Three key Paleocene deep-sea sections crop** out in northern Italy contain intercalations
of calciturbiditic, larger foraminifera-bearing beds derived from shallow water environments …

A marked switch in the abundance of the planktic foraminiferal genera Morozovella and
Acarinina occurred at low-latitude sites near the start of the Early Eocene Climatic Optimum …

Abstract Multiple short-term (< 10 5 years) global warming events (“hyperthermals”) occurred
throughout the early Eocene. Chemical weathering of continental silicate rocks is …

Abstract The Middle Eocene Climatic Optimum (MECO) was an unusual global warming
event that interrupted the long‐term Eocene cooling trend ca. 40 Ma. Here we present new …

The late Paleocene to early Eocene interval is characterized by a series of carbon
perturbations that caused transient warming (hyperthermal) events, of which the Paleocene …

The early to middle Eocene is marked by prominent changes in calcareous nannofossil
assemblages coinciding both with long‐term climate changes and modification of the North …

We combine stable isotope, calcareous nannoplankton, and benthic foraminiferal records for
Ocean Drilling Program Sites 1262 (paleodepth~ 3,500 m) and 1263 (paleodepth~ 1,500 m) …

Environmental and biotic responses to early Eocene hyperthermal events in the southwest
Pacific are critical for global paleoclimate reconstructions during Cenozoic greenhouse …

Silicified peritidal carbonates of the Tonian Draken Formation, Spitsbergen, contain highly
diverse and well‐preserved microfossil assemblages dominated by filamentous microbial …

Numerous models have been proposed to constrain the process of the South China Sea
formation, yet the Paleogene paleoenvironmental researches are hindered by the paucity of …