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Permian radiolarian faunas from chert in the Khabarovsk Complex, Far East Russia, and the age of each lithologic unit of the Khabarovsk Complex

Published online by Cambridge University Press:  11 August 2017

Noritoshi Suzuki ,
Satoru Kojima ,
Harumasa Kano ,
Satoshi Yamakita ,
Akihiro Misaki ,
Masayuki Ehiro ,
Shigeru Otoh ,
Toshiyuki Kurihara  and
Masashi Aoyama
Noritoshi Suzuki
Affiliation:
Institute of Geology and Paleontology, Graduate School of Sciences, Tohoku University, Sendai 980–8578, Japan,
Satoru Kojima
Affiliation:
Department of Civil Engineering, Faculty of Technology, Gifu University, Gifu 501–1193, Japan
Harumasa Kano
Affiliation:
Institute of Geology and Paleontology, Graduate School of Sciences, Tohoku University, Sendai 980–8578, Japan,
Satoshi Yamakita
Affiliation:
Department of Earth Sciences, Faculty of Education and Culture, Miyazaki University, Miyazaki 889–2192, Japan
Akihiro Misaki
Affiliation:
Institute of Geology and Paleontology, Graduate School of Sciences, Tohoku University, Sendai 980–8578, Japan,
Masayuki Ehiro
Affiliation:
The Tohoku University Museum, Sendai 980–8578, Japan
Shigeru Otoh
Affiliation:
Department of Earth Sciences, Faculty of Science, Toyama University, 3190 Gofuku, Toyama 930–8555, Japan
Toshiyuki Kurihara
Affiliation:
Department of Geology, Faculty of Science, Niigata University, Niigata 950–2181, Japan
Masashi Aoyama
Affiliation:
Department of Earth Sciences, Faculty of Science, Toyama University, 3190 Gofuku, Toyama 930–8555, Japan
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Abstract

The Khabarovsk Complex, a Jurassic accretionary complex distributed in and around the Khabarovsk city area, Far East Russia, comprises mélange and schist facies. From the review of previous studies including Russian papers, the lithology and age of the constituent rocks of the mélange facies can be summarized as follows: Upper Paleozoic basic volcanic rocks, mainly pillow lava, and altered gabbro, Upper Carboniferous to Upper Permian fusulinoidean-bearing limestone associated with tuff, Lower and Middle Jurassic siliceous mudstone, Upper Jurassic tuffaceous mudstone, uppermost Jurassic carbonate concretions embedded in mudstone, and age-unknown sandstone. Newly found sequences of limestone-chert and of basalt-chert in the mélange facies crop out along the Amur River in the Khabarovsk city area. A chert sample of the limestone-chert sequence contains Albaillella aff. asymmetrica and Pseudoalbaillella aff. lomentaria, and a chert sample of the basalt-chert sequence includes Follicucullus monacanthus, Follicucullus porrectus, and Pseudoalbaillella cf. yanaharaensis. The radiolarian assemblages from the limestone-chert and basalt-chert sequences have a maximum age of middle Early Permian and late Middle Permian, respectively, overlapping the time of deposition of the fusulinoidean-bearing limestone. The co-occurrence of chert and limestone indicates that the fusulinoidean-bearing limestone was formed on a basaltic topographic high in a pelagic ocean whereas the radiolarians accumulated in a deeper part. Limestone debris occasionally flowed into the depositional site of the radiolarian chert. Although the Khabarovsk Complex was simply considered as a northern extension of the Mino-Tamba Belt of the Inner Zone of southwest Japan, we propose a new correlation based on the lithologic associations. The mélange facies of the Khabarovsk Complex is correlative with one of the Kasugano, Funabuseyama, Nabi, and Yabuhara Formations in the Mino-Tamba Belt, whereas the schist facies is correlative with the Hikami Formation of the Ultra-Tamba Belt.

Type
Research Article
Information
Journal of Paleontology , Volume 79 , Issue 4 , July 2005 , pp. 687 - 701
Copyright
Copyright © The Paleontological Society 

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