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The marine redox change and nitrogen cycle in the Early Cryogenian interglacial time: Evidence from nitrogen isotopes and Mo contents of the basal Datangpo Formation, northeastern Guizhou, South China

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Abstract

Cryogenian Datangpo Formation was deposited during the interglacial time between the Sturtian and Marinoan ice ages. We studied nitrogen isotope compositions and contents of Mo of the black shales from the basal Datangpo Formation in northeastern Guizhou, South China, for an attempt to reconstruct the marine redox change and nitrogen cycle during the interglacial time. Based on lithostratigraphy as well as geochemical profiles, the basal black shales can be divided into four intervals: Interval 1 has the lowest δ15N value (+5.0‰); in interval 2, δ15N values vary between +6.4‰ and +7.4‰ (the first peak); interval 3 records stable values of δ15N around +6‰; and interval 4 is characterized by its higher δ15N values, between +6.7‰ and +7.8‰ (the second peak). The values of enrichment factor of Mo decrease from 56.8 to 2.6 with the ascending stratigraphic trend. It indicated that immediately after the Sturtian glaciations, the marine seawater above the transitional zone between the shelf to slope of the southern margin of the Yangtze Platform was stratified, with shallow seawater being oxic but deep water being sulfidic. Subsequently, high denitrification rates prevailed in expanded suboxic areas in spite of a short emergence of an oxic condition in the surface seawater, and the deep seawaters were still anoxic or even euxinic.

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  1. State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences, Nanjing University, Nanjing, 210023, China

    Wei Wei, Dan Wang, Da Li, Hongfei Ling, Xi Chen & Guangyi Wei

  2. Institute of Geology, CAGS, Laboratory of Isotope Geology, MLR, State Key Laboratory for Continental Tectonics and Dynamics, Beijing, 100037, China

    Feifei Zhang, Xiangkun Zhu & Bin Yan

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  1. Wei Wei
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  2. Dan Wang
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  3. Da Li
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Correspondence to Dan Wang.

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Wei, W., Wang, D., Li, D. et al. The marine redox change and nitrogen cycle in the Early Cryogenian interglacial time: Evidence from nitrogen isotopes and Mo contents of the basal Datangpo Formation, northeastern Guizhou, South China. J. Earth Sci. 27, 233–241 (2016). https://doi.org/10.1007/s12583-015-0657-1

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