Abstract
The Paleocene epoch showed short and extremely warm (hyperthermal) episodes.They are known as the Late Danian Event (LDE); the Danian/Selandian (D/S) event; the early-late Paleocene event (ELPE), also known as the mid-Paleocene biotic event (MPBE); and likely part of the long-lasting environmental disruption known as the Selandian-Thanetian Transition Event (STTE). Such prevailed warm and…