青白口纪宏观藻类生物群及其古地理意义

刘傲然; 冯庆来; 田立富

doi:10.3799/dqkx.2018.023

Volume 43 Issue 2

Feb. 2018

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Liu Aoran, Feng Qinglai, Tian Lifu, 2018. The Qingbaikou Macroalgae Biota and Their Implications for Rodinia Reconstruction. Earth Science, 43(2): 475-490. doi: 10.3799/dqkx.2018.023

Citation:

Liu Aoran, Feng Qinglai, Tian Lifu, 2018. The Qingbaikou Macroalgae Biota and Their Implications for Rodinia Reconstruction. Earth Science, 43(2): 475-490. doi: 10.3799/dqkx.2018.023

Liu Aoran, Feng Qinglai, Tian Lifu, 2018. The Qingbaikou Macroalgae Biota and Their Implications for Rodinia Reconstruction. Earth Science, 43(2): 475-490. doi: 10.3799/dqkx.2018.023

Citation:

Liu Aoran, Feng Qinglai, Tian Lifu, 2018. The Qingbaikou Macroalgae Biota and Their Implications for Rodinia Reconstruction. Earth Science, 43(2): 475-490. doi: 10.3799/dqkx.2018.023

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The Qingbaikou Macroalgae Biota and Their Implications for Rodinia Reconstruction

doi: 10.3799/dqkx.2018.023

Liu Aoran^{1,2
,},
Feng Qinglai^{1,3
,
,},
Tian Lifu²

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
College of Resource, Hebei GEO University, Shijiazhuang 050031, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2017-11-17
Publish Date: 2018-02-15

Abstract

Abstract

The evolution of Rodinia surpercontinent has always been of concern as an important scientific issue. Paleobiogeographic region analysis, as an effective method to solve the problem of the tectonic reconstruction of the continental masses, has rarely been applied to Rodinia. Longfengshan biota, characterized by Chuaria-Tawuia-Longfengshania, is one of the typical biota, whose biotic factor can be found globally, in the nearshore shallow water basin and Lagoon, Tonian. According to the reliable existing biota data reported globally, we make the paleobiogeographic analysis, zoning them into North China Craton-North Laurentia region(Chuaria-Tawuia-Longfengshania) and Yangtze Craton-India Craton region (Chuaria-Tawuia), constitute a low-latitude-Macroalgae realm (1 000-780 Ma). Furthermore, we have a new cognition on the position of North China Craton, in the east of Rodinia surpercontinent, near Laurentia Craton, and Yangtze Craton in the west, close to India Craton.
- Longfengshan biota,
- paleobiogeography,
- macroalgae,
- Rodinia supercontinent,
- paleontology

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References(110)

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