Volume 25 Issue 5
Oct.  2019
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Article Navigation >  Journal of Geomechanics  > 2019  >  25(5): 920-931
ZHANG Shuanhong, PEI Junling, HU Guohui, et al., 2019. GENETIC LINK BETWEEN LARGE IGNEOUS PROVINCES AND LARGE VOLUMES OF BLACK SHALE DEPOSITION AND ITS IMPLICATIONS. Journal of Geomechanics, 25 (5): 920-931. DOI: 10.12090/j.issn.1006-6616.2019.25.05.075
Citation: ZHANG Shuanhong, PEI Junling, HU Guohui, et al., 2019. GENETIC LINK BETWEEN LARGE IGNEOUS PROVINCES AND LARGE VOLUMES OF BLACK SHALE DEPOSITION AND ITS IMPLICATIONS. Journal of Geomechanics, 25 (5): 920-931. DOI: 10.12090/j.issn.1006-6616.2019.25.05.075
shu

GENETIC LINK BETWEEN LARGE IGNEOUS PROVINCES AND LARGE VOLUMES OF BLACK SHALE DEPOSITION AND ITS IMPLICATIONS

doi: 10.12090/j.issn.1006-6616.2019.25.05.075
  • 1.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 2.

    Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing 100081, China

More Information
  • Received: 2019-09-01
  • Revised: 2019-09-23
  • Published: 2019-10-31
    Abstract
  • Large igneous provinces (LIPs) have a significant influence on global climate changes and mass extinction events. Previous results show that some of the Global Boundary Stratotype Section and Points (GSSPs) in the Phanerozoic international geologic time scale are corresponding to the coeval global-scale LIPs, mass extinction events and/or ocean anoxic events (OAEs) represented by black shales. However, due to limited knowledge of atmospheric oxygen concentrations, ocean redox conditions and early fossils during the Meso-Neoproterozoic Era prior to the Ediacaran period, little is known on the climate and environmental effects of LIPs and link between LIPs and black shales during a billion years in "Earth's Middle Age" (or "Boring Billion") from 1800 Ma to 800 Ma. Recent results on global distribution of the~1380 Ma LIPs and black shales indicate a temporal and genetic link between the~1380 Ma LIPs and black shales in the Columbia (Nuna) supercontinent. The~1380 Ma LIPs are widely distributed in Baltica, North America, Greenland, Siberia, Kalahari, Congo, West Africa, Amazonia, East Antarctica and West Australia; the coeval black shales have been identified in North China and Northern Australia Graton, and probably in Siberia, Brazil and India Cratons. We proposed that the~1380 Ma black shales were deposited in an and/or several large marine basins, not some restricted basins as previously regarded. Comparisons of the baddeleyite/zircon U-Pb ages of~1380 Ma LIPs and zircon U-Pb ages of tuffs from the black shales within the Xiamaling Formation indicate that global deposition of the~1380 Ma black shales are related to an oceanic anoxic event induced by environment effects of the~1380 Ma LIPs, and the coeval black shales and LIPs provide a robust natural marker for the Calymmian-Ectasian boundary at 1383 Ma. Preliminary results on global distribution of other Meso-Neoproterozoic LIPs and black shales suggest that several other stages of LIPs in "Earth's Middle Age" are correlated with coeval black shales and can potentially provide more natural markers for the Meso-Neoproterozoic geological time scale.

     

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