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  4. Natural controls and anthropogenic impacts on organic carbon burial and remineralisation in fine-grained shelf sediments of the Helgoland Mud Area, North Sea
 
Zitierlink DOI
10.26092/elib/5828

Natural controls and anthropogenic impacts on organic carbon burial and remineralisation in fine-grained shelf sediments of the Helgoland Mud Area, North Sea

Veröffentlichungsdatum
2025-12-18
Autoren
Müller, Daniel
Betreuer
Kasten, Sabine  
Gutachter
Kasten, Sabine  
Diesing, Markus
Zusammenfassung
Since the industrial revolution, the global carbon cycle has significantly changed due to rising anthropogenic CO2 emissions from burning fossil fuels. Continental shelf sediments play a crucial role in the global carbon cycling. However, due to the dynamic nature of organic carbon-rich deposits, the mechanisms and quantities are yet not fully constrained. The North Sea is an ideal area to study the interplay between natural variability and anthropogenic impacts on organic carbon storage in shelf sediments, particularly in the Helgoland Mud Area (HMA), as the most important depot centre for fine-grained sediments in the German Bight of the North Sea. This thesis investigates the key factors influencing organic carbon burial and remineralisation in the HMA over space and time.
Key findings show organic carbon burial efficiency varied between 30 % and 78 %, primarily driven by high sedimentation rates and terrestrial organic carbon accumulation. Whereas high bottom-trawling activity seems to decrease organic carbon burial by approximately 30%.
In the HMA aerobic respiration is the most important pathway for organic carbon remineralisation, followed by sulphate reduction. Unexpectedly, the results show that various depositional parameters do not significantly influence the relative contributions of the different remineralisation pathways. Intensive bottom trawling was found to lower aerobic respiration contributions while enhancing sulphate reduction and total remineralisation.
Over the last millennium, major reductions in sedimentation and organic carbon accumulation rates of up to 93 % and 95 %, respectively, were found. The organic carbon storage capacity is estimated to have been reduced by 67 % in the HMA, due to changes in natural conditions and strong anthropogenic interventions in the shelf and coastal area, as well as in the catchment area of the rivers and waterway management.
Schlagwörter
Marine geochemistry

; 

(Bio-)geochemical processes

; 

Carbon cycle

; 

North Sea

; 

Reactive transport modeling
Institution
Universität Bremen  
Fachbereich
Fachbereich 05: Geowissenschaften (FB 05)  
Institute
Universität Bremen  
Forschungsdatenlink
https://doi.org/10.1594/PANGAEA.983802
https://doi.org/10.1594/PANGAEA.983806
https://doi.org/10.1594/PANGAEA.968969
https://doi.org/10.1594/PANGAEA.969033
https://doi.org/10.1594/PANGAEA.970325
Dokumenttyp
Dissertation
Lizenz
https://creativecommons.org/licenses/by/4.0/
Sprache
Englisch
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Natural controls and anthropogenic impacts on organic carbon burial and remineralisation in fine-grained shelf sediments of the Helgoland Mud Area, North Sea.pdf

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10.73 MB

Format

Adobe PDF

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