Rapid carbon input into the ocean–atmosphere system caused a dramatic shoaling of the
lysocline during the Paleocene–Eocene thermal maximum (PETM), a transient (∼ 170kyr) …

Nannofossil data from ODP Site 711 (equatorial Indian Ocean) yield a set of consistent,
reliable biohorizons that form the basis of a revised calcareous nannofossil biostratigraphy …

Palaeoecological changes in nannofossil assemblages in the Southern Ocean during
Oligocene times are examined through high-resolution, quantitative analyses of samples …

Based on the distribution patterns of seventy calcareous nannofossil species from one
hundred and seventy samples from the Oued Ettalla section (Central Tunisia), the upper …

We present new δ13C and δ18O records of surface (Morozovella and Acarinina) and
thermocline dwelling (Subbotina) planktonic foraminifera and benthic foraminifera …

Sedimentary archives from the world's oceans and continents indicate that as the world
warmed from the mild climate conditions of the mid-Paleocene to the extreme global warmth …

Within the last decade, several early Eocene hyperthermals have been detected globally.
These transient warming events have mainly been characterized geochemically–using …

In this study we present the results of a detailed analysis on calcareous nannofossil
assemblages from sediment cores of ODP Site 1263 (Southern East Atlantic, Walvis Ridge) …

Abstract The Paleocene-Eocene Thermal Maximum (PETM) was identified for the first time in
two sections (Bongue and Dibamba) from the Douala sub-basin located in the Gulf of …

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 …