| Summary: | The Latest Danian Event (LDE, ~ 62.2Ma) is characterized by global changes in the carbon cycle as indicated by two negative δ 13 C excursions of up to ~ 1‰. These δ 13 C shifts are accompanied by a 2–3°C warming of both surface and deep waters based on benthic and planktic foraminiferal δ 18 O measurements, and the LDE has, thus, been considered as a so-called hyperthermal event. The event lasted for 200kyr and has been identified in various ocean basins and shallow marine settings. Here, we present a compilation of data from three deep-sea cores covering the Pacific, North and South Atlantic oceans as well as a southern Tethyan shelf section to document the response of planktic foraminifera assemblages to ocean warming. In all studied successions, we observe the disappearance of the planktic foraminifer genus Praemurica on a global scale that took place close to the onset of the LDE. Moreover, on the long run, praemuricids were contemporaneously replaced by morozovellids. Both the decline of Praemurica and a temperature increase started between 200 and 260 kyr before the LDE onset and were punctuated by the LDE itself. In this paper, we propose two mechanisms that have controlled the environmental changes associated with this event, (1) increased activity of the North Atlantic Igneous Province acting on long time-scales, and (2) changes of orbital parameters resulting in insolation changes on shorter time-scales.
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