Sources of Dissolved Organic Carbon in Rivers of the Yenisei River Basin


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Abstract

The spatial and temporal variations in concentrations of dissolved organic carbon in the Yenisei River and its major tributaries are analyzed. The results obtained suggest that the maximal contribution to the flows of dissolved organic carbon in the Yenisei River is made by cryohydromorphic forest landscapes of the Central Siberian Plateau.

About the authors

A. S. Prokushkin

Sukachev Institute of Forestry, Siberian Branch; Siberian Federal University

Author for correspondence.
Email: prokushkin@ksc.krasn.ru
Russian Federation, Krasnoyarsk, 660036; Krasnoyarsk, 660041

O. S. Pokrovsky

Géosciences Environment Toulouse, Centre national de la recherché scientifique

Email: prokushkin@ksc.krasn.ru
France, Toulouse, 31400

M. A. Korets

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
Russian Federation, Krasnoyarsk, 660036

A. V. Rubtsov

Sukachev Institute of Forestry, Siberian Branch; Siberian Federal University

Email: prokushkin@ksc.krasn.ru
Russian Federation, Krasnoyarsk, 660036; Krasnoyarsk, 660041

S. V. Titov

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
Russian Federation, Krasnoyarsk, 660036

I. V. Tokareva

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
Russian Federation, Krasnoyarsk, 660036

R. A. Kolosov

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
Russian Federation, Krasnoyarsk, 660036

R. M. W. Amon

Texas Agriculture and Mechanical University at Galveston

Email: prokushkin@ksc.krasn.ru
United States, Galveston, Texas, 77553


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