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Molar tooth carbonates and benthic methane fluxes in Proterozoic oceans

Author

Listed:
  • Bing Shen

    (Key Laboratory of Orogenic Belts and Crustal Evolution, MOE
    School of Earth and Space Sciences, Peking University, No.5 Yiheyuan Road Haidian District, Beijing 100871, China)

  • Lin Dong

    (Key Laboratory of Orogenic Belts and Crustal Evolution, MOE)

  • Shuhai Xiao

    (Virginia Tech)

  • Xianguo Lang

    (Key Laboratory of Orogenic Belts and Crustal Evolution, MOE
    School of Earth and Space Sciences, Peking University, No.5 Yiheyuan Road Haidian District, Beijing 100871, China)

  • Kangjun Huang

    (Key Laboratory of Orogenic Belts and Crustal Evolution, MOE
    School of Earth and Space Sciences, Peking University, No.5 Yiheyuan Road Haidian District, Beijing 100871, China)

  • Yongbo Peng

    (Louisiana State University)

  • Chuanming Zhou

    (Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences)

  • Shan Ke

    (State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences)

  • Pengju Liu

    (Institute of Geology, Chinese Academy of Geological Sciences)

Abstract

Molar tooth structures are ptygmatically folded and microspar-filled structures common in early- and mid-Proterozoic (∼2,500–750 million years ago, Ma) subtidal successions, but extremely rare in rocks

Suggested Citation

  • Bing Shen & Lin Dong & Shuhai Xiao & Xianguo Lang & Kangjun Huang & Yongbo Peng & Chuanming Zhou & Shan Ke & Pengju Liu, 2016. "Molar tooth carbonates and benthic methane fluxes in Proterozoic oceans," Nature Communications, Nature, vol. 7(1), pages 1-6, April.
    • Handle: RePEc:nat:natcom:v:7:y:2016:i:1:d:10.1038_ncomms10317
    DOI: 10.1038/ncomms10317
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