https://vital.lib.tsu.ru/vital/access/manager/Index en-us 5 https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001015842 Tue 19 Dec 2023 10:04:38 KRAT ]]> https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000996391 Tue 14 Feb 2023 15:56:34 KRAT ]]> https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000996394 Tue 14 Feb 2023 15:49:40 KRAT ]]> https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001008913 99.5% C-CO2, <0.5% C-CH4) which is twice higher than the total dissolved C (organic and inorganic) riverine export flux during the same period. Applying a “substituting space for time” approach for northern and southern parts of the river basin, we suggest that the current riverine CO2 emission may increase 2 to 3 fold in the next decades due to on-going climate warming and permafrost thaw. When integrating the obtained results into global models of C and biogeochemical cycle in the Arctic and subarctic region, the use of the Taz River as a representative example of continental planes should help to estimate the consequences of frozen peatland thaw on CO2 cycle in the Arctic and subarctic regions.]]> Thu 09 Nov 2023 09:56:02 KRAT ]]> https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:001008914 Thu 09 Nov 2023 09:55:56 KRAT ]]>