From fresh to marine waters: characterization and fate of dissolved organic matter in the Lena River delta region, Siberia

• Published in: Frontiers in Marine Science
• Main Authors: Rafael eGonçalves-Araujo, Colin Andrew Stedmon, Birgit eHeim, Ivan eDubinenkov, Alexandra eKraberg, Denis eMoiseev, Astrid eBracher
• Format: Article in Journal/Newspaper
• Language: English
• Published: Frontiers Media S.A. 2015
• Subjects: Arctic; DOC; parafac; CDOM; Hydrography; optical indices; Science; Q; General. Including nature conservation; geographical distribution; QH1-199.5; Laptev Sea; Climate change; laptev; lena delta; lena river; Siberia
• Online Access: https://doi.org/10.3389/fmars.2015.00108; https://doaj.org/article/675b3c6e6181414fb60a15f539cce7f8

Connectivity between the terrestrial and marine environment in the Artic is changing as a result of climate change, influencing both freshwater budgets and the supply of carbon to the sea. This study characterizes the optical properties of dissolved organic matter (DOM) within the Lena Delta region and evaluates the behavior of DOM across the fresh water-marine gradient. Six fluorescent components (four humic-like; one marine humic-like; one protein-like) were identified by Parallel Factor Analysis (PARAFAC) with a clear dominance of allochthonous humic-like signals. Colored DOM (CDOM) and dissolved organic carbon (DOC) were highly correlated and had their distribution coupled with hydrographical conditions. Higher DOM concentration and degree of humification were associated with the low salinity waters of the Lena River. Values decreased towards the higher salinity Laptev Sea shelf waters. Results demonstrate different responses of DOM mixing in relation to the vertical structure of the water column, as reflecting the hydrographical dynamics in the region. Two mixing curves for DOM were apparent. In surface waters above the pycnocline there was a sharper decrease in DOM concentration in relation to salinity indicating removal. In the bottom water layer the DOM decrease within salinity was less. We propose there is a removal of DOM occurring primarily at the surface layer, which is likely driven by photodegradation and flocculation.