Kissinella-Christiania Associations in the early Ashgill Foliomena brachiopod fauna of South China

Lethaia ◽  
1994 ◽  
Vol 27 (1) ◽  
pp. 19-28 ◽  
Author(s):  
RONG JIA-YU ◽  
DAVID A.T. HARPER ◽  
ZHAN REN-BIN ◽  
LI RONG-YU
Keyword(s):  
2009 ◽  
Vol 33 (2) ◽  
pp. 163-183 ◽  
Author(s):  
Zhong-Qiang Chen ◽  
G. R. Shi ◽  
Yongqun Gao ◽  
Jinnan Tong ◽  
Fengqing Yang ◽  
...  

Lethaia ◽  
2006 ◽  
Vol 39 (1) ◽  
pp. 79-90 ◽  
Author(s):  
Z. Q. CHEN ◽  
G. R. SHI ◽  
FENG-QING YANG ◽  
YONG-QUAN GAO ◽  
JINNAN TONG ◽  
...  

2015 ◽  
Vol 39 (3) ◽  
pp. 295-314 ◽  
Author(s):  
Yang Zhang ◽  
Wei-Hong He ◽  
G.R. Shi ◽  
Ke-Xin Zhang ◽  
Hui-Ting Wu

2016 ◽  
Vol 53 (7) ◽  
pp. 674-679 ◽  
Author(s):  
Bing Huang ◽  
Ren-Bin Zhan ◽  
Guang-Xu Wang

A recovery brachiopod fauna occurs in the lower Niuchang Formation (upper Rhuddanian – lower Aeronian, Llandovery) of the Xinglongchang section, Meitan County, northern Guizhou Province, South China. Nine collections were made at the section, all of which are dominated by brachiopods, and three associations are recognized here and their paleoecology is discussed. Paleoenvironmental analysis shows a shallowing upward trend for the lower Niuchang Formation, although a global transgression was happening at that time. The balance between the global transgression and the regional Qianzhong Uplift guaranteed a stable environment for the formation of the Niuchang Formation and the recovery of brachiopods in South China after the end-Ordovician mass extinction. In addition to the traditional methods of principal component analysis and cluster analysis, a relatively new technique to paleontology, “network analysis”, is applied successfully in this study. It is suggested that network analysis could be used as one of the supporting methods in investigating brachiopod paleoecology.


2019 ◽  
Vol 94 (2) ◽  
pp. 239-254 ◽  
Author(s):  
Bing Huang ◽  
Jiayu Rong ◽  
David A.T. Harper ◽  
Hanghang Zhou

AbstractThe brachiopods collected from the Kuanyinchiao Beds (Hirnantian, uppermost Ordovician) in Meitan and Zunyi counties, northern Guizhou, include 13 species and one undetermined taxon, dominated by Hirnantia sagittifera (M'Coy, 1851) (which accounts for over one-third of the specimens), together with common Eostropheodonta hirnantensis (M'Coy, 1851). They are assigned to the Hirnantia–Eostropheodonta Community, which probably inhabited a shallow-water, nearshore Benthic Assemblage (BA) 2 to upper BA 3 environment. Population analysis shows that the community was well adapted to this environment after the first phase of the end-Ordovician mass extinction. Representative specimens of all the species are illustrated, and a new species, Minutomena missa, is described herein. The variation in Hirnantia sagittifera was noted in many of previous studies but was not statistically evidenced. Here we have measured representative specimens of that famous species from the major paleoplates and terranes in the world, along with other species assigned to the genus from South China. Having used principal component analysis (PCA), significant variations in the species are documented statistically and revised, and three nominal species, one subspecies, and two morphotypes are now reassigned to Hirnantia sagittifera sensu stricto.UUID: http://zoobank.org/references/3f83fb1e-a6dd-4585-9f9f-9586dad28244


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