The Diatom Dark Ages: Identification of mid-Cretaceous Arctic Platform diatoms from the basal transgression of the Kanguk Formation, Devon Island, Nunavut, Canada

• Main Author: Heins, Megan
• Format: Text
• Language: unknown
• Published: DigitalCommons@University of Nebraska - Lincoln 2022
• Subjects: micropaleontology; cretaceous; biostratigraphy; polar research; Earth Sciences; Geology; Oceanography and Atmospheric Sciences and Meteorology; Paleontology; Arctic; Nunavut; Canada; Devon Island
• Online Access: https://digitalcommons.unl.edu/geoscidiss/144; https://digitalcommons.unl.edu/context/geoscidiss/article/1147/viewcontent/Heins_2022.pdf

The lower part of the mid-Cretaceous Kanguk Formation (Lower Turonian interval) contains an important paleontological record crucial to the characterization of a poorly known interval of fossil marine diatoms history. Kanguk Formation mudstones are exposed in a ~200 m-thick section on Devon Island, Nunavut, Canadian High Arctic. Diatoms at this location are well-preserved due to shallow burial on this Arctic Platform site. The rock sequence was protected from glacial erosion that removed much of the Cretaceous record by being down-faulted in a linear graben. Study of these well-preserved fossil diatoms allows for a documentation of the assemblage, identification of potentially important biostratigraphic events, and an opportunity to assess paleoenvironmental changes that may have influenced their growth and sedimentation. This study identified 45 fossil marine diatom species and varieties, representing 22 genera, and some taxa that are treated informally. The lower ~60 meters of the Kanguk mudstone sequence on Devon Island is barren of diatoms, indicating that environmental conditions suitable for diatom growth were not coincident with the initial transgression, but developed later, or that marine connections that allowed migration of diatoms into the Arctic occurred after the marine transgression. Planktonic and benthic species are present in similar abundance suggesting a shallow water environment. The lower interval of the Kanguk Formation reported herein spans a ~3 m.y. time interval (~90.5 to ~93.5 Ma, Early Turonian) as indicated by carbon isotope chemostratigraphic correlations and silicoflagellate biostratigraphy, which allow correlation to other Kanguk Formation sections that are dated with bentonite ages. The presence of diatoms Gladius antiquus, Costopyxis antiqua, and Bascillicostephanus sp. 1 support these ages. Several events are identified as potentially important new biostratigraphic datum levels, which help divide the Gladius antiquus Zone and increase biostratigraphic resolution. In ascending ...