Molar tooth carbonates and benthic methane fluxes in Proterozoic oceans

Bing Shen (), Lin Dong, Shuhai Xiao, Xianguo Lang, Kangjun Huang, Yongbo Peng, Chuanming Zhou, Shan Ke and Pengju Liu
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Bing Shen: Key Laboratory of Orogenic Belts and Crustal Evolution, MOE
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
Kangjun Huang: Key Laboratory of Orogenic Belts and Crustal Evolution, MOE
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

Nature Communications, 2016, vol. 7, issue 1, 1-6

Abstract: 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

Date: 2016
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DOI: 10.1038/ncomms10317

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