Abstract
Nitrogen (N) availability regulates primary productivity and hence directly affects global oceanic carbon sequestration. Global fjords account for up to 11% of marine carbon burial. However, N loss via sediment burial remains largely unquantified. Here, we show that global fjords are hotspots of N burial, accounting for up to 18% of oceanic N burial despite only covering 0.1% of the ocean area. Burial is the dominant N loss mechanism, exceeding microbial N loss via denitrification and anammox, which are generally considered the major N loss mechanisms. Microbial N loss dominates in anoxic fjords and appears to be a function of temperature and nutrient availability. Overall, fjords efficiently sequester excess N in sediments over long time scales. Accelerated warming will promote both N burial from increased primary production and microbial N loss from warmer temperatures, affecting N budgets in fjords and in the ocean in general.
| Original language | English |
|---|---|
| Article number | 3148 |
| Number of pages | 9 |
| Journal | Nature Communications |
| Volume | 17 |
| DOIs | |
| Publication status | Published - 1 Apr 2026 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
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SDG 14 Life Below Water
Keywords
- Fjords
- Nitrogen
- Loss
- Sediment
- Water column
- Seabed
- Coastal
- O2 depletion
- Oxygen
- Burial
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Dataset and Markdown codes for article "Long-term nitrogen burial exceeds denitrification in global fjords"
Cheung, H. L. (Creator), Levin, L. (Creator), Smeaton, C. (Creator), Politi, T. (Creator), Thamdrup, B. (Creator), Santos, I. (Creator) & Bonaglia, S. (Creator), Zenodo, 5 Mar 2026
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