Reduction of carbon, alkalinity and nutrient fluxes in the southern Baltic Sea caused by dragging of otter trawl nets across the seafloor

Abstract. Mobile bottom-contacting fishing (MBCF) represents a substantial anthropogenic disturbance, significantly disrupting seafloor integrity and altering oceanic carbon storage. In this study, we conducted a benthic trawling experiment on organic-rich muddy sediments in the Mecklenburger Bight, southern Baltic Sea, employing an otter trawl. Multiple trawl tracks were made to assess the temporal impact of bottom fishing on the benthic ecosystem over time scales ranging from days to weeks. Focus was on the wide area where the net footrope was dragged between the otter boards, rather than on much smaller area impacted by the trawl doors. This study constitutes the first comprehensive investigation to systematically monitor the effects of MBCF on benthic oxygen, carbon, alkalinity and nutrient fluxes using autonomous in situ lander measurements. Seafloor observations revealed a profound impact of trawling on seafloor morphology. Flux measurements, coupled with sediment data, indicated reductions in benthic fluxes of O2, dissolved inorganic carbon (DIC), total alkalinity (TA), and nutrients (PO4-3, NH4+, and H4SiO4) within trawled areas compared to control sites. Additionally, observed decreases in organic carbon remineralization rates suggest that MBCF alters benthic respiration by disrupting key biogeochemical processes. Fluxes of O2, DIC, and TA had not returned to baseline levels by the conclusion of the 16 d observation period, indicating prolonged disturbance effects, although natural temporal variations may have an influence. Despite substantial alterations to the benthic biogeochemical pathways, modeling suggests that the reduction in benthic DIC and TA fluxes exerts only a minor influence on CO2 release to the atmosphere compared to the potential impact of pyrite oxidation in resuspended sediment.

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Publication Details

Journal
Biogeosciences
Published
2025-11-13
DOI
https://doi.org/10.5194/bg-22-6727-2025
Primary Topic
Marine and fisheries research
Type
article
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article

Reduction of carbon, alkalinity and nutrient fluxes in the southern Baltic Sea caused by dragging of otter trawl nets across the seafloor

Jens Kallmeyer, Andrew W. Dale, Florian Scholz, P. Linsy et al.
Biogeosciences
Marine and fisheries research
article

Reduction of carbon, alkalinity and nutrient fluxes in the southern Baltic Sea caused by dragging of otter trawl nets across the seafloor

Jens Kallmeyer, Andrew W. Dale, Florian Scholz, P. Linsy, Habeeb Thanveer Kalapurakkal, Stefan Sommer, Simone Bernsee
article en

Abstract

Abstract. Mobile bottom-contacting fishing (MBCF) represents a substantial anthropogenic disturbance, significantly disrupting seafloor integrity and altering oceanic carbon storage. In this study, we conducted a benthic trawling experiment on organic-rich muddy sediments in the Mecklenburger Bight, southern Baltic Sea, employing an otter trawl. Multiple trawl tracks were made to assess the temporal impact of bottom fishing on the benthic ecosystem over time scales ranging from days to weeks. Focus was on the wide area where the net footrope was dragged between the otter boards, rather than on much smaller area impacted by the trawl doors. This study constitutes the first comprehensive investigation to systematically monitor the effects of MBCF on benthic oxygen, carbon, alkalinity and nutrient fluxes using autonomous in situ lander measurements. Seafloor observations revealed a profound impact of trawling on seafloor morphology. Flux measurements, coupled with sediment data, indicated reductions in benthic fluxes of O2, dissolved inorganic carbon (DIC), total alkalinity (TA), and nutrients (PO4-3, NH4+, and H4SiO4) within trawled areas compared to control sites. Additionally, observed decreases in organic carbon remineralization rates suggest that MBCF alters benthic respiration by disrupting key biogeochemical processes. Fluxes of O2, DIC, and TA had not returned to baseline levels by the conclusion of the 16 d observation period, indicating prolonged disturbance effects, although natural temporal variations may have an influence. Despite substantial alterations to the benthic biogeochemical pathways, modeling suggests that the reduction in benthic DIC and TA fluxes exerts only a minor influence on CO2 release to the atmosphere compared to the potential impact of pyrite oxidation in resuspended sediment.

BiogeosciencesVol. 22(21)
Openalex Percentile: Top 68%
Marine and fisheries research
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