Devonian palynoevents in the circum-Arctic region

Authors

  • John E.A. Marshall School of Ocean and Earth Science, University of Southampton, National Oceanography Centre, Southampton SO14 3ZH, UK
  • Gunn Mangerud Department of Earth Science, University of Bergen, Allégaten 41, N-5007 Bergen, Norway
  • Manuel Bringué Geological Survey of Canada, 3303–3333 Street NW, Calgary, Alberta T2L 2A7, Canada
  • Jonathan Bujak Bujak Research (International), Burbage Lodge, Blackpool, Lancashire FY2 9JS, UK

DOI:

https://doi.org/10.4138/atlgeo.2022.015

Abstract

Devonian strata of the present-day Arctic contain abundant and diverse assemblages of terrestrial palynomorphs, particularly from Middle and Upper Devonian sections; few intervals of Lower Devonian and Silurian strata have been palynologically studied, and these demonstrate strong palynofloral similarities across the region. Based on published records, we present a compilation of six last occurrence events (LOs), 44 first occurrence events (FOs) and one acme event that have proven of value in correlation in the present-day Arctic. Although their chronostratigraphic resolution is relatively low, and a scarcity of independent age control hampers precise age assignments, palynology is the only biostratigraphic discipline available for confident chronostratigraphic correlation of most Arctic Devonian strata.

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2022-12-21

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Marshall, J. E., Mangerud, G., Bringué, M., & Bujak, J. (2022). Devonian palynoevents in the circum-Arctic region. Atlantic Geoscience, 58, 307–328. https://doi.org/10.4138/atlgeo.2022.015

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Special Series: Circum-Arctic Palynological Event Stratigraphy