Set number: 3194

  • Watznaueria arata 9078 1
  • Watznaueria arata 9081 2
  • Watznaueria arata 9083 3
  • Watznaueria arata 9084 4
  • Watznaueria arata 9079 5
  • Watznaueria arata 9080 6
  • Watznaueria arata 9082 7
    10µm
Watznaueria arata, Late Albian, Folkestone, SE England

Set number: 3195

  • Watznaueria arata 13103 1
  • Watznaueria arata 13106 2
  • Watznaueria arata 13107 3
  • Watznaueria arata 13109 4
  • Watznaueria arata 13104 5
  • Watznaueria arata 13105 6
  • Watznaueria arata 13108 7
    10µm
Watznaueria arata, Middle Albian, Folkestone, SE England

Set number: 3193

  • Watznaueria arata 3666 1
  • Watznaueria arata 3667 2
  • Watznaueria arata 3664 3
  • Watznaueria arata 3665 4
    10µm
Watznaueria arata, Early Berriasian, DSDP Leg 76, Site 534A, Blake-Bahama Basin, Atlantic Ocean

Set number: 3196

  • Watznaueria arata 34864 1
  • Watznaueria arata 34861 2
  • Watznaueria arata 34862 3
  • Watznaueria arata 34858 4
  • Watznaueria arata 34865 5
  • Watznaueria arata 34863 6
  • Watznaueria arata 34860 7
  • Watznaueria arata 34859 8
  • Watznaueria arata 34871 9
  • Watznaueria arata 34870 10
  • Watznaueria arata 34872 11
  • Watznaueria arata 34868 12
  • Watznaueria arata 34869 13
    10µm
Watznaueria arata, Early Turonian, Cauvery Basin, India
Final Epithet
Watznaueria arata (Black, 1973) Varol, n. comb.
Basionym

Ellipsagelosphaera arata Black, 1973

Optical Properties

In plan view under cross-polarised light, the shields display white interference colours, inclined extinction lines, and length-fast (–) elongation. The inner tube cycles exhibit less intense, greyish-white interference colours with inclined extinction. In distal side, the extinction angles in the shields is approximately 77°. This cannot be directly measured in the tube cycles due to the oblique orientation of their constituent segments; however, the apparent angle between extinction directions in the tube cycle is approximately 73°, corresponding to an obliquity of approximately 17°. Optical properties corroborate the presence of a narrow outer tube cycle observed under phase-contrast and bright-field illumination, especially in cross-polarised light with gypsum plate illumination. The locking cycle exhibits interference colours, producing a transitional boundary between the tube cycle and shield.

Remarks

Elliptical species of Watznaueria, composed of a single-tiered distal shield and a distinctly narrower single-tiered proximal shield, with a very narrow outer tube cycle and a wide, smooth inner tube cycle that completely closes the central area. The narrow outer tube cycle is readily observed under phase-contrast and bright-field illumination.

References

Black, M. 1973. British Lower Cretaceous Coccoliths. I-Gault Clay (Part 2). Palaeontographical Society Monograph 127: 49-112.