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Date of Award
Summer 2025
Document Type
Masters Thesis
Department or Program Affiliation
Geology
Degree Name
Master of Science (MS)
Department
Geology
First Advisor
Ponton, Camilo
Second Advisor
Housen, Bernard Arthur
Third Advisor
Foreman, Brady
Abstract
Terrestrial organic carbon (OC) is transported by rivers to continental margins and eventually deposited on the ocean floor by turbidity currents. Plant and wood fragments have been found to contribute significantly to the carbon load deposited on river-dominated continental margins, but carbon quantification is often exclusively performed on the fine-grained particles (< 2mm) excluding the coarse particulate fractions (> 2mm). Turbidites samples from the Nitinat Fan in the Cascadia Basin within the Pacific Northwest were analyzed to quantify OC, determine OC sourcing, and characterize “sedimentary wood” using stable carbon isotope ratios and Raman microscopy.
The results from this research show that OC sourcing in the Nitinat Fan is mostly from terrestrial C3 vascular vegetation based on carbon isotopes and C:N ratios. In some wood-containing sedimentary layers, more than 90% of the carbon is stored as woody debris rather than dispersed organic carbon. On average, coarse (>2mm) woody debris have a higher carbon content (60%) than finer (< 2mm) woody debris (40%) and therefore contributes more to bulk organic carbon (OCbulk ), 77% vs. 23% respectively. Sedimentary layers that incorporate wood were found to contain 6 times more carbon than regular fan sediment suggesting previous studies may have underestimated carbon storage in the ocean sink.
Raman microscopy was used to characterize woody debris (sedimentary wood), but while initial applications proved to be challenging for sedimentary wood samples that are degraded, the method was efficient at determining wood type (angiosperm vs. gymnosperm) and sometimes offer identification at the species level, when the wood is unaltered.
Type
Text
Keywords
Submarine fans, turbidity currents, turbidites, terrestrial organic carbon, wood fragments, Raman microscopy, ocean carbon sink
Publisher
Western Washington University
OCLC Number
1524901934
Subject – LCSH
Submarine fans--Northwest, Pacific; Water--Organic compound content--Northwest, Pacific; Carbon--Environmental aspects--Northwest, Pacific; Wood--Biodegradation--Northwest, Pacific; Marine sediments--Northwest, Pacific--Analysis; Sedimentation and deposition--Northwest, Pacific; Carbon sequestration--Northwest, Pacific; Turbidites--Northwest, Pacific; Turbidity currents
Geographic Coverage
Northwest, Pacific; Cascadia Subduction Zone
Format
application/pdf
Genre/Form
masters theses
Language
English
Rights
Copying of this document in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this document for commercial purposes, or for financial gain, shall not be allowed without the author’s written permission.
Recommended Citation
Okedoyin, Omololu Eunice, "Quantifying the carbon storage potential of submarine fans: an example from the Nitinat Fan in the Cascadia Margin" (2025). WWU Graduate School Collection. 1413.
https://cedar.wwu.edu/wwuet/1413