Articles | Volume 13, issue 1
Biogeosciences, 13, 147–157, 2016
https://doi.org/10.5194/bg-13-147-2016
Biogeosciences, 13, 147–157, 2016
https://doi.org/10.5194/bg-13-147-2016

Research article 15 Jan 2016

Research article | 15 Jan 2016

Insights into the transfer of silicon isotopes into the sediment record

V. N. Panizzo et al.

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Cited articles

Alleman, L. Y., Cardinal, D., Cocquyt, C., Plisnier, P. D., Descy, J. P., Kimirei, I., Sinyinza, D., and Andre, L.: Silicon isotopic fractionation in Lake Tanganyika and its main tributaries, J. Great Lakes Res., 31, 509–519, 2005.
Appleby, P. G. and Oldfield, F.: The calculation of 210Pb dates assuming a constant rate of supply of unsupported 210Pb to the sediment, Catena, 5, 1–8, 1978.
Atlas Baikalia: “Siberia” Program Interdepartmental Scientific Committee of the SB RAS, Federal'naya Sluzhba Geodezii i Kartografii Rossii, Moscow, 1993 (in Russian).
Battarbee, R. W., Anderson, N. J., Jeppesen, E., and Leavitt, P. R.: Combining palaeolimnological and limnological approaches in assessing lake ecosystem response to nutrient reduction, Freshwater Biol., 50, 1772–1780, 2005.
Cardinal, D., Alleman, L. Y., de Jong, J., Ziegler, K., and Andre, L.: Isotopic composition of silicon measured by multicollector plasma source mass spectrometry in dry plasma mode, J. Anal. Atom. Spectrom., 18, 213–218, 2003.
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Short summary
Lake Baikal, Siberia, is the world's most voluminous lake. Diatoms are the most dominant primary producers in the lake and form the basis of the food chain. This paper investigated the productivity of these organisms over the course of a year with a view to understanding their preservation in sediments and their value for reconstructing past productivity in the lake. This is important when recent climate change and the pressures of pollution are having demonstrable impacts in the region.
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