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Gaozhuang Formation

Gaozhuang Fm


Period: 
Neogene

Age Interval: 
Early Pliocene (Zanclean), N2 , (17b)


Province: 
Shanxi

Type Locality and Naming

The type section is located at exposures (E112°53′, N37°01′) between the villages of Gaozhuang and Zhaozhuang, about 10 km southwest of the county of Yushe, Shanxi Province. It was named by Qiu et al. (1987).


Lithology and Thickness

The Gaozhuang Fm is divided into three members: lower Taoyang Mbr is characterized by a thick series of golden-brown and rusty yellow fine large interlaced medium-grained sandstones interbedded with purplish-red laminations of clay. middle Nanzhuanggou Mbr consists of rusty yellow and purplish-red clays with three layers of greyish-green marlstones. upper Culiugou Mbr is formed by purple and brownish-red coarse-grained sandstones with gravels. It contains abundant fossil fishes, turtles, mammals, insects, gastropods, ostracods, charophytes, plants, and sporopollens. Its thickness is about 450 m.


Lithology Pattern: 
Clayey sandstone


Relationships and Distribution

Lower contact

In the type section, the Gaozhuang Fm unconformably contacts with the underlying Upper Miocene Mahui Fm.

Upper contact

In the type section, the Gaozhuang Fm unconformably is overlain by the Upper Pliocene Mazegou Fm.

Regional extent

The formation is restricted in the Yuncu Sub-basin of the Yushe Basin.


GeoJSON

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Fossils

Mammals: Blarinini indet., Soriculus praecursus, Desmana kowalskae, Yanshuella primaeva, Scaptochirus sp., Eutamias ertemtensis, Sciurus sp., S. yusheensis, Sinotamias sp., Pliopetaurista rugosa, Castor anderssoni, Dipoides majori, Myomimus sp., Cricetinus sp., Allocricetus sp., Neocricetodon grangeri, Nanocricetus mongolicus, Chardina truncatus, Prosiphneus eriksoni, Mesosiphneus praetingi, Mimomys sp., Germanomys sp., Rhizomys shansius, Dipus fraudator, Apodemus qiui, Micromys chalceus, M. tedfordi, Karnimata hipparionum, Chardinomys yusheensis, Huaxiamys downsi, Hystrix sp., Alilepus annectens, Trischizolagus sp., Hypolagus sp., Ochotona lagrelli, Nyctereutes tingi, N. sinensis, Eucyon davisi, E. zhoui, Canis sp., Agriotherium sp., Ursus sp., Plesiogulo brachygnathus, Martes sp., Thalassictis sp., Chasmaporthetes kani, Pachycrocuta pyrenaica, Metailurus sp., Mammut borsoni, Sinomastodon intermedius, Stegodon zdanskyi, Hipparion platyodus, H. houfenense, H. pater, H. insperatum, H. licenti, Dicerorhinus ringstroemi, Shansirhinus ringstroemi, Sus erymanthius, Paracamelus sp., Moschus sp., Paracervulus cf. P. killgusi, Metacervulus sp., Muntiacus cf. M. lacustris, Axis speciosus, Cervavitus demissus, Eucladoceros proboulei, Procapreolus sp., Gazella gaozhuangensis, G. nihensis, G. yushensis, cf. Protoryx yushensis, cf. Tragocerus laticornis (Tedford et al., 1991; Qiu and Qiu, 1995; Flynn et al., 1997). Fishes: Xenocypris yushensis, Cyprinus carpio, Carassius auratus, Culter cf. C. mongolicus, Hemiculterella longicephalus, Leuciscus tchangi, Hypophthalmichthys molitrix, Pseudorasbora changtsunense, Mylopharyngodon piceus, Ctenophary ngodonidellus, Parasilurus asotus, Sinoperca wusiangensis, Ophicephalus argus (Liu and Su, 1962). Amphibian: Rana yushensis (Liu, 1961). Ostracods: Ilyocypris cornae, I. manasensis, I. gibba, I. biplicata, I. salebrosa, I. dunschanensis, I. qingxuensis, I. pulchra, I. errabundis, I. bradyi, Cypris subglobosa, Eucypris inflata, Eucypris cf. E. concinna, Cyprinotus salinus, C. yusheensis, C. chiuhsinensis, C. formalis, C. reticulata, Potamocypris sp., Cypridopsis sp., Candona yaozitouensis, C. kirgizica, Candoniella albicans, C. suzini, C. mirabilis, Leucocythere mirabilis, Cyprideis littoralis (Huang et al., 1991) Gastropods: Cincinnatia alticonula, Stothyra glabra, Neumayria sp., Bithynia phrygica, Hydrobioides yusheensis, Parafossarulus? sp., Galba turritella, Radix pereger, Acella sp., Bulinus sp., Gyraulus albus, G. compressus, G. sibiricus, G. Borealis, Polypylis succinea, Planorbarius corneus, Nesopupa wesleyana, Vertigo lilljeborgi, Gastrocopta armigerella, G. paucidentata, Pupilla bituberculata, Vallonia tenuilabris, V. asiaticae, Succinea oblonga, S. altaica (Wang, 1992). Bivalves: Sphaerium rivicolum, S. subsolidum, Pisidium amnicum (Huang et al., 1991). Sporopollens: Pinus, Picea, Abies, Larix, Tsuga, Betula, Quercus, Corylus, Tilia, Castanea, Carpinus, Ulmus, Ephedra, Artemisia, Chenopodiaceae, Compositae, Labiatae, Poaceae, Leguminosae, Polygonaceae, Cyperaceae, Typha, Potamogeton, Sinopteridaceae. (Li et al., 2002) Charophytes: Grambastichara weinanensis, Lychnothamnus subeiensis, Chara cf. C. sejuncta, Nemegtichara sp. (Huang et al., 1991). Plants: Hemiptelea sp., Quercus miovariablis, Quercus cf. Q. dentate, Quercus cf. Q. liaotungensi, Quercus cf. Q. mongolica, Carpinus cf. C. miofangiana, C. subcordata, Acer florinii, A. subpictum, A. diabolicum, Zelkova ungeri, Ulmus cf. U. parvifolia, Juglans sp., Pterocarya sp., Cudrania sp., Broussonetia sp., Populus latior, Salix cf. S. wallichiana, Albizza sp., Spiraea sp., Evodia sp., Koelreuteria cf. K. integrifolia, Tyhpa sp. (Cao and Cui, 1990).


Age 

Teilhard and Young (1933) assigned this formation to the Sanmen Stage. Licent and Trassaert (1935) placed it at their “Yushe Zone III”. Pei et al. (1963) renamed as “Upper Yushe Fm”. Bureau of Geology and Mineral Resources of Shanxi Province (BGMRS(Shanxi)P) (1989) named the Zhangcun Fm. Qiu et al. (1987) considered that the Gaozhuang Fm can be correlated to the upper part of the Zhangcun Fm. The recent magnetic dating of the Gaozhuang Fm is in range of 4.2~5.8 Ma (Opdyke et al., 2013). The Gaozhuang Fm and Fauna are the fundamentals of the Gaozhuangian Stage of the continental Pliocene series in China (Deng et al., 2010). Tao Deng et al. (2019; Neogene integrated stratigraphy and timescale of China) show it as spanning the Zanclean.

Age Span: 

    Beginning stage: 
Zanclean

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
5.34

    Ending stage: 
Zanclean

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
3.60

Depositional setting

It is interpreted as a river-lake environment.


Depositional pattern:  

Additional Information


Compiler:  

Tao Deng, Sukuan Hou, J.Z. Qigao, Q. Li, Q.Q. Shi, B.Y. Sun, S.Q. Wang, F.X. Wu