Calcareous dinoflagellate blooms during the Late Cretaceous 'greenhouse' world- a case study from western Ukraine

The Late Cretaceous was a unique period in the history of the Earth characterized by elevated sea levels, reduced land area, and significantly high concentrations of atmospheric CO2 resulting in increased temperatures across the globe-a 'Greenhouse World'. During this period, calcareous dinoflagellate cysts (c-dinocysts) flourished and became a ubiquitous constituent of calcifying plankton around the world. An acme in calcareous dinocysts during the Albian to the Turonian coincided with the highest recorded seawater surface temperatures and was possibly linked to conditions that favored calcification and a highly oligotrophic system in European shelf seas. This study examines the potential applicability of c-dinocysts as a proxy for paleoenvironmental conditions based on their assemblage changes plotted against foraminiferal occurrences and microfacies analysis. The material was extracted from the upper Turonian chalk of the Dubivtsi region in western Ukraine. An inverse correlation was observed between species diversity and the number of c-dinocyst specimens. Nutrient availability gradients apparently determined important changes in the calcareous dinocysts distribution. These trophic changes were likely caused by the interplay of eustatic sealevel fluctuations and Subhercynian tectonic activity leading to changeable nutrient inputs from the nearby land.

Automated summary

The Late Cretaceous was a unique period characterized by elevated sea levels, reduced land area, and high concentrations of atmospheric CO2. Calcification of plankton, specifically calcareous dinoflagellate cysts, was prevalent during this time and may be a potential proxy for paleoenvironmental conditions. Nutrient availability and tectonic activity influenced the distribution of calcareous dinocysts.