Cuneus is a genus of foraminifera in the Rotaliida found in Upper Cretaceous (Coniacian) to Paleocene marine sediments throughout the boreal regions. The test is pyramidal in form, triserial throughout, with a triangular section, and may be slightly twisted. The test wall is calcareous, transparent. and finely perforate, the surface smooth. Sides are flat to slightly concave; sutures flush and oblique. The aperture is a narrow vertical loop on the apertural face of the final chamber.
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| - Cuneus (protista) (es)
- Cuneus (foram) (en)
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| - Cuneus is a genus of foraminifera in the Rotaliida found in Upper Cretaceous (Coniacian) to Paleocene marine sediments throughout the boreal regions. The test is pyramidal in form, triserial throughout, with a triangular section, and may be slightly twisted. The test wall is calcareous, transparent. and finely perforate, the surface smooth. Sides are flat to slightly concave; sutures flush and oblique. The aperture is a narrow vertical loop on the apertural face of the final chamber. (en)
- Cuneus es un género de foraminífero bentónico de la familia Turrilinidae, de la superfamilia Turrilinoidea, del suborden Buliminina y del orden Buliminida. Su especie tipo es . Su rango cronoestratigráfico abarca desde el Coniaciense (Cretácico superior) hasta el Paleoceno. (es)
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| - mid Late Cretaceous to Paleocene (en)
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| - Cuneus is a genus of foraminifera in the Rotaliida found in Upper Cretaceous (Coniacian) to Paleocene marine sediments throughout the boreal regions. The test is pyramidal in form, triserial throughout, with a triangular section, and may be slightly twisted. The test wall is calcareous, transparent. and finely perforate, the surface smooth. Sides are flat to slightly concave; sutures flush and oblique. The aperture is a narrow vertical loop on the apertural face of the final chamber. (en)
- Cuneus es un género de foraminífero bentónico de la familia Turrilinidae, de la superfamilia Turrilinoidea, del suborden Buliminina y del orden Buliminida. Su especie tipo es . Su rango cronoestratigráfico abarca desde el Coniaciense (Cretácico superior) hasta el Paleoceno. (es)
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