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- W2592382487 endingPage "958" @default.
- W2592382487 startingPage "941" @default.
- W2592382487 abstract "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 µmol cm−3) and Fe oxides (up to 100 µmol 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 µmol 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 ∼ 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." @default.
- W2592382487 created "2017-03-16" @default.
- W2592382487 creator A5013095317 @default.
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- W2592382487 creator A5057235495 @default.
- W2592382487 creator A5057288476 @default.
- W2592382487 creator A5067286446 @default.
- W2592382487 date "2017-03-01" @default.
- W2592382487 modified "2023-10-17" @default.
- W2592382487 title "Manganese and iron reduction dominate organic carbon oxidation in surface sediments of the deep Ulleung Basin, East Sea" @default.
- W2592382487 cites W1512098610 @default.
- W2592382487 cites W1552936675 @default.
- W2592382487 cites W1586239332 @default.
- W2592382487 cites W161482917 @default.
- W2592382487 cites W194483290 @default.
- W2592382487 cites W1965193842 @default.
- W2592382487 cites W1969394853 @default.
- W2592382487 cites W1970465286 @default.
- W2592382487 cites W1974361251 @default.
- W2592382487 cites W197444862 @default.
- W2592382487 cites W1978530465 @default.
- W2592382487 cites W1979717448 @default.
- W2592382487 cites W1982050236 @default.
- W2592382487 cites W1986404326 @default.
- W2592382487 cites W1988291936 @default.
- W2592382487 cites W1990611318 @default.
- W2592382487 cites W1991421453 @default.
- W2592382487 cites W2002200270 @default.
- W2592382487 cites W2002235658 @default.
- W2592382487 cites W2005639928 @default.
- W2592382487 cites W2005990125 @default.
- W2592382487 cites W2010282358 @default.
- W2592382487 cites W2013398329 @default.
- W2592382487 cites W2014766704 @default.
- W2592382487 cites W2018052335 @default.
- W2592382487 cites W2028921645 @default.
- W2592382487 cites W2029048327 @default.
- W2592382487 cites W2029438495 @default.
- W2592382487 cites W2034653555 @default.
- W2592382487 cites W2035061771 @default.
- W2592382487 cites W2037190201 @default.
- W2592382487 cites W2037582162 @default.
- W2592382487 cites W2038338599 @default.
- W2592382487 cites W2038349674 @default.
- W2592382487 cites W2038360704 @default.
- W2592382487 cites W2041926482 @default.
- W2592382487 cites W2042225411 @default.
- W2592382487 cites W2043612119 @default.
- W2592382487 cites W2043668123 @default.
- W2592382487 cites W2044233272 @default.
- W2592382487 cites W2044357613 @default.
- W2592382487 cites W2045107431 @default.
- W2592382487 cites W2046007293 @default.
- W2592382487 cites W2047550514 @default.
- W2592382487 cites W2048310861 @default.
- W2592382487 cites W2052996965 @default.
- W2592382487 cites W2054645658 @default.
- W2592382487 cites W2056392157 @default.
- W2592382487 cites W2062988577 @default.
- W2592382487 cites W2064514607 @default.
- W2592382487 cites W2065504687 @default.
- W2592382487 cites W2067890461 @default.
- W2592382487 cites W2068489309 @default.
- W2592382487 cites W2069186965 @default.
- W2592382487 cites W2069232403 @default.
- W2592382487 cites W2073456692 @default.
- W2592382487 cites W2073470532 @default.
- W2592382487 cites W2077506757 @default.
- W2592382487 cites W2082250875 @default.
- W2592382487 cites W2085181344 @default.
- W2592382487 cites W2085333478 @default.
- W2592382487 cites W2090240224 @default.
- W2592382487 cites W2091456728 @default.
- W2592382487 cites W2091913250 @default.
- W2592382487 cites W2101441039 @default.
- W2592382487 cites W2104463724 @default.
- W2592382487 cites W2106809403 @default.
- W2592382487 cites W2111598462 @default.
- W2592382487 cites W2114797059 @default.
- W2592382487 cites W2117421676 @default.
- W2592382487 cites W2124535797 @default.
- W2592382487 cites W2135113899 @default.
- W2592382487 cites W2140673114 @default.
- W2592382487 cites W2142462683 @default.
- W2592382487 cites W2146771742 @default.
- W2592382487 cites W2150393300 @default.
- W2592382487 cites W2160770158 @default.
- W2592382487 cites W2162291034 @default.
- W2592382487 cites W2163717864 @default.
- W2592382487 cites W2164424086 @default.
- W2592382487 cites W2166403415 @default.
- W2592382487 cites W2167881866 @default.
- W2592382487 cites W2169082262 @default.
- W2592382487 cites W2171472582 @default.
- W2592382487 cites W2171788173 @default.
- W2592382487 cites W2467982116 @default.