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Permian fusuline fauna from the lower part of the lugu formation in the central qiangtang block and its geological implications

Zhang,Y, Shi,G, Shen,S and Yuan,D 2014, Permian fusuline fauna from the lower part of the lugu formation in the central qiangtang block and its geological implications, Acta Geologica Sinica, vol. 88, no. 2, pp. 365-379, doi: 10.1111/1755-6724.12202.

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Title Permian fusuline fauna from the lower part of the lugu formation in the central qiangtang block and its geological implications
Author(s) Zhang,Y
Shi,GORCID iD for Shi,G orcid.org/0000-0002-5126-4036
Shen,S
Yuan,D
Journal name Acta Geologica Sinica
Volume number 88
Issue number 2
Start page 365
End page 379
Total pages 15
Publisher Wiley-Blackwell Publishing Asia
Place of publication Melbourne, Vic.
Publication date 2014-04
ISSN 0001-5717
1755-6724
Keyword(s) Fusuline
Peri-Gondwanan blocks
Permian
Qiangtang Block
Tibet
Summary A Kubergandian (Kungurian) fusuline fauna from the lower part of the Lugu Formation in the Cuozheqiangma area, central Qiangtang Block is described. This fusuline fauna belongs to the Southern Transitional Zone in palaeobiogeography, and is characterised by the presence of the distinctive bi-temperate genus Monodiexodina and many genera common in lower latitude Tethyan areas such as Parafusulina and Pseudodoliolina. The occurrence of Monodiexodina in the fauna confirms that the seamount-type carbonates of the Lugu Formation did not originate from the Palaeotethys Ocean, but rather from a branch of the Neotethys Ocean after the rifting of the Qiangtang Block from the Tethys Himalaya area in the Artinskian. © 2014 Geological Society of China.
Language eng
DOI 10.1111/1755-6724.12202
Field of Research 060206 Palaeoecology
Socio Economic Objective 960305 Ecosystem Adaptation to Climate Change
HERDC Research category C1 Refereed article in a scholarly journal
Copyright notice ©2014, Wiley-Blackwell
Persistent URL http://hdl.handle.net/10536/DRO/DU:30067946

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