scholarly journals Latest Wuchiapingian to Earliest Triassic Conodont Zones and δ13Ccarb Isotope Excursions from Deep-Water Sections in Western Hubei Province, South China

2019 ◽  
Vol 30 (5) ◽  
pp. 1059-1074 ◽  
Author(s):  
Bo Yang ◽  
Hanxiao Li ◽  
Paul B. Wignall ◽  
Haishui Jiang ◽  
Zhijun Niu ◽  
...  
Keyword(s):  
South China ◽  
Deep Water ◽  
Hubei Province ◽  
Western Hubei

Radiolarian fauna from the Chiungchussuan Shuijingtuo Formation (Cambrian Series 2) in Western Hubei Province, South China

2019 ◽  
Vol 62 (10) ◽  
pp. 1645-1658 ◽  
Author(s):  
Qiangfen Ma ◽  
Qinglai Feng ◽  
Wenchao Cao ◽  
Lei Zhang ◽  
Yan Ye ◽  
...  
Keyword(s):  
South China ◽  
Hubei Province ◽  
Western Hubei ◽  
Radiolarian Fauna

Depositional environment and organic matter enrichment of the lower Cambrian Niutitang shale in western Hubei Province, South China

2019 ◽  
Vol 109 ◽  
pp. 381-393 ◽  
Author(s):  
Yiquan Ma ◽  
Yongchao Lu ◽  
Xiaofeng Liu ◽  
Gangyi Zhai ◽  
Yufang Wang ◽  
...  
Keyword(s):  
Organic Matter ◽  
South China ◽  
Lower Cambrian ◽  
Depositional Environment ◽  
Hubei Province ◽  
Western Hubei

Latest Permian deep-water foraminifers from Daxiakou, Hubei, South China

2015 ◽  
Vol 89 (3) ◽  
pp. 448-464 ◽  
Author(s):  
Muhui Zhang ◽  
Songzhu Gu
Keyword(s):  
New Species ◽  
South China ◽  
Deep Water ◽  
Water Environment ◽  
Hubei Province ◽  
Abundance And Diversity

AbstractA latest Changhsingian (latest Permian) foraminiferal fauna composed of 19 species (belonging to 10 genera) was recovered from the Daxiakou section in Xingshan County, Hubei Province, South China. Compared to contemporaneous faunas in South China, the Daxiakou fauna displays unique features: (1) nodosariids are the dominant forms in abundance and diversity; and (2) the most abundant forms have elongate and flattened tests, and include Geinitzina, Howchinella, and Ichthyolaria. The predominance of flattened elongate tests and their smaller size suggest that these foraminifers possibly lived in an oxygen-depleted, deep-water environment. Seven new species, Nodosaria quinquecostata n. sp., Howchinella inflata n. sp., H. hubeiensis n. sp., H. complanata n. sp., H. xiangxiensis n. sp., Ichthyolaria celsa n. sp., and Pseudotristix elongata n. sp. are described.

scholarly journals An integrated chemostratigraphic (δ13C-δ18O-87Sr/86Sr-δ15N) study of the Doushantuo Formation in western Hubei Province, South China

2019 ◽  
Vol 320 ◽  
pp. 232-252 ◽  
Author(s):  
Zhongwu Lan ◽  
Yuji Sano ◽  
Takuya Yahagi ◽  
Kentaro Tanaka ◽  
Kotaro Shirai ◽  
...  
Keyword(s):  
South China ◽  
Hubei Province ◽  
Doushantuo Formation ◽  
Western Hubei

Late Permian (Changhsingian) conodont biozonation and the basal boundary, Ganxi section, western Hubei Province, south China

2006 ◽  
Vol 43 (2) ◽  
pp. 121-133 ◽  
Author(s):  
Mutwakil Nafi ◽  
Xia Wenchen ◽  
Zhang Ning
Keyword(s):  
South China ◽  
Hubei Province ◽  
Late Permian ◽  
Evolutionary Lineage ◽  
First Occurrence ◽  
Western Hubei

Four neogondolellid conodont interval zones were recognized across the Changhsingian stage at Ganxi section, western Hubei Province, south China. They are in ascending order: the Clarkina wangi Zone, the Clarkina changxingensis changxingensis Zone, the Clarkina changxingensis yini Zone, and the Clarkina meishanensis meishanensis Zone. The present study suggests that the base of the Changhsingian can be defined by the first appearance datum (FAD) of Clarkina wangi within an evolutionary lineage from Clarkina longicuspidata to Clarkina wangi. The Wuchiapingian–Changhsingian boundary can be placed at the base of bed 104 at Ganxi section, south China because of the first occurrence of Clarkina wangi.

The origin of bedding-parallel fibrous calcite veins in the Lower Permian Chihsia Formation in western Hubei Province, South China

2015 ◽  
Vol 60 (20) ◽  
pp. 1778-1786
Author(s):  
Hao Yu ◽  
XiQiang Zhou ◽  
JianGuo Wang ◽  
Chuan Guo ◽  
HengYe Wei ◽  
...  
Keyword(s):  
South China ◽  
Hubei Province ◽  
Lower Permian ◽  
Calcite Veins ◽  
Western Hubei
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