Favocassidulina is a foraminiferal genus; rotaliid family Cassidulinidae, known from the middle Miocene to recent in the Indian and Pacific oceans. Its habitat is benthic, near shore.
The test wall is calcareous, finely perforate; primary wall indistinctly optically radial, as the calcite crystals are dendritic in form and occur in bundles; inner and outer surface of the wall covered by a microgranular veneer. Variation in wall structure results in thick walls appearing optically granular. The surface is covered with a secondarily formed honeycomb network of narrow elevated ridges forming polygonal open areas.
Favocassidulina is a foraminiferal genus; rotaliid family Cassidulinidae, known from the middle Miocene to recent in the Indian and Pacific oceans. Its habitat is benthic, near shore.
The test wall is calcareous, finely perforate; primary wall indistinctly optically radial, as the calcite crystals are dendritic in form and occur in bundles; inner and outer surface of the wall covered by a microgranular veneer. Variation in wall structure results in thick walls appearing optically granular. The surface is covered with a secondarily formed honeycomb network of narrow elevated ridges forming polygonal open areas.
Favocassidulina es un género de foraminífero bentónico de la subfamilia Cassidulininae, de la familia Cassidulinidae, de la superfamilia Cassidulinoidea, del suborden Buliminina y del orden Buliminida.[1][2] Su especie tipo es Pulvinulina parvus. Su rango cronoestratigráfico abarca desde el Mioceno medio hasta la Actualidad.
Clasificaciones previas incluían Favocassidulina en el suborden Rotaliina del orden Rotaliida.[3]
Favocassidulina incluye a las siguientes especies:[4][5]
Favocassidulina es un género de foraminífero bentónico de la subfamilia Cassidulininae, de la familia Cassidulinidae, de la superfamilia Cassidulinoidea, del suborden Buliminina y del orden Buliminida. Su especie tipo es Pulvinulina parvus. Su rango cronoestratigráfico abarca desde el Mioceno medio hasta la Actualidad.