A new stiodermatid (Hexactinellida, Porifera) from the latest Ordovician of Anhui, South China and its significance for searching the missing link between the Cambrian and late Palaeozoic stiodermatid lineage

2022 ◽  
pp. 1-11
Author(s):  
Lixia Li ◽  
Joachim Reitner ◽  
Fangyi Gong ◽  
Guanzhou Yan ◽  
Rongchang Wu
2016 ◽  
Vol 34 (1) ◽  
pp. 45-61 ◽  
Author(s):  
C. Zhang ◽  
J. Yu ◽  
S. Y. O'Reilly ◽  
W. L. Griffin ◽  
J. Qian ◽  
...  

Zootaxa ◽  
2020 ◽  
Vol 4766 (1) ◽  
pp. 1-47 ◽  
Author(s):  
CHATCHALERM KETWETSURIYA ◽  
BARAN KARAPUNAR ◽  
THASINEE CHAROENTITIRAT ◽  
ALEXANDER NÜTZEL

A new Permian gastropod assemblage from the Roadian (Middle Permian) Khao Khad Formation, Saraburi Group (Lopburi Province, Central Thailand) which is part of the Indochina Terrane, has yielded one of the most diverse Permian gastropod faunas known from Thailand. A total of 44 gastropod species belonging to 30 genera are described herein, including thirteen new species and one new genus. The new genus is Altotomaria. The new species are Bellerophon erawanensis, Biarmeaspira mazaevi, Apachella thailandensis, Gosseletina microstriata, Worthenia humiligrada, Altotomaria reticulata, Yunnania inflata, Trachydomia suwanneeae, Trachyspira eleganta, Heterosubulites longusapertura, Platyzona gradata, Trypanocochlea lopburiensis and Streptacis? khaokhadensis. Most of the species in the studied assemblage represent vetigastropods  (35.6%) and caenogastropods (26.7%) and most of the species belong to Late Palaeozoic cosmopolitan genera. The studied faunas come from shallow water carbonates that are rich in fusulinids, followed by gastropods, ostracods, bivalves and brachiopods. The gastropod assemblage from the Khao Khad Formation shares no species with the gastropod assemblages from other Permian formations in Thailand, the Tak Fa Limestone and the Ratburi Limestone. However, it is similar to the Late Permian gastropod faunas from South China of the Palaeo-Tethys, therefore it suggests that the Indochina Terrane was not located far from South China. 


1990 ◽  
Vol 127 (5) ◽  
pp. 393-405 ◽  
Author(s):  
Luo Zhili ◽  
Jin Yizhong ◽  
Zhao Xikui

AbstractThe Yangtze Platform (Yangtze Palaeoplate) drifted into the area of southern China following late Silurian tectonism. In late Palaeozoic to early Mesozoic time the Yangtze Platform was subjected to strong extensional movements in its southeastern region within Yunnan, Guizhou, Guangxi and Hunan provinces, and along its northwestern margin in the Songpan-Ganzi area. Taphrogenesis (intracontinental extension) began in Devonian times, climaxed with the late Permian eruption of the Emeishan basalts, and ended in mid Triassic times. Therefore, the senior author (LZL) has named this extension the ‘Emei Taphrogenesis’, a phenomenon that was constrained by the neighbouring tectonic units of the Yangtze Platform. The platform has been substantially affected by the early Palaeozoic south China fold zone along its eastern margin, and by the late Palaeozoic opening of the Tethys Ocean on the northwestern margin. This paper delineates the tectonic patterns associated with the Emei Taphrogenesis.


Geology ◽  
1995 ◽  
Vol 23 (5) ◽  
pp. 407 ◽  
Author(s):  
Zheng-Xiang Li ◽  
Linghua Zhang ◽  
Christopher McA. Powell

2007 ◽  
Vol 31 (1-4) ◽  
pp. 107-138 ◽  
Author(s):  
Lianxing Gu ◽  
Khin Zaw ◽  
Wenxuan Hu ◽  
Kaijun Zhang ◽  
Pei Ni ◽  
...  

2008 ◽  
Vol 340 (2-3) ◽  
pp. 151-165 ◽  
Author(s):  
Liangshu Shu ◽  
Michel Faure ◽  
Bo Wang ◽  
Xinmin Zhou ◽  
Biao Song

PsycCRITIQUES ◽  
2010 ◽  
Vol 55 (28) ◽  
Author(s):  
David Elkind
Keyword(s):  

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