open access publication

Article, 2023

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

LIMNOLOGY AND OCEANOGRAPHY, ISSN 0024-3590, 0024-3590, Volume 68, 3, Pages 631-648, 10.1002/lno.12299

Contributors

Leiva-Duenas, Carmen 0000-0001-8974-9883 (Corresponding author) [1] Graversen, Anna Elizabeth Lovgren 0000-0003-4116-0054 [1] Banta, Gary 0000-0002-3000-9837 [2] Holmer, M. 0000-0002-6095-5488 [2] Masque, Pere 0000-0002-1789-320X [3] [4] [5] Staehr, Peter 0000-0002-1580-4875 [1] Krause-Jensen, D. 0000-0001-9792-256X [1]

Affiliations

  1. [1] Aarhus Univ, Dept Ecosci, Aarhus C, Denmark
  2. [NORA names: AU Aarhus University; University; Denmark; Europe, EU; Nordic; OECD];
  3. [2] Univ Southern Denmark, Dept Biol, Odense M, Denmark
  4. [NORA names: SDU University of Southern Denmark; University; Denmark; Europe, EU; Nordic; OECD];
  5. [3] Univ Autonoma Barcelona, Inst Ciencia & Tecnol Ambientals, Dept Fis, Bellaterra, Spain
  6. [NORA names: Spain; Europe, EU; OECD];
  7. [4] Edith Cowan Univ, Ctr Marine Ecosyst Res, Joondalup, WA, Australia
  8. [NORA names: Australia; Oceania; OECD];
  9. [5] IAEA, Marine Environm Labs, Principality Of Monaco, Monaco
  10. [NORA names: Monaco; Europe, Non-EU]

Abstract

The ability of seagrass meadows to filter nutrients and capture and store CO2 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 Pb-210 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 Pb-210, 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 CO2 emissions and 6.9% +/- 5.2% of the total terrestrial N load.

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