Abstract
The Latest Danian Event is a short warming event, documented for the early Paleogene. Similar to Paleocene-Eocene Thermal Maximum, this event is characterized by global warming, carbonate disolution and shallowing of lysocline and CCD, poor oxygenated and stratified column water.
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Kotti, N., Mardassi, B., & Ouali, J. A. (2018). Application of geochemistry to characterize the progressive paleoenvironmental changes linked to abrupt warming hyperthermal event during the latest danian of central tunisia (Southern tethys) and impact on foraminifera fauna. In Advances in Science, Technology and Innovation (pp. 1673–1676). Springer Nature. https://doi.org/10.1007/978-3-319-70548-4_486
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