Set number: 2763

  • Biscutum hannibalis 42324 1
  • Biscutum hannibalis 42328 2
  • Biscutum hannibalis 42327 3
  • Biscutum hannibalis 42331 4
  • Biscutum hannibalis 42325 5
  • Biscutum hannibalis 42326 6
  • Biscutum hannibalis 42329 7
  • Biscutum hannibalis 42330 8
  • Biscutum hannibalis 42334 9
  • Biscutum hannibalis 42333 10
    10µm
Biscutum centriperforatus, Late Cenomanian, Paipa Creek, Colombia

Set number: 2764

  • Biscutum hannibalis 5603 1
  • Biscutum hannibalis 5601 2
  • Biscutum hannibalis 5602 3
    10µm
Biscutum centriperforatus, Early Coniacian, Mauritania, West Africa

Set number: 2762

  • Biscutum hannibalis 2517 1
  • Biscutum hannibalis 2518 2
    10µm
Biscutum centriperforatus, Late Albian, Arabian Peninsula (The specific location cannot be disclosed)

Set number: 2761

  • Biscutum centriperforatus 2289 1
  • Biscutum hannibalis 2290 2
    10µm
Biscutum centriperforatus, Late Albian, Arabian Peninsula (The specific location cannot be disclosed)

Set number: 2760

  • Biscutum hannibalis 2264 1
  • Biscutum hannibalis 2265 2
    10µm
Biscutum centriperforatus, Late Albian, Arabian Peninsula (The specific location cannot be disclosed)
Final Epithet
Biscutum centriperforatus (Burns, 1976) Varol, n. comb.
Basionym

Cenorbiculus centriperforatus Burns, 1976

Synonyms

Discorhabdus hannibalis Aguado, 2012

Holotype

Size: 5.0 µm; number of segments in the distal shield: ¬12

Optical Properties

In plan view under XPL, the distal shield is in constant extinction because the optic axis (c-axis) is perpendicular to the microscope stage, whereas the proximal shield displays a white interference colour and exhibits length-fast (–) elongation.

Remarks

The circular placolith has shields composed of approximately 10-16 segments. The tube cycle is indistinct under the light microscope and may be absent.

References

Aguado, R. 2012. Two new Cretaceous calcareous nannofossils from SE Spain and Tunisia. Journal of Nannoplankton Research. 32(2): 53-57.

Burns, D. A. 1976. Nannofossils from the Lower and Upper Cretaceous deposits, Nettleton, Lincolnshire, England. Revista Española de Micropaleontología. 8(2): 279-300.