The Termination and Aftermath of the Lomagundi-Jatuli Carbon Isotope Excursions in the Paleoproterozoic Hutuo Group, North China

Zhenbing She; Fanyan Yang; Wei Liu; Luhua Xie; Yusheng Wan; Chao Li; Dominic Papineau

doi:10.1007/s12583-015-0654-4

Volume 27 Issue 2

Mar 2016

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Journal of Earth Science > 2016 > 27(2): 297-316.

Zhenbing She, Fanyan Yang, Wei Liu, Luhua Xie, Yusheng Wan, Chao Li, Dominic Papineau. The Termination and Aftermath of the Lomagundi-Jatuli Carbon Isotope Excursions in the Paleoproterozoic Hutuo Group, North China. Journal of Earth Science, 2016, 27(2): 297-316. doi: 10.1007/s12583-015-0654-4

Citation:

Zhenbing She, Fanyan Yang, Wei Liu, Luhua Xie, Yusheng Wan, Chao Li, Dominic Papineau. The Termination and Aftermath of the Lomagundi-Jatuli Carbon Isotope Excursions in the Paleoproterozoic Hutuo Group, North China. Journal of Earth Science, 2016, 27(2): 297-316. doi: 10.1007/s12583-015-0654-4

Citation:

Zhenbing She, Fanyan Yang, Wei Liu, Luhua Xie, Yusheng Wan, Chao Li, Dominic Papineau. The Termination and Aftermath of the Lomagundi-Jatuli Carbon Isotope Excursions in the Paleoproterozoic Hutuo Group, North China. Journal of Earth Science, 2016, 27(2): 297-316. doi: 10.1007/s12583-015-0654-4

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The Termination and Aftermath of the Lomagundi-Jatuli Carbon Isotope Excursions in the Paleoproterozoic Hutuo Group, North China

doi: 10.1007/s12583-015-0654-4

Zhenbing She^{1, 2
,
,},
Fanyan Yang³,
Wei Liu⁴,
Luhua Xie^{5, 6},
Yusheng Wan⁷,
Chao Li¹,
Dominic Papineau^{8, 9}

1.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Ningxia Geology And Mineral Resources Centre Lab, Yinchuan 750021, China
4.
Tianjin Research Institute for Water Transport Engineering, M. O. T., Tianjin 300456, China
5.
State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
6.
Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
7.
Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
8.
London Centre for Nanotechnology, University College London, London
9.
Department of Earth Sciences, University College London, 17-19 Gower Street, London, United Kingdom

More Information

Corresponding author: Zhenbing She, zbsher@cug.edu.cn
Received Date: 24 Mar 2015
Accepted Date: 17 Sep 2015
Publish Date: 01 Apr 2016

Abstract

Abstract

The Lomagundi-Jatuli Event (LJE) is one of the largest and earliest positive carbon isotope excursions preserving δ¹³C_carb values between +5 and +16‰ in Paleoproterozoic carbonates worldwide. However, the duration, amplitude and patterns of these excursions remain poorly constrained. The 2.14-1.83 Ga Hutuo Group in the North China Craton is a > 10 km thick volcano-sedimentary sequence, including > 5 km thick well-preserved carbonates that were deposited in supra-tidal to sub-tidal environments. C-O isotopic and elemental analyses of 152 least altered samples of the carbonates revealed a three-stage δ¹³C evolution. It began with an exclusively positive δ¹³C_carb (+1.3 to + 3.4‰) stage in the ~2.1 Ga carbonate in the Dashiling and Qingshicun Formations, followed by a transition from positive values to oscillating positive and negative values in ~3 000 m thick carbonates of the Wenshan, Hebiancun, Jianancun, and Daguandong Formations, and end with exclusively negative δ¹³C_carb values preserved in > 500 m thick dolostones of the Huaiyincun and Beidaxing Formations. It appears that much of the LJE, particularly those extremely positive δ¹³C_carb signals, was not recorded in the Hutuo carbonates. The exclusively positive δ¹³C_carb values (+1.3 to + 3.4‰) preserved in the lower formations likely correspond to the end of the LJE, whereas the subsequent two stages reflect the aftermath of the LJE and the onset of Shunga-Francevillian event (SFE). The present data point to an increased influence of oxygen on the carbon cycle from the Doucun to the Dongye Subgroups and demonstrate that the termination of the LJE in the North China Craton is nearly simultaneous with those in Fennoscandia and South Africa.
- Paleoproterozoic,
- Lomagundi-Jatuli event,
- Hutuo Group,
- carbon isotope,
- carbonate

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References(69)

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The Termination and Aftermath of the Lomagundi-Jatuli Carbon Isotope Excursions in the Paleoproterozoic Hutuo Group, North China

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