REDOX GEOCHEMISTRY AND CARBON ISOTOPE CHEMOSTRATIGRAPHY OF THE MIDDLE-LATE DEVONIAN HORN RIVER GROUP
Abstract/Contents
- Abstract
- The Late Devonian mass extinction is the most contentious of the “Big Five” extinction events: its timing, severity, and causes remain under much debate. A major hindrance to a holistic understanding of the Late Devonian mass extinction event(s) is a lack of sedimentary geochemical data coupled with a lack of reliable age constraints. Moreover, during this interval, oxygen levels may have stabilized to modern levels for the first time in Earth’s history. To better characterize changes in marine redox conditions and their relationship to the Late Devonian extinction, I measured iron speciation and carbon isotopes to characterize the Horn River Group, Northwest Territories, Canada. These data elucidate local redox conditions and more precisely correlate the shales and carbonates understood to be broadly co-eval in time. My findings show that the basin was predominantly euxinic throughout the Middle Devonian, and that it likely records the Frasnes hot shale event. Whereas much work remains to be done to characterize the enigmatic Late Devonian extinctions, the results presented here represent a step forward in understanding how marine redox conditions varied throughout the Devonian.
Description
Type of resource | text |
---|---|
Publication date | January 5, 2023 |
Creators/Contributors
Author | Endriga, Cecilia |
---|---|
Thesis advisor | Sperling, Erik |
Advisor | Payne, Jonathan |
Degree granting institution | Stanford University |
Department | Geological Sciences |
Subjects
Subject | Devonian |
---|---|
Subject | Geochemistry |
Genre | Text |
Genre | Thesis |
Bibliographic information
Access conditions
- Use and reproduction
- User agrees that, where applicable, content will not be used to identify or to otherwise infringe the privacy or confidentiality rights of individuals. Content distributed via the Stanford Digital Repository may be subject to additional license and use restrictions applied by the depositor.
- License
- This work is licensed under a Creative Commons Attribution Non Commercial 4.0 International license (CC BY-NC).
Preferred citation
- Preferred citation
- Endriga, C. (2023). REDOX GEOCHEMISTRY AND CARBON ISOTOPE CHEMOSTRATIGRAPHY OF THE MIDDLE-LATE DEVONIAN HORN RIVER GROUP. Stanford Digital Repository. Available at https://purl.stanford.edu/hd310tx5135. https://doi.org/10.25740/hd310tx5135.
Collection
Master's Theses, Doerr School of Sustainability
View other items in this collection in SearchWorksContact information
- Contact
- celyt@stanford.edu
Also listed in
Loading usage metrics...