Articles | Volume 16, issue 3
https://doi.org/10.5194/os-16-729-2020
https://doi.org/10.5194/os-16-729-2020
Research article
 | 
19 Jun 2020
Research article |  | 19 Jun 2020

Biogeochemical processes accounting for the natural mercury variations in the Southern Ocean diatom ooze sediments

Sara Zaferani and Harald Biester

Related authors

Iron oxides control sorption and mobilisation of iodine in a tropical rainforest catchment
Laura Balzer, Katrin Schulz, Christian Birkel, and Harald Biester
SOIL Discuss., https://doi.org/10.5194/soil-2020-20,https://doi.org/10.5194/soil-2020-20, 2020
Manuscript not accepted for further review
Changes in dissolved organic matter quality in a peatland and forest headwater stream as a function of seasonality and hydrologic conditions
Tanja Broder, Klaus-Holger Knorr, and Harald Biester
Hydrol. Earth Syst. Sci., 21, 2035–2051, https://doi.org/10.5194/hess-21-2035-2017,https://doi.org/10.5194/hess-21-2035-2017, 2017
Short summary
Hydrologic controls on DOC, As and Pb export from a polluted peatland – the importance of heavy rain events, antecedent moisture conditions and hydrological connectivity
T. Broder and H. Biester
Biogeosciences, 12, 4651–4664, https://doi.org/10.5194/bg-12-4651-2015,https://doi.org/10.5194/bg-12-4651-2015, 2015
Short summary
Long-term trends at the Boknis Eck time series station (Baltic Sea), 1957–2013: does climate change counteract the decline in eutrophication?
S. T. Lennartz, A. Lehmann, J. Herrford, F. Malien, H.-P. Hansen, H. Biester, and H. W. Bange
Biogeosciences, 11, 6323–6339, https://doi.org/10.5194/bg-11-6323-2014,https://doi.org/10.5194/bg-11-6323-2014, 2014
Short summary
Comparison of different methods to determine the degree of peat decomposition in peat bogs
H. Biester, K.-H. Knorr, J. Schellekens, A. Basler, and Y.-M. Hermanns
Biogeosciences, 11, 2691–2707, https://doi.org/10.5194/bg-11-2691-2014,https://doi.org/10.5194/bg-11-2691-2014, 2014

Cited articles

Aksentov, K. I. and Sattarova, V. V.: Mercury geochemistry of deep-sea sediment cores from the Kuril area, northwest Pacific, Prog. Oceanogr., 180, 102235, https://doi.org/10.1016/j.pocean.2019.102235, 2020. 
Amos, H. M., Jacob, D. J., Streets, D. G., and Sunderland, E. M.: Legacy impacts of all-time anthropogenic emissions on the global mercury cycle, Global Biogeochem. Cy., 27, 410–421, https://doi.org/10.1002/gbc.20040, 2013. 
Amyot, M., Gill, G. A., and Morel, F. M. M.: Production and loss of dissolved gaseous mercury in coastal seawater, Environ. Sci. Technol., 31, 3606–3611, https://doi.org/10.1021/es9703685, 1997. 
Arrigo, K. R., Worthen, D., Schnell, A., and Lizotte, M. P.: Primary production in Southern Ocean waters, J. Geophys. Res.-Ocean., 103, 15587–15600, https://doi.org/10.1029/98JC00930, 1998. 
Canário, J., Santos-Echeandia, J., Padeiro, A., Amaro, E., Strass, V., Klaas, C., Hoppema, M., Ossebaar, S., Koch, B. P., and Laglera, L. M.: Mercury and methylmercury in the Atlantic sector of the Southern Ocean, Deep-Sea Res. Pt II, 138, 52–62, https://doi.org/10.1016/j.dsr2.2016.07.012, 2017. 
Download
Short summary
Mercury is a metal of environmental concern due to its toxic nature and its high potential for biomagnification. The role of oceans in the global mercury cycle is poorly understood. Investigation of biogenic sediments revealed that biological production and related scavenging of water-phase mercury by rapidly sinking algae or algae-derived organic matter after intense algae blooms controlled preindustrial mercury accumulation in Adélie Basin, East Antarctica.