Global Geology 2012, 15(2) 85-96 DOI:     ISSN: 1673-9736 CN: 22-1371/P

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Keywords
Zhesi brachiopod fauna
Jiamusi-Mongolia Block
reconstruction of tectonopaleogeography
paleolatitude
ocean-land allocation relationship
Authors
WANG Chengwen1
LI Ning1 and ZONG Pu2
PubMed
Article by WANG Chengwen1
Article by LI Ning1 and ZONG Pu2

Biogeographic characteristics of Zhesi brachiopod fauna and reconstruction of tectonopaleogeography of Jiamusi-Mongolia Block

WANG Chengwen1, LI Ning1 and ZONG Pu2

1�� College of Earth Sciences��Jilin University��Changchun 130061��China 2�� School of Earth and Space Sciences��Peking University��Beijing 100871��China

Abstract��

The Kungurian-Capitanian ( Permian) Zhesi branchiopod fauna is mainly composed of cold-water typed taxa with high diversity and abundance�� This fauna is similar with the coeval brachiopod faunas from Timan- Pechora��Svalbard��and Queen Elizabeth Islands of the Boreal Realm��with no real“warm-water”species�� Zhesi brachiopod fauna is a cold-water fauna and should be assigned to the Boreal Realm�� Considering the paleogeographic characteristics of this fauna and the basic rationale of paleobiogeographic provinces being controlled by latitude-temperate��and that the above areas were located at 50°N �� 70°N in the global paleoclimate reconstruction map compiled by Boucot et al�� ��the paleo-latitude of the southern margin of Jiamusi-Mongolia Block��where developed the Zhesi brachiopod fauna��is suggested ranging from 40°N to 60°N�� Zhesi brachiopod fauna is an endemic fauna��containing more than 75% endemic species and self-grouped as a biogeographic province��termed Inner Mongolia Province�� These characteristics indicate that this area was closed or semiclosed at that time�� On the Jiamusi-Mongolia Block��the Herlen-Jiamusi Old-land as an obvious“continental barrier”hindered the northward migration of the Zhesi brachiopod fauna and the immigration of brachiopod species from other areas�� The Tarim plate has collided with the Kazakhstan plate and the western part of South Tianshan-Beishan-Xar Moron Ocean has been closed�� At the same time��the western margin of Jiamusi-Mongolia Block was joined with the Tarim plate�� The Xar Moron Ocean in south of Jiamusi-Mongolia Block was wide enough and the ocean temperature rose gradually southward��so that it is not suitable for the cold-water brachiopods to survive and thrive on the northern margin of the North China plate�� Thus��the ocean with large width and high temperature formed another natural barrier for the southward migration of the cold-water brachiopods��

Keywords�� Zhesi brachiopod fauna   Jiamusi-Mongolia Block   reconstruction of tectonopaleogeography   paleolatitude   ocean-land allocation relationship  
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