Thermochemical oxidation of methane by manganese oxides in hydrothermal sediments

Microbial anaerobic oxidation of methane coupled to the reduction of Mn(IV)-oxides, typically MnO 2 , derived from continental weathering and riverine transport has been proposed as a globally important sink of methane. However, the potential role of hydrothermal Mn(IV) oxide-rich sediments as a met...

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Published inCommunications earth & environment Vol. 4; no. 1; pp. 224 - 10
Main Authors Huang, Qin, Jiang, Shao-Yong, Pi, Dao-Hui, Konhauser, Kurt O., Wen, Xing-Ping, Lu, Liu-Yi, Yan, Hao
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group 01.12.2023
Nature Portfolio
Subjects
Anaerobic microorganisms
Carbon isotopes
Diagenesis
Geochemistry
Hausmannite
High temperature
Manganese
Manganese dioxide
Manganese ores
Manganese oxides
Methane
Microorganisms
Oceans
Oxidation
Oxides
Petrography
Sediments
Triassic
China
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ISSN2662-4435
2662-4435
DOI10.1038/s43247-023-00891-6

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Abstract Microbial anaerobic oxidation of methane coupled to the reduction of Mn(IV)-oxides, typically MnO 2 , derived from continental weathering and riverine transport has been proposed as a globally important sink of methane. However, the potential role of hydrothermal Mn(IV) oxide-rich sediments as a methane sink, and the mechanisms of underpinning methane oxidation at high-temperature hydrothermal fields remain poorly understood. Here, we report the occurrence of almost pure rhodochrosite with extremely negative δ 13 C PDB values (as low as –76.4‰) in direct association with hausmannite formed through hydrothermal activity in the Late Triassic Heqing Mn deposit in Southern China. Based on detailed petrography and geochemistry, this rhodochrosite is interpreted as the result of the thermochemical oxidation of methane by hausmannite during early diagenesis. Given high hydrothermal Mn 2+ and CH 4 release coupled to low sulfate concentration observed in the Archean oceans, we propose that hydrothermal Mn(IV) oxides may have been effective methane sinks in Earth’s ancient oceans.
AbstractList Microbial anaerobic oxidation of methane coupled to the reduction of Mn(IV)-oxides, typically MnO2, derived from continental weathering and riverine transport has been proposed as a globally important sink of methane. However, the potential role of hydrothermal Mn(IV) oxide-rich sediments as a methane sink, and the mechanisms of underpinning methane oxidation at high-temperature hydrothermal fields remain poorly understood. Here, we report the occurrence of almost pure rhodochrosite with extremely negative δ13CPDB values (as low as –76.4‰) in direct association with hausmannite formed through hydrothermal activity in the Late Triassic Heqing Mn deposit in Southern China. Based on detailed petrography and geochemistry, this rhodochrosite is interpreted as the result of the thermochemical oxidation of methane by hausmannite during early diagenesis. Given high hydrothermal Mn2+ and CH4 release coupled to low sulfate concentration observed in the Archean oceans, we propose that hydrothermal Mn(IV) oxides may have been effective methane sinks in Earth’s ancient oceans.Rhodochrosite with very negative carbon isotope values is identified in association with hausmannite in manganese ores from the Late Triassic Heqing deposit, China, and could have formed from high-temperature oxidation of methane during early diagenesis.
Abstract Microbial anaerobic oxidation of methane coupled to the reduction of Mn(IV)-oxides, typically MnO2, derived from continental weathering and riverine transport has been proposed as a globally important sink of methane. However, the potential role of hydrothermal Mn(IV) oxide-rich sediments as a methane sink, and the mechanisms of underpinning methane oxidation at high-temperature hydrothermal fields remain poorly understood. Here, we report the occurrence of almost pure rhodochrosite with extremely negative δ13CPDB values (as low as –76.4‰) in direct association with hausmannite formed through hydrothermal activity in the Late Triassic Heqing Mn deposit in Southern China. Based on detailed petrography and geochemistry, this rhodochrosite is interpreted as the result of the thermochemical oxidation of methane by hausmannite during early diagenesis. Given high hydrothermal Mn2+ and CH4 release coupled to low sulfate concentration observed in the Archean oceans, we propose that hydrothermal Mn(IV) oxides may have been effective methane sinks in Earth’s ancient oceans.
Microbial anaerobic oxidation of methane coupled to the reduction of Mn(IV)-oxides, typically MnO 2 , derived from continental weathering and riverine transport has been proposed as a globally important sink of methane. However, the potential role of hydrothermal Mn(IV) oxide-rich sediments as a methane sink, and the mechanisms of underpinning methane oxidation at high-temperature hydrothermal fields remain poorly understood. Here, we report the occurrence of almost pure rhodochrosite with extremely negative δ 13 C PDB values (as low as –76.4‰) in direct association with hausmannite formed through hydrothermal activity in the Late Triassic Heqing Mn deposit in Southern China. Based on detailed petrography and geochemistry, this rhodochrosite is interpreted as the result of the thermochemical oxidation of methane by hausmannite during early diagenesis. Given high hydrothermal Mn 2+ and CH 4 release coupled to low sulfate concentration observed in the Archean oceans, we propose that hydrothermal Mn(IV) oxides may have been effective methane sinks in Earth’s ancient oceans.
ArticleNumber 224
Author Jiang, Shao-Yong
Wen, Xing-Ping
Huang, Qin
Yan, Hao
Konhauser, Kurt O.
Pi, Dao-Hui
Lu, Liu-Yi
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Snippet Microbial anaerobic oxidation of methane coupled to the reduction of Mn(IV)-oxides, typically MnO 2 , derived from continental weathering and riverine...
Microbial anaerobic oxidation of methane coupled to the reduction of Mn(IV)-oxides, typically MnO2, derived from continental weathering and riverine transport...
Abstract Microbial anaerobic oxidation of methane coupled to the reduction of Mn(IV)-oxides, typically MnO2, derived from continental weathering and riverine...
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SubjectTerms Anaerobic microorganisms
Carbon isotopes
Diagenesis
Geochemistry
Hausmannite
High temperature
Manganese
Manganese dioxide
Manganese ores
Manganese oxides
Methane
Microorganisms
Oceans
Oxidation
Oxides
Petrography
Sediments
Triassic
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Title Thermochemical oxidation of methane by manganese oxides in hydrothermal sediments
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