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Date of Award
Summer 2024
Document Type
Masters Thesis
Department or Program Affiliation
Geology
Degree Name
Master of Science (MS)
Department
Geology
First Advisor
Ponton, Camilo
Second Advisor
Pfeiffer, Allison
Third Advisor
Love, Brooke
Abstract
The dynamics of the Cordilleran Ice Sheet (CIS) over the last glacial period are complex, with several instances of ice retreat and readvance before the final retreat. This study demonstrates that in western Washington, marine sediment cores can be used to reconstruct continental ice cover. Here, I present a reconstruction of terrestrial landscape evolution within the Puget Sound during the last deglaciation, using geochemical analyses of organic matter from marine sediment cores. I measured the carbon isotope composition in bulk organic matter (d13Corg) and concentrations of leaf wax biomarkers (n-alkanes and fatty acid methyl esters) from three marine sediment cores off the coast of Washington State. Sedimentary organic matter is predominantly terrestrial in origin in all three cores and constitutes 75-95% of the total organic matter. The end of glacial sedimentation is marked by a positive carbon isotope excursion (2.3 - 6.9‰ in magnitude) and by an increase in concentration of leaf wax biomarkers, that most likely represents a period of rapid ice sheet retreat in the Puget Lowlands. Using biomarker abundances to produce an estimate for terrestrial organic matter (%Terr) and an isotope mass balance mixing model, I determined the isotopic excursion represents a change in source of vegetation cover among C3plant varieties. My calculations suggest that shrubs and forbs were more abundant than trees in the Puget Lowlands during the last glacial period. Furthermore, I propose the positive isotopic excursion marks the drainage of Glacial Lake Russell into the Strait of Juan de Fuca and the reorganization of continental drainage pathways as the Puget Lobe of the CIS retreated north.
Type
Text
Keywords
stable isotopes, biomarkers, Puget Lobe, Cordilleran Ice Sheet, carbon, n-alkanes, Fatty Acids, vegetation cover, Pacific Northwest plants
Publisher
Western Washington University
OCLC Number
1452262148
Subject – LCSH
Land cover--Washington (State)--Puget Sound; Phytogeography--Washington (State)--Puget Sound; Drift--Washington (State)--Puget Sound; Marine sediments--Washington (State)--Puget Sound--Analysis; Drift--Washington (State)--Puget Sound
Geographic Coverage
Puget Sound (Wash.)
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
McQuarrie, Emily, "Reconstructing vegetation cover during the retreat of the Puget Lobe of the Cordilleran Ice Sheet using organic matter from marine sediment cores" (2024). WWU Graduate School Collection. 1326.
https://cedar.wwu.edu/wwuet/1326