Paleoenvironmental fluctuations across the Jurassic–Cretaceous boundary from the Scotian margin, Canada

Two wells, Thebaud C-74 and South Desbarres O-76 were investigated to evaluate paleoenvironmental changes during the Jurassic/Cretaceous boundary on the Scotian margin, offshore Nova Scotia. A multi-technique approach using several proxies of paleoredox, productivity, terrigenous input, and paleosal...

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Main Author: Lin, Noelle Jia-Rong
Format: Thesis
Language:English
Published: Memorial University of Newfoundland 2023
Subjects:
Online Access:https://research.library.mun.ca/16013/
https://research.library.mun.ca/16013/1/converted.pdf
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spelling ftmemorialuniv:oai:research.library.mun.ca:16013 2023-10-01T03:57:59+02:00 Paleoenvironmental fluctuations across the Jurassic–Cretaceous boundary from the Scotian margin, Canada Lin, Noelle Jia-Rong 2023-05 application/pdf https://research.library.mun.ca/16013/ https://research.library.mun.ca/16013/1/converted.pdf en eng Memorial University of Newfoundland https://research.library.mun.ca/16013/1/converted.pdf Lin, Noelle Jia-Rong <https://research.library.mun.ca/view/creator_az/Lin=3ANoelle_Jia-Rong=3A=3A.html> (2023) Paleoenvironmental fluctuations across the Jurassic–Cretaceous boundary from the Scotian margin, Canada. Masters thesis, Memorial University of Newfoundland. thesis_license Thesis NonPeerReviewed 2023 ftmemorialuniv 2023-09-03T06:50:33Z Two wells, Thebaud C-74 and South Desbarres O-76 were investigated to evaluate paleoenvironmental changes during the Jurassic/Cretaceous boundary on the Scotian margin, offshore Nova Scotia. A multi-technique approach using several proxies of paleoredox, productivity, terrigenous input, and paleosalinity was employed, resulting in identification of a geochemical anomalies in both wells associated with the boundary. A shift to more reducing conditions and elevated productivity correlate with low terrigenous input at the start of the anomaly, followed by a shift of redox and productivity proxies back to background levels and elevated terrigenous input and paleosalinity. These correlative relationships are consistent in both wells, reflecting a transition to anoxic/euxinic conditions at the start of the anomaly that was predominantly driven by the consumption of oxidative agents due to a higher abundance of decomposing organic matter. The lack of correlation between productivity and terrigenous input indicates that the increase in micronutrients driving elevated productivity is not related to an influx of terrigenous input, but rather upwelling. The positive correlation between terrigenous input and paleosalinity suggests limited fluvial input. These results agree with global paleoclimate and sealevel variations during the Late Jurassic/Early Cretaceous and reflect semi-arid/arid conditions related to relative sealevel fall and open ocean circulation as the North Atlantic Ocean expanded. Thesis North Atlantic Memorial University of Newfoundland: Research Repository Canada
institution Open Polar
collection Memorial University of Newfoundland: Research Repository
op_collection_id ftmemorialuniv
language English
description Two wells, Thebaud C-74 and South Desbarres O-76 were investigated to evaluate paleoenvironmental changes during the Jurassic/Cretaceous boundary on the Scotian margin, offshore Nova Scotia. A multi-technique approach using several proxies of paleoredox, productivity, terrigenous input, and paleosalinity was employed, resulting in identification of a geochemical anomalies in both wells associated with the boundary. A shift to more reducing conditions and elevated productivity correlate with low terrigenous input at the start of the anomaly, followed by a shift of redox and productivity proxies back to background levels and elevated terrigenous input and paleosalinity. These correlative relationships are consistent in both wells, reflecting a transition to anoxic/euxinic conditions at the start of the anomaly that was predominantly driven by the consumption of oxidative agents due to a higher abundance of decomposing organic matter. The lack of correlation between productivity and terrigenous input indicates that the increase in micronutrients driving elevated productivity is not related to an influx of terrigenous input, but rather upwelling. The positive correlation between terrigenous input and paleosalinity suggests limited fluvial input. These results agree with global paleoclimate and sealevel variations during the Late Jurassic/Early Cretaceous and reflect semi-arid/arid conditions related to relative sealevel fall and open ocean circulation as the North Atlantic Ocean expanded.
format Thesis
author Lin, Noelle Jia-Rong
spellingShingle Lin, Noelle Jia-Rong
Paleoenvironmental fluctuations across the Jurassic–Cretaceous boundary from the Scotian margin, Canada
author_facet Lin, Noelle Jia-Rong
author_sort Lin, Noelle Jia-Rong
title Paleoenvironmental fluctuations across the Jurassic–Cretaceous boundary from the Scotian margin, Canada
title_short Paleoenvironmental fluctuations across the Jurassic–Cretaceous boundary from the Scotian margin, Canada
title_full Paleoenvironmental fluctuations across the Jurassic–Cretaceous boundary from the Scotian margin, Canada
title_fullStr Paleoenvironmental fluctuations across the Jurassic–Cretaceous boundary from the Scotian margin, Canada
title_full_unstemmed Paleoenvironmental fluctuations across the Jurassic–Cretaceous boundary from the Scotian margin, Canada
title_sort paleoenvironmental fluctuations across the jurassic–cretaceous boundary from the scotian margin, canada
publisher Memorial University of Newfoundland
publishDate 2023
url https://research.library.mun.ca/16013/
https://research.library.mun.ca/16013/1/converted.pdf
geographic Canada
geographic_facet Canada
genre North Atlantic
genre_facet North Atlantic
op_relation https://research.library.mun.ca/16013/1/converted.pdf
Lin, Noelle Jia-Rong <https://research.library.mun.ca/view/creator_az/Lin=3ANoelle_Jia-Rong=3A=3A.html> (2023) Paleoenvironmental fluctuations across the Jurassic–Cretaceous boundary from the Scotian margin, Canada. Masters thesis, Memorial University of Newfoundland.
op_rights thesis_license
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