Abstract The Paleocene/Eocene Thermal Maximum (PETM) is characterized by pronounced
global warming and associated environmental changes. In the more-or-less two decades …

The late Paleocene thermal maximum, or LPTM (ca. 55 Ma), represents a geologically brief
time interval (∼ 220 ky) characterized by profound global warming and associated …

Dinocyst assemblages changed abruptly during latest Thanetian mid-Biochron NP9 in low
and midlatitudes from relatively diverse populations with few Apectodinium to low-diversity …

To further understand the distribution and abundance of Apectodinium through space and
time, dinoflagellate cyst (dinocyst) records from two well-calibrated Paleogene sections in …

Ubiquitous predominance of Apectodinium, a presumably heterotrophic, warm water
dinoflagellate, is one of the most prominant biotic response in the marginal marine realm to …

Late Paleocene and Early Eocene climates and ecosystems underwent significant change
during several transient global warming phases, associated with rapidly increasing …

Manifestations of profound perturbations in biogeochemical systems during the Paleocene–
Eocene thermal maximum (PETM) include a prominent global negative δ13C and a …

Organic-walled dinoflagellate cysts and acritarchs are a vital tool for reconstructing past
environmental change, in particular in the Neogene of the high northern latitudes where …

Worldwide distribution of dinoflagellate cysts from the Aptian and Late Albian periods has
been reported on palaeogeographical maps. A total of 32 and 38 species, derived from 36 …

The Paleocene–Eocene Thermal Maximum (PETM, 56 Ma) was a phase of rapid global
warming associated with massive carbon input into the ocean–atmosphere system from a 13 …