Late Cretaceous (Cenomanian to Campanian) Dinoflagellate Cyst Assemblages and Palaeoproductivity Signals from the Kanguk Formation, Sverdrup Basin, Nunavut, Canada
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The response of the Polar Sea to Cretaceous carbon perturbations is poorly understood and palaeotemperature data from the Arctic are limited. To understand high latitude palaeoceanographic dynamics, dinocyst assemblages were collected from a composite Cenomanian to Campanian section from the Bastion Ridge and Kanguk formations within the Sverdrup Basin at Glacier Fiord, Axel Heiberg Island and Slidre Fiord, Ellesmere Island. Dinocyst assemblages were compared to carbon isotope and benthic foraminiferal age data indicating that age ranges for several Late Cretaceous dinocyst taxa need regional revision. At Glacier Fiord a turnover in dinocyst assemblages reveal a change from a brackish to marine palaeoenvironmental change before the onset of OAE 2. A correlation between δ13Corg, peridiniod dinoflagellate cysts and cooling global sea surface temperatures indicate an increase in palaeoproductivity during a Coniacian to Campanian cooling trend. Three dinocyst biozonations are proposed for the Sverdrup Basin.
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Copyright © 2018 the author(s). Theses may be used for non-commercial research, educational, or related academic purposes only. Such uses include personal study, research, scholarship, and teaching. Theses may only be shared by linking to Carleton University Institutional Repository and no part may be used without proper attribution to the author. No part may be used for commercial purposes directly or indirectly via a for-profit platform; no adaptation or derivative works are permitted without consent from the copyright owner.
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