Set number: 3233

  • Watznaueria martelae 3449 1
  • Watznaueria martelae 3450 2
  • Watznaueria martelae 3452 3
  • Watznaueria martelae 3451 4
    10µm
Watznaueria cf.coronata, Late Maastrichtian, The specific location cannot be disclosed.

Set number: 3238

  • Watznaueria gresslyi 3526 1
  • Watznaueria gresslyi 3525 2
  • Watznaueria gresslyi 3523 3
  • Watznaueria gresslyi 3524 4
    10µm
Watznaueria cf.coronata, Early Valanginian, DSDP Leg 76, Site 534, Blake-Bahama Basin, Atlantic Ocean

Set number: 3239

  • Watznaueria gresslyi 1425 1
  • Watznaueria gresslyi 1424 2
    10µm
Watznaueria cf.coronata, Tithonian, Mississippi Canyon, Gulf of Mexico
Final Epithet
Watznaueria cf.coronata (Gartner, 1968) Bukry, 1969
Basionym

Watznaueria cf. coronata (Gartner, 1968) Bukry, 1969

Description

Elliptical species of Watznaueria are characterised by single-tiered distal and proximal shields, narrow tube cycles, and a broad, elongate central opening devoid of central-area structures. The central opening exceeds 1.5 μm in width and has an ellipticity greater than 1.5.

Optical Properties

Under cross-polarised light in plan view, the shields and tube cycles exhibit white interference colours, inclined extinction lines, and length-fast (–) elongation. Extinction angles measured on the distal side are approximately 75° in the shields and 71° in the tube cycles. The locking cycle remains in constant extinction, forming a narrow dim suture between the shield and tube cycle.

References

Bukry, D. 1969. Upper Cretaceous coccoliths from Texas and Europe. University of Kansas Paleontological Contributions, Articles 51 (Protista 2): 1-79.

Gartner, S., 1968. Coccoliths and related calcareous nannofossils from Upper Cretaceous deposits of Texas and Arkansas. University of Kansas Paleontological Contributions, Articles 48 (Protista 1), 1-56.