A shallow-water oxygen minimum zone in an oligotrophic Tonian basin

The Tonian Period (1000-720 Ma) bore witness to the transition from a prokaryote-dominated marine ecosystem to one characterized by the proliferation of eukaryotes. This fundamental shift has generally been attributed to evolving marine redox states. Here, we present sedimentological and geochemical analyses of the early Tonian Huainan, Feishui, and Huaibei groups in the Xuhuai basin of the North China craton. Multiple redox proxies show consistent, water depth-dependent variations across the Xuhuai basin. Excess barium contents and Ba/Al ratios further highlight spatial variations in primary productivity which ultimately regulate basinal redox structures. We propose that a shallow-water oxygen minimum zone sandwiched between the oxic/suboxic mid-depth and surface layer water masses occur in the oligotrophic Xuhuai basin, which is analogous to, but much shallower than modern oxygen minimum zones. Such marine redox architectures may benefit the maintenance of a bioavailable nitrate reservoir in the ocean, foreboding the subsequent expansion of eukaryotes.

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Publication Details

Journal
Nature Communications
Published
2025-01-16
DOI
https://doi.org/10.1038/s41467-025-55881-3
Citations
8
Primary Topic
Paleontology and Stratigraphy of Fossils
Type
article
Field-Weighted Citation Impact
34.63

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article

A shallow-water oxygen minimum zone in an oligotrophic Tonian basin

Xianguo Lang, Xianye Zhao, Chuanming Zhou, Qing Ouyang et al.
8 citations
Nature Communications
Paleontology and Stratigraphy of Fossils
34.63
article

A shallow-water oxygen minimum zone in an oligotrophic Tonian basin

Xianguo Lang, Xianye Zhao, Chuanming Zhou, Qing Ouyang, Yongliang Hu, Guangjin Li, Ke Pang, Wei Wang, Hongyi Shi, Chengguo Guan, Yunpeng Sun
article en
8 citations

Abstract

The Tonian Period (1000-720 Ma) bore witness to the transition from a prokaryote-dominated marine ecosystem to one characterized by the proliferation of eukaryotes. This fundamental shift has generally been attributed to evolving marine redox states. Here, we present sedimentological and geochemical analyses of the early Tonian Huainan, Feishui, and Huaibei groups in the Xuhuai basin of the North China craton. Multiple redox proxies show consistent, water depth-dependent variations across the Xuhuai basin. Excess barium contents and Ba/Al ratios further highlight spatial variations in primary productivity which ultimately regulate basinal redox structures. We propose that a shallow-water oxygen minimum zone sandwiched between the oxic/suboxic mid-depth and surface layer water masses occur in the oligotrophic Xuhuai basin, which is analogous to, but much shallower than modern oxygen minimum zones. Such marine redox architectures may benefit the maintenance of a bioavailable nitrate reservoir in the ocean, foreboding the subsequent expansion of eukaryotes.

Nature CommunicationsVol. 16(1)
Nanjing University of Chinese Medicine (CN), Vrije Universiteit Brussel (BE), Chinese Academy of Sciences (CN), Chengdu University of Technology (CN), State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation (CN), Nanjing Institute of Geology and Paleontology (CN), University of Chinese Academy of Sciences (CN)
National Natural Science Foundation of China, State Key Laboratory of Palaeobiology and Stratigraphy, National Key Research and Development Program of China
Openalex Percentile: Top 0%
Paleontology and Stratigraphy of Fossils
34.63
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