Petrographical and Geochemical Signatures Linked to Fe/Mn Reduction in Subsurface Marine Sediments from the Hydrate-Bearing Area, Dongsha, the South China Sea
Abstract:Fe and Mn oxides and (oxy)-hydroxides are the most abundant solid-phase electron acceptors in marine sediments, and dissimilatory Fe/Mn reduction usually links with the anaerobic oxidation of methane (AOM) and organic matter oxidation (OMO) in sediments. In this study, we report the results from subsurface marine sediments in the Dongsha hydrate-bearing area in the South China Sea. The petrological and geochemical signatures show that the Fe/Mn reduction mediated by AOM and OMO might occur in sediments above t… Show more
“…A large number of findings have since been emerging about the biogeochemistry of cold seep carbonates, benthos, and sediments in the Haima cold seep ( 30 – 33 ). Massive amounts of terrigenous metal oxides are supplied into the continental slope of the South China Sea from rivers ( 34 ). Consequently, iron/manganese-containing minerals are part of the major components in the sediments of this region with high-flux methane seeps, rendering it a natural laboratory to investigate the role of metal oxides in the methane cycle.…”
Anaerobic oxidation of methane (AOM) coupled with reduction of metal oxides is supposed to be a globally important bioprocess in marine sediments. However, the responsible microorganisms and their contributions to methane budget are not clear in deep sea cold seep sediments.
“…A large number of findings have since been emerging about the biogeochemistry of cold seep carbonates, benthos, and sediments in the Haima cold seep ( 30 – 33 ). Massive amounts of terrigenous metal oxides are supplied into the continental slope of the South China Sea from rivers ( 34 ). Consequently, iron/manganese-containing minerals are part of the major components in the sediments of this region with high-flux methane seeps, rendering it a natural laboratory to investigate the role of metal oxides in the methane cycle.…”
Anaerobic oxidation of methane (AOM) coupled with reduction of metal oxides is supposed to be a globally important bioprocess in marine sediments. However, the responsible microorganisms and their contributions to methane budget are not clear in deep sea cold seep sediments.
“…A large number of findings have since been emerging about the biogeochemistry of cold-seep carbonates, benthos and sediments in Haima cold seep [29][30][31][32] . Massive amounts of terrigenous metal oxides are supplied into the continental slope of the South China Sea from rivers 33 . Consequently, iron/manganese-containing minerals are part of the major components in the sediments of this region with high-flux methane seeps, rendering it be such a natural laboratory to investigate the role of metal oxides in methane cycle.…”
Anaerobic oxidation of methane (AOM) coupled with reduction of metal oxides is supposed to be a globally important bioprocess in marine sediments. However, the responsible microorganisms and their contributions to methane budget are not clear in deep sea cold seep sediments. Here, we combined geochemistry, muti-omics and numerical modeling to study metal-dependent AOM in methanic cold seep sediments in the northern continental slope of the South China Sea. Geochemical data based on methane concentrations, carbon stable isotope, solid-phase sediment analysis and pore water measurements indicate the occurrence of anaerobic methane oxidation coupled to metal oxides reduction in the methanic zone. The 16S rRNA gene amplicons and transcripts, along with metagenomic and metatranscriptomic data suggest that diverse ANME groups actively mediated methane oxidation in the methanic zone either independently or in syntrophy with e.g. ETH-SRB1 as potential metal reducers. Modeling results suggest that the estimated rates of methane consumption via Fe-AOM and Mn-AOM were both 0.3 μmol cm-2 yr-1, which account for ~3% of total CH4 removal in sediments. Overall, our results highlight metal-driven anaerobic oxidation of methane as an important methane sink in methanic cold seep sediments.
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