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Long-term nitrogen burial exceeds denitrification in global fjords

Henry L. S. Cheung*, Lubrina S. Levin, Craig Smeaton, Tobia Politi, Bo Thamdrup, Isaac R. Santos, Stefano Bonaglia

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

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 languageEnglish
Article number3148
Number of pages9
JournalNature Communications
Volume17
DOIs
Publication statusPublished - 1 Apr 2026

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

  1. SDG 13 - Climate Action
    SDG 13 Climate Action
  2. SDG 14 - Life Below Water
    SDG 14 Life Below Water

Keywords

  • Fjords
  • Nitrogen
  • Loss
  • Sediment
  • Water column
  • Seabed
  • Coastal
  • O2 depletion
  • Oxygen
  • Burial

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