The paleoenvironmental evolution of the Cambrian Longwangmiao Formation (Stage 4, Toyonian) on the Yangtze Platform, South China: Petrographic and geochemical constrains

2019 ◽  
Vol 100 ◽  
pp. 391-411 ◽  
Author(s):  
Ying Ren ◽  
Dakang Zhong ◽  
Chonglong Gao ◽  
Bing Li ◽  
Xuan Cao ◽  
...  
2017 ◽  
Vol 92 (1) ◽  
pp. 49-58 ◽  
Author(s):  
Yuning Yang ◽  
Xingliang Zhang ◽  
Yuanlong Zhao ◽  
Yiru Qi ◽  
Linhao Cui

AbstractThe Cambrian Yanwangbian assemblage (Series 2, Stage 4) in South Shaanxi, China, is one of the Burgess Shale–type faunas as it represents the only relatively diverse Cambrian biota from the north margin of the Yangzte Platform, South China. The paleoscolecids (Cycloneuralia) illustrated herein are one of the major components of the fauna, although they appear to be much less abundant than skeletonized fossils, according to available collections. A new taxon, Shaanxiscolex xixiangensis new genus new species, is described based on the scleritome pattern: each annulus has two rows of alternating Hadimopanella-type plates positioned close to the borders, and a mosaic pattern of microplates occurs between the plates and within intersegmental furrows. The occurrence of the new taxon confirms a fairly diversified and widespread distribution of paleoscolecidan worms recognized in the early Cambrian of South China. Moreover, the ecology of paleoscolecids is reappraised based on burial position of the S. xixiangensis and gut contens of Cambrian taxa from South China, hinting that paleoscolecids (at least some taxa) were both deposit feeders and carnivores, as well as active bioturbators in the substrates of the Cambrian sea, which sheds new light on the ‘Cambrian Substrate Revolution.’


2017 ◽  
Author(s):  
Caroline Kelleher ◽  
◽  
Sarah Thorne ◽  
Marcello Minzoni ◽  
Meiyi Yu ◽  
...  

2016 ◽  
Vol 53 (7) ◽  
pp. 651-659
Author(s):  
Zhongyang Chen ◽  
Chengyuan Wang ◽  
Ru Fan

Previous studies of conodonts suggested that the upper member of the Xiushan Formation (late Llandovery) corresponds to the Pterospathodus eopennatus Superbiozone, but no data were obtained from the lower member in the Xiushan area. In this study, the entire Xiushan Formation was resampled from the Datianba section in the Xiushan area of Chongqing City on the Yangtze Platform in South China. In total, 40 samples were collected and processed. Fifteen of these samples contained identifiable conodont specimens. The present study indicates that the lower member and main part of the upper member of the Xiushan Formation correspond to the Pterospathodus eopennatus Superbiozone, while the top of the upper member probably correlates with the Pterospathodus celloni Superbiozone.


2007 ◽  
Vol 261 (1-2) ◽  
pp. 303-320 ◽  
Author(s):  
Ganqing Jiang ◽  
Alan J. Kaufman ◽  
Nicholas Christie-Blick ◽  
Shihong Zhang ◽  
Huaichun Wu

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