Preprints
https://doi.org/10.5194/egusphere-2026-3315
https://doi.org/10.5194/egusphere-2026-3315
19 Jun 2026
 | 19 Jun 2026
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Lateral Transport Controls Particulate Organic Carbon Stocks and Fluxes in the Baltic Sea

Lucas Porz, Jan Kossack, David Pogorzelski, and Wenyan Zhang

Abstract. The sediments of the Baltic Sea represent a substantial regional carbon sink. Yet, detailed mapping of organic carbon (OC) content and stock in the Baltic Sea is lacking, and our understanding of the transport pathways of particulate OC (POC) in the water column is limited. Here, we generate high-resolution (500×500 m) maps of surface OC content from available data using a deep neural network. The results are combined with porosity and Holocene sediment thickness maps to derive OC stocks per maritime zone of each Baltic Sea country. The total surface (top 10 cm) OC stock is estimated to 1.29 ± 0.36 GtC and the spatially averaged surface stock to 3.14 ± 0.86 kgC m-2. A process-based, 3D numerical model is then used to simulate fluxes of resuspended POC. The results imply that horizontal transport of resuspended POC, rather than in-situ biological production, is the key factor determining the flux and distribution of sediment OC. Net horizontal transport of resuspended POC across maritime boundaries reaches the order of 1 MtC yr-1, with substantial interannual variability. These fluxes are in the same magnitude as the recent net OC accumulation rate, underscoring the importance of laterally derived, allochthonous carbon in sedimentary Blue Carbon habitats. Regional numerical modelling may be useful in addressing the issues of double counting and additionality in Blue Carbon accounting and management.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
Share
Lucas Porz, Jan Kossack, David Pogorzelski, and Wenyan Zhang

Status: open (until 31 Jul 2026)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
Lucas Porz, Jan Kossack, David Pogorzelski, and Wenyan Zhang
Lucas Porz, Jan Kossack, David Pogorzelski, and Wenyan Zhang
Metrics will be available soon.
Latest update: 19 Jun 2026
Download
Short summary
As a major part of coastal “Blue Carbon” ecosystems, the seabed stores carbon originating from atmospheric CO2, especially where natural depressions trap sediment, such as in the Baltic Sea. Here, the amount of carbon stored in the surface of the seafloor is estimated to 1.3 billion tonnes. Computer simulations show that ocean currents transport a large amount of carbon-rich particles across maritime boundaries. These findings may be useful in making Blue Carbon accounting more robust.
Share