Set number: 3230

  • Watznaueria tubulata 9239 1
  • Watznaueria tubulata 9242 2
  • Watznaueria tubulata 9243 3
  • Watznaueria tubulata 9245 4
  • Watznaueria tubulata 9240 5
  • Watznaueria tubulata 9241 6
  • Watznaueria tubulata 9244 7
    10µm
Watznaueria tubulata, Late Albian, Folkestone, England

Set number: 3229

  • Watznaueria tubulata 12874 1
  • Watznaueria tubulata 12876 2
  • Watznaueria tubulata 12879 3
  • Watznaueria tubulata 12881 4
  • Watznaueria tubulata 12875 5
  • Watznaueria tubulata 12877 6
  • Watznaueria tubulata 12878 7
  • Watznaueria tubulata 12880 8
    10µm
Watznaueria tubulata, Middle Albian, Folkestone, England

Set number: 3231

  • Watznaueria tubulata 2668 1
  • Watznaueria tubulata 2667 2
  • Watznaueria tubulata 2665 3
  • Watznaueria tubulata 2666 4
    10µm
Watznaueria tubulata, Late Aptian, Gargas, SE France

Set number: 3235

  • Watznaueria tubulata 2911 1
  • Watznaueria tubulata 2910 2
  • Watznaueria tubulata 2908 3
  • Watznaueria tubulata 2909 4
    10µm
Watznaueria tubulata, Early Hauterivian, Speeton Clay at Speeton, England

Set number: 3234

  • Watznaueria tubulata 3602 1
  • Watznaueria tubulata 3601 2
  • Watznaueria tubulata 3599 3
  • Watznaueria tubulata 3600 4
    10µm
Watznaueria tubulata, Early Hauterivian, Speeton Clay at Speeton, England
Final Epithet
Watznaueria tubulata (Grün & Zweili, 1980) de Kaenel & Bergen, 1996
Basionym

Ellipsagelosphaera? tubulata Grün & Zweili, 1980

Optical Properties

The shields, as well as the tube cycles, display first-order white interference colours with inclined extinction lines and length-fast (–) elongation. In distal view, extinction angles are approximately 82° in the shields. This angle cannot be directly measured in the tube cycles due to the oblique orientation of their constituent elements; however, the apparent angle between extinction lines in the tube cycle is about 73°, corresponding to an obliquity of about 17°. Differentiation of the inner and outer tube cycles is difficult under all illumination conditions.

Remarks

Elliptical species of Watznaueria are characterised by a large subcircular to elliptical central opening devoid of internal structures. The width of the central opening consistently exceeds that of the pelaga. Watznaueria tubulata differs from Watznaueria fossacincta and Watznaueria martelae in possessing a large central opening wider than the pelaga, whereas the latter species have smaller openings with widths less than that of the pelaga. In addition, extinction angles in the tube cycles and shields differ significantly between these taxa.

Watznaueria tubulata is further distinguished from Watznaueria coronata by its large subcircular to elliptical central opening, whereas the latter exhibits a narrow, elongate opening.

References

de Kaenel, E. & Bergen, J. A. 1996b. Mesozoic calcareous nannofossil biostratigraphy from sites 897, 899, and 901, Iberia Abyssal Plain: New biostratigraphic evidence. Proceedings of the Ocean Drilling Program, Scientific Results. 149: 27-59

Grün, W. & Zweili, F. 1980. Das kalkige Nannoplankton der Dogger-Malm-Grenze im Berner Jura bei Liesberg (Schweiz). Jahrbuch der Geologischen Bundesanstalt. 123: 231-341.