The evolution of the Cenozoic cryosphere from unipolar to bipolar over the past 30 million
years (Myr) is broadly known. Highly resolved records of carbonate (CaCO3) content …

We investigate the response of calcareous nannoplankton to the middle-late Eocene
transition in the SW Neo-Tethys and compare our data to published results from X-ray …

Studying monsoon dynamics during past warm time periods such as the Miocene Climatic
Optimum (MCO;∼ 16.9–14.5 Ma) could greatly aid in better projecting monsoon intensity, in …

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 …

A detailed biostratigraphic, chemostratigraphic, and chronostratigraphic study was carried
out in the South‐Western margin of the Neo‐Tethys ocean (Tunisia) covering the Eocene …

The Chicxulub impact caused a crash in productivity in the world's oceans which contributed
to the extinction of∼ 75% of marine species. In the immediate aftermath of the extinction …

We reconstructed changes in productivity and surface/subsurface and deep-water dynamics
in the Western Mediterranean through a multi-proxy study of Ocean Drilling Program Site …

The global climate of the early Oligocene was characterized by initiated Antarctic glaciation
and meridional overturning circulation, which then led to profound eutrophication in the …

During IODP expedition 359 multiple holes recovered Modern to Middle Miocene sediments
from the Kardiva Drift which is strongly influenced by monsoonally-driven currents. Two …

Calcareous nannoplankton have been one of the dominant primary producers in the surface
oceans since the late Triassic. The bolide impact at the Cretaceous/Paleogene (K/Pg) …