Set number: 3214

  • Watznaueria cynthae 36401 1
  • Watznaueria cynthae 36398 2
  • Watznaueria cynthae 36402 3
  • Watznaueria cynthae 36407 4
  • Watznaueria cynthae 36400 5
  • Watznaueria cynthae 36399 6
  • Watznaueria cynthae 36403 7
  • Watznaueria cynthae 36408 8
    10µm
Watznaueria cynthae, Early Turonian, CB06 C-T, Cauvery Basin, India

Set number: 3213

  • Watznaueria cyntiae 3540 1
  • Watznaueria cynthae 3539 2
  • Watznaueria cynthae 3537 3
  • Watznaueria cynthae 3538 4
    10µm
Watznaueria cynthae, Early Valanginian, DSDP Leg 76, Site 534, Blake-Bahama Basin, Atlantic Ocean

Set number: 3212

  • Watznaueria cynthae 2739 1
  • Watznaueria cynthae 2740 2
  • Watznaueria cynthae 2742 3
  • Watznaueria cynthae 2741 4
    10µm
Watznaueria cynthae, Late Aptian, Gargas, SE France
Final Epithet
Watznaueria cynthae Worsley, 1971
Basionym

Watznaueria cynthae Worsley, 1971

Optical Properties

The shields, as well as the inner and outer tube cycles, display first-order white interference colours with inclined extinction lines and length-fast (–) elongation. In distal view, the extinction angles are approximately 73° in the distal shield and about 68° in the tube cycles. Variation in the orientation of extinction lines between the tube cycles and the shield supports the identification of a narrow outer tube cycle, in conjunction with observations under phase-contrast and bright-field illumination.

Remarks

Large (>8.0 µm), subcircular to elliptical species of Watznaueria, characterised by a wide inner tube cycle bearing two pores arranged diagonally along the long axis of the placolith. The central area is often more elliptical than the shields. The narrow outer tube cycle is readily observed under phase-contrast and bright-field illumination.

Watznaueria cynthae differs from Watznaueria biporta primarily in the arrangement of the pores: in Watznaueria cynthae, the pores are diagonally aligned, whereas in Watznaueria biporta they are aligned along the long axis of the placolith.

References

Worsley, T. R., 1971. Calcareous nannofossil zonation of Upper Jurassic and Lower Cretaceous sediments from the Western Atlantic. In: Farinacci, A. (ed.), Proceedings of the Second Planktonic Conference Roma 1970. Edizioni Tecnoscienza, Rome vol. 2, pp. 1301-1321.