Molar tooth carbonates and benthic methane fluxes in Proterozoic oceans

Molar tooth carbonates and benthic methane fluxes in Proterozoic oceans

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

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Bibliographische Detailangaben
Veröffentlicht in:Nature communications 2016-01, Vol.7 (1), p.10317-10317, Article 10317
Hauptverfasser: Shen, Bing, Dong, Lin, Xiao, Shuhai, Lang, Xianguo, Huang, Kangjun, Peng, Yongbo, Zhou, Chuanming, Ke, Shan, Liu, Pengju
Format: Artikel
Sprache:eng
Schlagworte:
704/158/47
704/2151/213
704/2151/2738
704/2151/2809
Carbonates - chemistry
Fossils
Humanities and Social Sciences
Magnesium - analysis
Methane - metabolism
Molar - chemistry
multidisciplinary
Oxidation-Reduction
Science
Science (multidisciplinary)
Sulfates - metabolism
Sulfides - metabolism
Sulfur Isotopes - analysis
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Beschreibung
Zusammenfassung: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
ISSN:2041-1723
2041-1723
DOI:10.1038/ncomms10317