Growth of multichambered foraminifera can be studied by investigation of chamber volumes.
This approach is applicable to the vast majority of living and fossil species. Cell growth is …

Abstract The Paleocene‐Eocene Thermal Maximum (PETM) is associated with major
extinctions in the deep ocean, and significant paleogeographic and ecological changes in …

We present here new quantitative analyses of planktic and benthic foraminifera to assess
the impact of the Middle Eocene Climatic Optimum (MECO,~ 40 Ma) on these biotic groups …

Biostromes and low‐relief bioherms, some of which are characterized by exceptionally
large, flat specimens of larger benthic foraminifera, are common in Palaeogene and …

This study focuses on the paleontological content of the middle Eocene (Bartonian)
carbonate–siliciclastic sediments of the Capo Mortola Calcarenite Formation from Olivetta …

Previous attempts to quantify the test-flattening trend in Heterostegina depressa with water
depth have been rather unsuccessful. Due to its broad depth distribution, H. depressa is a …

The present study provides new data on the diversity, abundance and depth distribution of
larger foraminifera (LBF) from a number of sites offshore Brunei Darussalam. This region …

The genesis of nummulite banks remains a poorly understood topic and the aim of this work
is to shed light on it by observing the hydrodynamic behavior of selected larger foraminifera …

Representatives of the foraminifer Nummulites are important in Earth history for timing
Cenozoic shallow-water carbonates. Taphonomic complexity explains the construction of …

Morphometric characters of equatorial sections of larger benthic foraminifera have been
widely applied to define species for both biostratigraphic and evolutionary studies. In order …