Articles | Volume 14, issue 4
https://doi.org/10.5194/bg-14-941-2017
https://doi.org/10.5194/bg-14-941-2017
Research article
 | 
01 Mar 2017
Research article |  | 01 Mar 2017

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

Jung-Ho Hyun, Sung-Han Kim, Jin-Sook Mok, Hyeyoun Cho, Tongsup Lee, Verona Vandieken, and Bo Thamdrup

Cited articles

Aller, R. C.: Bioturbation and manganese cycling in hemipelagic sediments, Philos. T. R. Soc. Lond. A, 331, 51–68, 1990.
Aller, R. C., Hall, P. O. J., Rude, P. D., and Aller, J. Y.: Biogeochemical heterogeneity and suboxic diagenesis in hemipelagic sediments of the Panama Basin, Deep-Sea Res. Pt. I, 45, 133–165, 1998.
Berg, P., Risgaard-Petersen, N., and Rysgaard, S.: Interpretation shelf and slope: A comparison of in situ microelectrode and chamber flux measurements, Limnol. Oceanogr., 37, 614–629, 1998.
Boudreau, B. P.: Is burial velocity a master parameter for bioturbation?, Geochim. Cosmochim. Ac., 58, 1243–1249, 1994.
Bowles, M. W., Mogollón, J. M., Kasten, S., Zabel, M., and Hinrichs, K. U.: Global rates of marine sulfate reduction and implications for sub-sea-floor metabolic activities, Science, 344, 889–891, 2014.
Download
Short summary
The surface sediments of the Ulleung Basin (UB) in the East Sea are characterized by high organic carbon contents (> 2.5 %, dry wt.) and very high concentrations of Mn oxides (> 200 μmol cm−3) and Fe oxides (up to 100 μmol cm−3). For the first time in deep offshore sediments on the Asian margin with water depth over 2000 m, we report that Mn reduction and Fe reduction were the dominant organic carbon (Corg) oxidation pathways, comprising 45 % and 20 % of total Corg oxidation, respectively.
Share
Altmetrics
Final-revised paper
Preprint