Original paper
Organic-walled dinoflagellate cysts in biostratigraphy: state of the art and perspectives for future research
Pross, Jörg; Bijl, Peter K.; Brinkhuis, Henk; Bujak, Jonathan; Eldrett, James S.; Fensome, Robert A.; Head, Martin J.; Kotthoff, Ulrich; Pearce, Martin A.; Riding, James B.; Sangiorgi, Francesca; Schiøler, Poul; Śliwińska, Kasia K.; Sluijs, Appy; Williams, Graham L.
Newsletters on Stratigraphy (2025)
247 references
published online: May 8, 2025
manuscript accepted: Mar 31, 2025
manuscript received: Feb 3, 2025
Open Access (paper may be downloaded free of charge)
Abstract
Over the past 70 years, the potential of organic-walled dinoflagellate cysts (or dinocysts) for the dating and correlation of marine deposits from the Upper Triassic onwards has been increasingly realized, and dinocyst biostratigraphy has developed into a valuable stratigraphic method both in academic and industrial applications. Its utility is traditionally considered to be greatest in shelfal settings, but dinocyst biostratigraphy has also been successfully applied to deep-ocean sedimentary successions. As such, dinocyst-derived age information is complementary to that of other microfossil groups with typically more offshore distribution centers such as planktonic foraminifera, calcareous nannofossils, diatoms, and radiolaria. Due to the limited preservation potential of calcareous and siliceous microfossils in high-latitude settings, dinocysts are particularly important for age determinations in polar to sub-polar regions. The versatility of dinocyst signals is further enhanced in microscope slide preparations containing these microfossils because they typically also include terrestrial palynomorphs such as pollen and spores, yielding direct land–sea correlations. Regardless of its impressive potential, dinocyst biostratigraphy comes with specific challenges. The present article aims to provide a critical and comprehensive review of dinocyst biostratigraphy. It first discusses the principles of dinocyst morphology and taxonomy, as well as current concepts in dinoflagellate (cyst) paleoecology, because accurate identification and an understanding of environmental tolerances are indispensable for successful dinocyst-based biostratigraphic analysis. It then considers the suitability of dinocysts as biostratigraphic markers in terms of morphological distinctiveness and abundances, taxonomic diversity, stratigraphic ranges, and (paleo-) geographic distributions. Finally, it identifies perspectives and potential for future work.
Keywords
dinoflagellate cyst • biostratigraphy • Mesozoic • Paleogene • Neogene • Quaternary