Articles | Volume 12, issue 10
https://doi.org/10.5194/bg-12-3009-2015
https://doi.org/10.5194/bg-12-3009-2015
Research article
 | 
21 May 2015
Research article |  | 21 May 2015

Seasonal dynamics of organic carbon and metals in thermokarst lakes from the discontinuous permafrost zone of western Siberia

R. M. Manasypov, S. N. Vorobyev, S. V. Loiko, I. V. Kritzkov, L. S. Shirokova, V. P. Shevchenko, S. N. Kirpotin, S. P. Kulizhsky, L. G. Kolesnichenko, V. A. Zemtzov, V. V. Sinkinov, and O. S. Pokrovsky

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Cited articles

Audry, S., Pokrovsky, O. S., Shirokova, L. S., Kirpotin, S. N., and Dupré, B.: Organic matter mineralization and trace element post-depositional redistribution in Western Siberia thermokarst lake sediments, Biogeosciences, 8, 3341–3358, https://doi.org/10.5194/bg-8-3341-2011, 2011.
Avagyan, A., Runkle, B. R. K., and Kutzbach, L.: Application of high-resolution spectral absorbance measurements to determine dissolved organic carbon concentration in remote areas, J. Hydrol., 517, 435–446, 2014.
Benedetti, M. F., Milne, C., Kinniburgh, D., van Riemsdijk, W., and Koopal, L.: Metal ion binding to humic substances: Application of the non ideal competitive adsorption model, Environ. Sci. Technol., 29, 446–457, 1995.
Berg, B.: Litter decomposition and organic matter turnover in northern forest soils, Forest Ecol. Manag., 133, 13–22, 2000.
Boike, J., Kattenstroth, B., Abramova, K., Bornemann, N., Chetverova, A., Fedorova, I., Fröb, K., Grigoriev, M., Grüber, M., Kutzbach, L., Langer, M., Minke, M., Muster, S., Piel, K., Pfeiffer, E.-M., Stoof, G., Westermann, S., Wischnewski, K., Wille, C., and Hubberten, H.-W.: Baseline characteristics of climate, permafrost and land cover from a new permafrost observatory in the Lena River Delta, Siberia (1998–2011), Biogeosciences, 10, 2105–2128, https://doi.org/10.5194/bg-10-2105-2013, 2013.
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Short summary
A year-around hydrochemical study (including full winter freezing and spring flood) of shallow thermokarst lakes from a discontinuous permafrost zone of western Siberia revealed conceptually new features of element concentration evolution over different seasons within a large scale of the lake size.
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