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Manganese and iron reduction dominate organic carbon oxidation in surface sediments of the deep Ulleung Basin, East Sea

Title
Manganese and iron reduction dominate organic carbon oxidation in surface sediments of the deep Ulleung Basin, East Sea
Author
김성한
Keywords
CONTINENTAL-MARGIN SEDIMENTS; BACTERIAL SULFATE REDUCTION; CLIPPERTON FRACTURE-ZONE; COASTAL MARINE-SEDIMENTS; ACID VOLATILE SULFIDE; SALT-MARSH SEDIMENTS; MATTER MINERALIZATION; EAST SEA; HEMIPELAGIC SEDIMENTS
Issue Date
2017-03
Publisher
European Geosciences Union (EGU).
Citation
Biogeosciences, v. 14, No. 4, Page. 941-958
Abstract
Rates and pathways of benthic organic carbon (Corg) oxidation were investigated in surface sediments of the Ulleung Basin (UB) characterized by high Corg contents (˃ 2.5 %, dry wt.) and very high contents of Mn oxides (˃ 200 mu mol cm(-3)) and Fe oxides (up to 100 mu mol cm(-3)). The combination of geochemical analyses and independently executed metabolic rate measurements revealed that Mn and Fe reduction were the dominant Corg oxidation pathways in the center of the UB, comprising 45 and 20% of total Corg oxidation, respectively. By contrast, sulfate reduction was the dominant Corg oxidation pathway, accounting for 50% of total Corg mineralization in sediments of the continental slope. The relative significance of each Corg oxidation pathway matched the depth distribution of the respective electron acceptors. The relative importance of Mn reduction for Corg oxidation displays saturation kinetics with respect to Mn oxide content with a low half-saturation value of 8.6 mu mol cm(-3), which further implies that Mn reduction can be a dominant Corg oxidation process even in sediments with lower MnO2 content as known from several other locations. This is the first report of a high contribution of manganese reduction to Corg oxidation in offshore sediments on the Asian margin. The high manganese oxide content in the surface sediment in the central UB was maintained by an extreme degree of recycling, with each Mn atom on average being reoxidized similar to 3800 times before permanent burial. This is the highest degree of recycling so far reported for Mn-rich sediments, and it appears linked to the high benthic mineralization rates resulting from the high Corg content that indicate the UB as a biogeochemical hotspot for turnover of organic matter and nutrient regeneration.
URI
http://findresearcher.sdu.dk:8080/portal/en/publications/id(dd20e4ee-1743-4ccf-bd14-79240b936b51).htmlhttps://repository.hanyang.ac.kr/handle/20.500.11754/72005
ISSN
1726-4170; 1726-4189
DOI
10.5194/bg-14-941-2017
Appears in Collections:
RESEARCH INSTITUTE[E](부설연구소) > INSTITUTE OF OCENA AND ATMOSPHERIC SCIENCES(해양ㆍ대기과학연구소) > Articles
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