A. Guy Plint
Trans-Atlantic correlation of Late Cretaceous high-frequency sea-level cycles
Plint, A. Guy; Uličný, David; Čech, Stanislav; Walaszczyk, Ireneusz; Gröcke, Darren R.; Laurin, Jiří; Shank, Joel A.; Jarvis, Ian
Authors
David Uličný
Stanislav Čech
Ireneusz Walaszczyk
Professor Darren Grocke d.r.grocke@durham.ac.uk
Professor
Jiří Laurin
Joel A. Shank
Ian Jarvis
Abstract
Previous studies of Cretaceous sedimentary rocks have used multi-proxy correlation methods to suggest eustatic change, modulated by the c. 400 kyr long eccentricity rhythm. Although numerous authors have inferred eustatic changes on shorter timescales, none have demonstrated synchronous sea-level changes in separate basins on different plates, thousands of kilometres apart. Our study integrates basin-scale, three-dimensional sequence architecture, molluscan biostratigraphy, and carbon-isotope chemostratigraphy to demonstrate synchronous sea-level changes in upper Turonian to lower Coniacian shallow-marine clastic successions in the Western Canada Foreland Basin, and the Bohemian Cretaceous Basin. Depositional sequences in both basins are plotted in a common time domain using an astronomically calibrated age model, allowing direct comparison. In both basins, at least seven major transgressive events can be shown to be synchronous within the limits of combined biostratigraphic and chemostratigraphic resolution. ‘Major’ and ‘minor’ sequences of late Turonian age appear to have been paced, respectively, by the long (c. 400 kyr) and short (c. 100 kyr) eccentricity cycles. In contrast, early Coniacian sequences evidence pacing by the c. 38 kyr obliquity rhythm. Stratal architecture suggests that sequences developed in response to eustatic changes of c. 14–20 m at average rates ranging 0.08 to >1.3 m/kyr. At a time of ‘warm greenhouse’ climate, sea-level change of this magnitude and timescale may not be explicable entirely as a result of thermal- and aquifer-eustasy, and hence glacio-eustasy may also have been a contributing factor.
Citation
Plint, A. G., Uličný, D., Čech, S., Walaszczyk, I., Gröcke, D. R., Laurin, J., Shank, J. A., & Jarvis, I. (2022). Trans-Atlantic correlation of Late Cretaceous high-frequency sea-level cycles. Earth and Planetary Science Letters, 578, Article 117323. https://doi.org/10.1016/j.epsl.2021.117323
Journal Article Type | Article |
---|---|
Acceptance Date | Nov 25, 2021 |
Online Publication Date | Dec 7, 2021 |
Publication Date | 2022-01 |
Deposit Date | Dec 17, 2021 |
Publicly Available Date | Dec 7, 2022 |
Journal | Earth and Planetary Science Letters |
Print ISSN | 0012-821X |
Publisher | Elsevier |
Peer Reviewed | Peer Reviewed |
Volume | 578 |
Article Number | 117323 |
DOI | https://doi.org/10.1016/j.epsl.2021.117323 |
Public URL | https://durham-repository.worktribe.com/output/1218581 |
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http://creativecommons.org/licenses/by-nc-nd/4.0/
Copyright Statement
© 2021. This manuscript version is made available under the CC-BY-NC-ND 4.0 license https://creativecommons.org/licenses/by-nc-nd/4.0/
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