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Autor:
Olga Yu. Drozdova, Oleg S. Pokrovsky, Olga V. Oleinikova, Sergey A. Lapitskiy, Andrey Yu. Bychkov, Emmanuele Gérard, Liudmila S. Shirokova
Publikováno v:
Geochimica et Cosmochimica Acta. 205:313-330
Bacterial mineralization of allochthonous (soil) dissolved organic matter (DOM) in boreal waters governs the CO 2 flux from the lakes and rivers to the atmosphere, which is one of the main factor of carbon balance in high latitudes. However, the fate