Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/36209
Appears in Collections:Biological and Environmental Sciences eTheses
Title: Source-to-Sea: The Transport and Storage of Organic Carbon and Iron from Forested Environments to (Fjord) Sediments
Author(s): Kellock, Celeste C I
Supervisor(s): Schrӧder, Christian
Smeaton, Craig
Shah, Nadeem
Jump, Alistair
Keywords: Organic carbon
organic carbon burial
reactive iron
source-to-sea
carbon transport
carbon geochemistry
iron geochemistry
carbon burial in fjord sediments
iron and carbon associations
ferrihydrite
biomarkers
Issue Date: 19-Apr-2024
Publisher: University of Stirling
Abstract: Fjords are globally important carbon stores due to their ability to store carbon long-term. However, the source of organic carbon and the influence of catchment processes and land cover on sedimentary carbon storage is poorly understood. This impacts our ability to effectively protect and manage dynamic coastal environments. Globally, ~ 20 % of organic carbon (OC) stored in sediment is directly bound to reactive iron (FeR). In this study, I explore the role of OC-FeR associations on the preservation and storage of OC in catchment and sediments of a mid-latitude Scottish fjord, Loch Creran. On average 37 % of OC was bound to FeR in forested catchment soils, 41 % in freshwater sediments, and ~16 % in fjord sediments. Ferrihydrite was found to be the dominant species of iron throughout the catchment and sediments, indicating that some OC-FeR complexes may travel from source (upstream and surrounding terrestrial environments) to fjord sediments without extensive reworking. On average, 47 – 67 % of OC in fjord sediments originated from terrestrial sources, identified from Bayesian modelling, and this was further explored using n-alkanes, specific δ¹³C isotopic signatures and pine resins. Methyl dehydroabietate (pine resin) was able to capture the presence of coniferous material where n-alkane abundance and isotopes could not. Furthermore, biomarkers were stored effectively in fjord sediments over long time periods, showing little degradation of either proxy downcore. Through conducting a source to sea study and utilising biogeochemical information across vegetation, soils, rivers and sediments, I was able to create a better understanding of the mechanisms that promote lateral carbon movement and the chemical changes that carbon complexes can withstand. I demonstrate that in mid-latitude fjords OC-FeR complexes play an important role in biogeochemical cycling, OC storage in forest soils, and OC transport and storage from source towards sea.
Type: Thesis or Dissertation
URI: http://hdl.handle.net/1893/36209

Files in This Item:
File Description SizeFormat 
CelesteKellock_FinalThesis.pdfCeleste Kellock - PhD Thesis7.54 MBAdobe PDFUnder Embargo until 2026-09-20    Request a copy

Note: If any of the files in this item are currently embargoed, you can request a copy directly from the author by clicking the padlock icon above. However, this facility is dependent on the depositor still being contactable at their original email address.



This item is protected by original copyright



Items in the Repository are protected by copyright, with all rights reserved, unless otherwise indicated.

The metadata of the records in the Repository are available under the CC0 public domain dedication: No Rights Reserved https://creativecommons.org/publicdomain/zero/1.0/

If you believe that any material held in STORRE infringes copyright, please contact library@stir.ac.uk providing details and we will remove the Work from public display in STORRE and investigate your claim.