Set number: 3097

  • Helenea acuminata 3530 1
  • Helenea acuminata 3529 2
  • Helenea acuminata 3527 3
  • Helenea acuminata 3528 4
    10µm
Helenea acuminata, Early Valanginian, DSDP Leg 76, Site 534, Blake-Bahama Basin, Atlantic Ocean

Set number: 3096

  • Helenea acuminata 2648 1
  • Helenea acuminata 2651 2
  • Helenea acuminata 2652 3
  • Helenea acuminata 2649 4
  • Helenea acuminata 2650 5
  • Helenea acuminata 2653 6
    10µm
Helenea acuminata, Late Aptian, Gargas, SE France

Set number: 3101

  • Helenea acuminata 2628 1
  • Helenea acuminata 2627 2
  • Helenea acuminata 2625 3
  • Helenea acuminata 2626 4
    10µm
Helenea acuminata, Late Aptian, Gargas, SE France

Set number: 3100

  • Helenea acuminata 2607 1
  • Helenea acuminata 2608 2
  • Helenea acuminata 2610 3
  • Helenea acuminata 2609 4
    10µm
Helenea acuminata, Late Aptian, Gargas, SE France

Set number: 3109

  • Helenea cf acuminata 1284 1
  • Helenea cf acuminata 1285 2
    10µm
Helenea acuminata, Late Hauterivian, Mississippi Canyon, Gulf of Mexico

small form

Final Epithet
Helenea acuminata Varol, in prep.
Basionym

Helenea acuminata Varol, in prep.

Etymology

From the Latin acuminata, meaning “pointed”, referring to the pointed ends of the arms of the central cross.

Dimensions Of Holotype

Length: 7.35 µm; width: 6.43 µm; width of the pelaga: 1.94 µm; width of the central area: 2.55 µm; ellipticity: 1.14.

Description

Subcircular species (ellipticity: <1.15) of Helenea are characterised by an axial cross that may be slightly rotated relative to the axis of the placolith. The arms of the cross have pointed terminations and support a short distal process with a distinct square-shaped termination.

Optical Properties

Optical properties consistent with those of Helenea.

Remarks

Helenea acuminata is distinguished from Helenea chiasta and Helenea staurolithina by its subcircular outline and by having a central cross with arms terminating in blunt points. The latter species has an elliptical outline (ellipticity approximately 1.25) and a central cross with arms that terminate in bifurcations, without forming additional pores.

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.