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Updated: Feb 13, 2026

Understanding Dissolved Organic Matter Biogeochemistry Through In Situ Nutrient Manipulations in Stream Ecosystems
Published on: October 29, 2016
Terrestrial dissolved organic matter distribution in the North Sea
Stuart C Painter1, Dan J Lapworth2, E Malcolm S Woodward3
1National Oceanography Centre, Southampton, UK.
Terrestrial dissolved organic matter (tDOM) largely remains in the North Sea, with minimal transfer to the Atlantic Ocean. Most tDOM is buried or remineralized internally, impacting the global carbon cycle.
Area of Science:
- Environmental Science
- Oceanography
- Biogeochemistry
Background:
- Terrestrial carbon flow to aquatic systems is crucial for the global carbon cycle.
- The efficiency of terrestrial organic carbon transfer through coastal filters to the ocean is unknown.
- Understanding this flux is vital for assessing the role of terrestrial carbon in climate regulation.
Purpose of the Study:
- To investigate the spatial distribution of terrestrial dissolved organic matter (tDOM) in the North Sea.
- To test the hypothesis of quantitative tDOM transfer from the North Sea to the North Atlantic.
- To identify sources and pathways of tDOM within the North Sea.
Main Methods:
- Utilized fluorescent and chromophoric dissolved organic matter (FDOM and CDOM) as proxies for tDOM.
- Employed excitation emission matrix fluorescence and parallel factor analysis (EEM-PARAFAC).
- Analyzed spatial distribution and salinity relationships of FDOM and CDOM.
Main Results:
- Identified a single terrestrial humic-like FDOM class, primarily in coastal areas and linked to riverine inputs.
- Detected two distinct sources of fluorescent humic-like material from major river outflows and the Baltic Sea.
- Found insignificant tDOM flux from the North Sea to the Atlantic, with potential export via unsampled Norwegian waters.
Conclusions:
- The majority of tDOM from Northwest Europe and Scandinavia is buried or remineralized within estuarine and coastal systems.
- Residence time in these systems significantly controls tDOM fate and atmospheric carbon loss.
- Current models may overestimate the oceanic storage of terrestrial carbon due to limited transfer efficiency.
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