Set number: 1757

  • Ellipsagelosphaera britannica 5183 1
  • Ellipsagelosphaera britannica 5186 2
  • Ellipsagelosphaera britannica 5187 3
  • Ellipsagelosphaera britannica 5184 4
  • Ellipsagelosphaera britannica 5185 5
  • Ellipsagelosphaera britannica 5188 6
    10µm
Ellipsagelosphaera britannica, Early Tithonian, Eastern Gulf of Mexico

Set number: 1758

  • Ellipsagelosphaera britannica 3808 1
  • Ellipsagelosphaera britannica 3804 2
  • Ellipsagelosphaera britannica 3807 3
  • Ellipsagelosphaera britannica 3809 4
  • Ellipsagelosphaera britannica 3805 5
  • Ellipsagelosphaera britannica 3806 6
    10µm
Ellipsagelosphaera britannica, Early Valanginian, DSDP Leg 76, Site 534, Blake-Bahama Basin, Atlantic Ocean

Set number: 1759

  • Ellipsagelosphaera britannica 3511 1
  • Ellipsagelosphaera britannica 3510 2
  • Ellipsagelosphaera britannica 3508 3
  • Ellipsagelosphaera britannica 3509 4
    10µm
Ellipsagelosphaera britannica, Early Valanginian, DSDP Leg 76, Site 534, Blake-Bahama Basin, Atlantic Ocean
Final Epithet
Ellipsagelosphaera britannica (Strander, 1963) Perch-Nielsen, 1968c
Basionym

Coccolithus britannicus Stradner, 1963

Dimensions Of Holotype

In plan view under cross-polarised light, all parts exhibit inclined extinction lines and length-fast (-) elongation. The extinction lines are dextrogyre on the distal side, and their typical angle is about 67° on the distal shield, but they can not be measured in the tube cycle due to the oblique orientation of the tube cycle segments. The apparent angle between extinction on the tube cycle is 73°, corresponding to an obliquity angle of 17°.

Description

The elliptical placolith consists of single-tiered distal and proximal shields, a double tube cycle and a central area spanned by a disjunct traverse bar. 

References

Perch-Nielsen, K., 1968c. Der Feinbau und die Klassifikation der Coccolithen aus dem Maastrichtien von Danemark. Biologiske Skrifter, Kongelige Danske Videnskabernes Selskab 16, 1-96.

Stradner, H. 1963. New contributions to Mesozoic stratigraphy by means of nannofossils. Proceedings of the Sixth World Petroleum Congress. Section 1 Paper 4: 167-183.