dadianzi Fm.

Regional extent

The present lexicon correlates the Xiguayuan Formation with the Yixian Fm of western Liaoning. Both are roughly in one stratigraphic horizon.


GeoJSON

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Fossils

"Huajiying Fm (= Xiguayuan Fm), the lowest Jehol fossil-bearing deposits in northern China, … Huajiying Formation of the Sichakou Basin in northern Hebei Province, northern China contains key vertebrate taxa of the early Jehol Biota, e.g., Protopteryx fengningensis, Archaeornithura meemannae, Peipiaosteus fengningensis, and Eoconfuciusornis zhengi. This formation arguably documents the second-oldest bird-bearing horizon, producing the oldest fossil records of the two major Mesozoic avian groups Enantiornithes and Ornithuromorpha." (Saihong Yang et al., 2020, "The appearance and duration of the Jehol Biota: Constraint from SIMS U-Pb zircon dating for the Huajiying Formation in northern China", Proc. Nat. Acad. Sci. USA, 117: 14299-14305).


Age 

There is a U-Pb (SIMS) date of ca. 135 Ma (135.4 +/- 1.2 Ma) for the lowest Huajiying Fm (= Xiguayuan Fm). "Our findings, combined with previous radiometric dates, suggest that the oldest enantiornithine and ornithuromorph birds in the Jehol Biota are ca. 129−131 Ma, and that the Jehol Biota most likely first appeared at ca. 135 Ma.". [NOTE: This would imply a late Valanginian age for base, using GTS2020]

Age Span: 

    Beginning stage: 
Barremian

    Fraction up in beginning stage: 
0.2

    Beginning date (Ma): 
125.48

    Ending stage: 
Aptian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
117.30

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Wan Xiaoqiao