open access publication

Article, 2023

Capturing of organic carbon and nitrogen in eelgrass sediments of southern Scandinavia

Limnology and Oceanography, ISSN 1939-5590, 0024-3590, Volume 68, 3, Pages 631-648, 10.1002/lno.12299

Contributors

Leiva-Dueñas, Carmen 0000-0001-8974-9883 (Corresponding author) [1] Graversen, Anna Elizabeth Løvgren 0000-0003-4116-0054 [1] Banta, Gary Thomas 0000-0002-3000-9837 [2] Holmer, Marianne 0000-0002-6095-5488 [2] Masqué, Pere 0000-0002-1789-320X [3] [4] [5] Staehr, Peter Anton Upadhyay 0000-0002-1580-4875 [1] Krause-Jensen, Dorte Søndergaard 0000-0001-9792-256X [1]

Affiliations

  1. [1] Aarhus University
  2. [NORA names: AU Aarhus University; University; Denmark; Europe, EU; Nordic; OECD];
  3. [2] University of Southern Denmark
  4. [NORA names: SDU University of Southern Denmark; University; Denmark; Europe, EU; Nordic; OECD];
  5. [3] Autonomous University of Barcelona
  6. [NORA names: Spain; Europe, EU; OECD];
  7. [4] Edith Cowan University
  8. [NORA names: Australia; Oceania; OECD];
  9. [5] International Atomic Energy Agency, Marine Environmental Laboratories, Principality of Monaco, Monaco
  10. [NORA names: Monaco; Europe, Non-EU]

Abstract

Abstract The ability of seagrass meadows to filter nutrients and capture and store CO 2 and nutrients in the form of organic carbon (OC) and nitrogen (N) in their sediments may help to mitigate local eutrophication as well as climate change via meadow restoration and protection. This study assesses OC and N sediment stocks (top 50 cm) and sequestration rates within Danish eelgrass meadows. At four locations, eelgrass‐vegetated and nearby unvegetated plots were studied in protected and exposed areas. The average OC and N sediment 50 cm stocks were 2.6 ± 0.3 kg OC m −2 and 0.23 ± 0.01 kg N m −2 , including vegetated and unvegetated plots. In general, OC and N stocks did not differ significantly between eelgrass meadows and unvegetated sediments. Lack of accumulation of excess 210 Pb suggested sediment erosion or low rates of sediment accumulation at most sites. OC accumulation rates ranged from 6 to 134 g m −2  yr −1 and N from 0.7 to 14 g m −2  yr −1 . Generalized additive models showed that ≥ 80% of the variation in sediment OC and N stocks was explained by sediment grain size, organic matter source, and hydrodynamic exposure. Long cores, dated with 210 Pb, showed declining OC and N densities toward present time, suggesting long‐term declines in eelgrass OC and N pools. Estimates of potential nation‐wide OC and N accumulation in eelgrass sediments show that they could annually capture up to 0.7% ± 0.5% of CO 2 emissions and 6.9% ± 5.2% of the total terrestrial N load.

Keywords

CO 2, CO 2 emissions, N accumulation, N density, N loading, N pools, N stocks, OC accumulation rates, Pb, Scandinavia, accumulation, accumulation of excess, accumulation rates, additive model, area, average OC, carbon, changes, climate, climate change, core, decline, eelgrass, eelgrass meadows, eelgrass sediments, erosion, estimation, eutrophication, excess, exposed areas, exposure, filtering nutrients, generalized additive model, grain size, hydrodynamic exposure, lack, local eutrophication, location, long core, long-term decline, low rate, low rates of sediment accumulation, matter sources, meadow restoration, meadows, model, nitrogen, nitrogen (N, nutrients, organic carbon, organic matter sources, plots, protection, rate, rates of sediment accumulation, restoration, seagrass, seagrass meadows, sediment OC, sediment accumulation, sediment erosion, sediment grain size, sediments, sequestration, sequestration rate, sites, size, source, southern Scandinavia, stock, study, unvegetated plots, unvegetated sediments, variation

Funders

  • Australian Research Council
  • The Velux Foundations

Data Provider: Digital Science