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- Ogneva, Olga, et al.
(författare)
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Particulate organic matter in the Lena River and its delta : from thepermafrost catchment to the Arctic Ocean
- 2023
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Ingår i: Biogeosciences. - 1726-4170 .- 1726-4189. ; 20:7, s. 1423-1441
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Tidskriftsartikel (refereegranskat)abstract
- Rapid Arctic warming accelerates permafrost thaw, causing an additional release of terrestrial organic matter (OM) into rivers and, ultimately, after transport via deltas and estuaries, to the Arctic Ocean nearshore. The majority of our understanding of nearshore OM dynamics and fate has been developed from freshwater rivers despite the likely impact of highly dynamic estuarine and deltaic environments on the transformation, storage, and age of OM delivered to coastal waters. Here, we studied particulate organic carbon (POC) dynamics in the Lena River delta and compared them with POC dynamics in the Lena River main stem along a similar to 1600 km long transect from Yakutsk, downstream to the delta. We measured POC, total suspended matter (TSM), and carbon isotopes (delta C-13 and Delta C-14) in POC to compare riverine and deltaic OM composition and changes in OM source and fate during transport offshore. We found that TSM and POC concentrations decreased by 70% during transit from the main stem to the delta and Arctic Ocean. We found deltaic POC to be strongly depleted in C-13 relative to fluvial POC. Dual-carbon (Delta C-14 and delta C-13) isotope mixing model analyses indicated a significant phytoplankton contribution to deltaic POC (similar to 68 +/- 6 %) and suggested an additional input of permafrost-derived OM into deltaic waters (similar to 18 +/- 4% of deltaic POC originates from Pleistocene deposits vs. similar to 5 +/- 4% in the river main stem). Despite the lower concentration of POC in the delta than in the main stem (0.41 +/- 0.10 vs. 0.79 +/- 0.30 mg L-1, respectively), the amount of POC derived from Yedoma deposits in deltaic waters was almost twice as large as the amount of POC of Yedoma origin in the main stem (0.07 +/- 0.02 and 0.04 +/- 0.02 mg L-1, respectively). We assert that estuarine and deltaic processes require consideration in order to correctly understand OM dynamics throughout Arctic nearshore coastal zones and how these processes may evolve under future climate-driven change.
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| 2. |
- Sanders, Tina, et al.
(författare)
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Seasonal nitrogen fluxes of the Lena River Delta
- 2022
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Ingår i: Ambio. - : Springer Science and Business Media LLC. - 0044-7447 .- 1654-7209. ; 51:2, s. 423-438
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Tidskriftsartikel (refereegranskat)abstract
- The Arctic is nutrient limited, particularly by nitrogen, and is impacted by anthropogenic global warming which occurs approximately twice as fast compared to the global average. Arctic warming intensifies thawing of permafrost-affected soils releasing their large organic nitrogen reservoir. This organic nitrogen reaches hydrological systems, is remineralized to reactive inorganic nitrogen, and is transported to the Arctic Ocean via large rivers. We estimate the load of nitrogen supplied from terrestrial sources into the Arctic Ocean by sampling in the Lena River and its Delta. We took water samples along one of the major deltaic channels in winter and summer in 2019 and sampling station in the central delta over a one-year cycle. Additionally, we investigate the potential release of reactive nitrogen, including nitrous oxide from soils in the Delta. We found that the Lena transported nitrogen as dissolved organic nitrogen to the coastal Arctic Ocean and that eroded soils are sources of reactive inorganic nitrogen such as ammonium and nitrate. The Lena and the Deltaic region apparently are considerable sources of nitrogen to nearshore coastal zone. The potential higher availability of inorganic nitrogen might be a source to enhance nitrous oxide emissions from terrestrial and aquatic sources to the atmosphere.
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