The ‘‘critical shear velocity’ ’ and ‘‘settling velocity’ ’ of foraminiferal shells are important parameters for determining hydrodynamic conditions during deposition of Nummulites banks. These can be estimated by determining the size, shape, and density of nummulitid shells examined in axial sections cut perpendicular to the bedding plane. Shell size and shape can be determined directly from the shell diameter and thickness, but density must be calculated indirectly from the thin section. Calculations using the half-tori method approx-imate shell densities by equalizing the chamber volume of each half whorl, based on the half whorl’s lumen area and its center of gravity. Results from this method yield the same lumen volumes produced empiri...
Palaeoenvironmental reconstruction using foraminifera relies on the assumption that assemblages refl...
International audienceWe investigated the influence of bioturbation by macrofauna on the vertical di...
We investigated the influence of bioturbation by macrofauna on the vertical distribution of living (...
The "critical shear velocity" and "settling velocity" of foraminiferal shells are important paramete...
The genesis of nummulite banks remains a poorly understood topic and the aim of this work is to shed...
The main physical variables influencing the hydrodynamic behaviour of nummulitid tests are size, den...
The genesis of nummulite banks remains a poorly understood topic and the aim of this work is to shed...
The genesis of nummulite banks remains a poorly understood topic and the aim of this work is to shed...
Larger benthic foraminifera (LBF) are important and prolific carbonate producers both in modern and ...
The calculation from 3D images of chamber volumes and shapes and their changes during ontogeny provi...
Four specimens of larger benthic foraminifera (the Recent Palaeonummulites venosus and Operculina am...
Th is work demonstrates the potential of three-dimensional biometric quantifi cation using microtomo...
Large benthic foraminifers are considered to be good indicators of shallow marine carbonate environm...
Laboratory experiments are undertaken in which the hydrodynamic properties of empty foraminifera tes...
Symbiont-bearing larger benthic foraminifera inhabit the photic zone to provide their endosymbiotic ...
Palaeoenvironmental reconstruction using foraminifera relies on the assumption that assemblages refl...
International audienceWe investigated the influence of bioturbation by macrofauna on the vertical di...
We investigated the influence of bioturbation by macrofauna on the vertical distribution of living (...
The "critical shear velocity" and "settling velocity" of foraminiferal shells are important paramete...
The genesis of nummulite banks remains a poorly understood topic and the aim of this work is to shed...
The main physical variables influencing the hydrodynamic behaviour of nummulitid tests are size, den...
The genesis of nummulite banks remains a poorly understood topic and the aim of this work is to shed...
The genesis of nummulite banks remains a poorly understood topic and the aim of this work is to shed...
Larger benthic foraminifera (LBF) are important and prolific carbonate producers both in modern and ...
The calculation from 3D images of chamber volumes and shapes and their changes during ontogeny provi...
Four specimens of larger benthic foraminifera (the Recent Palaeonummulites venosus and Operculina am...
Th is work demonstrates the potential of three-dimensional biometric quantifi cation using microtomo...
Large benthic foraminifers are considered to be good indicators of shallow marine carbonate environm...
Laboratory experiments are undertaken in which the hydrodynamic properties of empty foraminifera tes...
Symbiont-bearing larger benthic foraminifera inhabit the photic zone to provide their endosymbiotic ...
Palaeoenvironmental reconstruction using foraminifera relies on the assumption that assemblages refl...
International audienceWe investigated the influence of bioturbation by macrofauna on the vertical di...
We investigated the influence of bioturbation by macrofauna on the vertical distribution of living (...