Articles | Volume 14, issue 7
Biogeosciences, 14, 1811–1823, 2017
https://doi.org/10.5194/bg-14-1811-2017

Special issue: Climate–carbon–cryosphere interactions in the...

Biogeosciences, 14, 1811–1823, 2017
https://doi.org/10.5194/bg-14-1811-2017

Research article 05 Apr 2017

Research article | 05 Apr 2017

Export of calcium carbonate corrosive waters from the East Siberian Sea

Leif G. Anderson et al.

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Cited articles

Alling, V., Porcelli, D., Mörth, C.-M., Anderson, L. G., Sanchez-Garcia, L., Gustafsson, Ö., Andersson, P. S., and Humborg, C.: Degradation of terrestrial organic carbon, primary production and out-gassing of CO2 along the Laptev and East Siberian Seas as inferred from δ13C values of DIC, Geochim. Cosmochim. Ac., 95, 143–159, 2012.
Anderson, L. G., Björk, G., Holby, O., Kattner, G., Koltermann, P. K., Jones, E. P., Liljeblad, B., Lindegren, R., Rudels, B., and Swift, J.: Water Masses and Circulation in the Eurasian Basin: Results from the Oden 91 North Pole Expedition, J. Geophys. Res., 99, 3273–3283, 1994.
Anderson, L. G., Jutterström, S., Kaltin, S., Jones, E. P., and Björk, G.: Variability in river runoff distribution in the Eurasian Basin of the Arctic Ocean, J. Geophys. Res., 109, C01016, https://doi.org/10.1029/2003JC001773, 2004.
Anderson, L. G., Jutterström, S., Hjalmarsson, S., Wåhlström, I., and Semiletov, I. P.: Out-gassing of CO2 from Siberian Shelf Seas by terrestrial organic matter decomposition, Geophys. Res. Lett., 36, L20601, https://doi.org/10.1029/2009GL040046, 2009.
Anderson, L. G., Tanhua, T., Björk, G., Hjalmarsson, S., Jones, E. P., Jutterström, S., Rudels, B., Swift, J. H., and Wåhlström, I.: Arctic Ocean shelf – basin interaction, an active continental shelf CO2 pump and its impact on the degree of calcium carbonate dissolution, Deep-Sea Res. Pt. I, 57, 869–879 https://doi.org/10.1016/j.dsr.2010.03.012, 2010.
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Waters with very high pCO2, nutrients and low oxygen concentrations were observed along the continental margin of the East Siberian Sea and well out into the deep Makarov and Canada basins during the SWERUS-C3 expedition in 2014. This water had a low saturation state with respect to calcium carbonate, down to less than 0.8 for calcite and 0.5 for aragonite, and is traced in historic data to the Canada Basin and in the waters flowing out of the Arctic Ocean in the western Fram Strait.
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