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Understanding Jurassic and Cretaceous High Arctic Paleoenvironmental and Paleoclimate Change

Subject Area Palaeontology
Term from 2012 to 2023
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 208089140
 
Final Report Year 2024

Final Report Abstract

Understanding the paleoenvironmental and paleoclimatic evolution of Canada’s Arctic region is essential for assessing short- and long-term climate, environmental, and paleogeographic changes during the Jurassic and Cretaceous periods. Our three Arctic field seasons (2011, 2014, 2019) were highly successful; for the first time, we documented significant Jurassic and Cretaceous paleoceanographic and paleoclimatic events, including Oceanic Anoxic Events (OAEs; Toarcian Event, Weissert Event, OAE1a, late Aptian cold snap, OAE2, OAE3) at Glacier Fiord, Lost Hammer, Slidre Fiord, and Strand Fiord on Axel Heiberg Island and Eidsbotn Graben at Devon Island of the High Arctic Sverdrup Basin. We also made substantial advancements in the chronology of lithostratigraphic Formations of the High Arctic Jurassic-Cretaceous sedimentary successions, which is crucial for understanding the evolution of the Sverdrup Basin during the Mesozoic and the associated volcanism, particularly the relationship between Arctic Large Igneous Province (LIP) volcanism and Oceanic Anoxic Events such as the (OAEs 1a and 2). Our findings suggests that the Jurassic and Cretaceous High Arctic Ocean functioned as a significant carbon sink on a global scale and underscore the potential of these sedimentary successions to reveal marine paleoenvironmental dynamics during Jurassic and Cretaceous key intervals. Using proxies such as carbon and osmium isotopes, TEX86, organic geochemistry (i.e., biomarker), and microfossils, we recorded variations in temperature, productivity, and the onset of dysoxic to anoxic bottom waters. Furthermore, we were able to calibrate Arctic diatom and silicoflagellate evolution within a chronostratigraphic framework for the late Cretaceous. The latter will help to illuminate a long-standing gap in the siliceous plankton evolution, bridging the exceptionally well-preserved middle Albian diatoms from the Weddell Sea of Antarctica and the well-documented Campanian/Maastrichtian silicoflagellate and diatom-rich deposits. Our international collaborative efforts have resulted in several peer-reviewed publications numerous B.Sc. and M.Sc. theses that enhance our understanding of the Mesozoic evolution of the High Arctic realm. Furthermore, as part of our public relations work, we have produced a documentary film, ‘Arctic Greenhouse’, to make our findings accessible to a wider public.

Publications

 
 

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