Methane-derived authigenic carbonate from the lower Doushantuo Formation of South China: Implications for seawater sulfate concentration and global carbon cycle in the early Ediacaran ocean

Methane-derived authigenic carbonate from the lower Doushantuo Formation of South China: Implications for seawater sulfate concentration and global carbon cycle in the early Ediacaran ocean

Authigenic carbonate associated with anaerobic oxidation of methane (AOM), usually via microbial sulfate reduction (MSR) or ferric iron reduction, is generally characterized by extremely low δ13C values (

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Veröffentlicht in:Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2016-11, Vol.461, p.145-155
Hauptverfasser: Zhou, Chuanming, Guan, Chengguo, Cui, Huan, Ouyang, Qing, Wang, Wei
Format: Artikel
Sprache:eng
Schlagworte:
Anaerobic oxidation of methane
Carbon cycle
Carbon isotope chemostratigraphy
Cold seep deposits
Marine
Microbial sulfate reduction
Sulfur cycle
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Zusammenfassung:Authigenic carbonate associated with anaerobic oxidation of methane (AOM), usually via microbial sulfate reduction (MSR) or ferric iron reduction, is generally characterized by extremely low δ13C values (
ISSN:0031-0182
1872-616X
DOI:10.1016/j.palaeo.2016.08.017