Set number: 801

  • Helicosphaera carteri 47205 1
  • Helicosphaera carteri 47208 2
  • Helicosphaera carteri 47212 3
  • Helicosphaera carteri 47201 4
  • Helicosphaera carteri 47206 5
  • Helicosphaera carteri 47207 6
  • Helicosphaera carteri 47210 7
  • Helicosphaera carteri 47199 8
  • Helicosphaera carteri 47197 9
  • Helicosphaera carteri 47202 10
  • Helicosphaera carteri 47204 11
  • Helicosphaera carteri 47203 12
  • Helicosphaera carteri 47200 13
  • Helicosphaera carteri 47198 14
    10µm
Helicosphaera kamptneri, Late Miocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean

in mobile mount

Set number: 463

  • Helicosphaera carteri kamptneri VR 05342 1
  • Helicosphaera carteri kamptneri VR 05351 2
  • Helicosphaera carteri kamptneri VR 05343 3
  • Helicosphaera carteri kamptneri VR 05350 4
  • Helicosphaera carteri kamptneri VR 05341 5
  • Helicosphaera carteri kamptneri VR 05340 6
  • Helicosphaera carteri kamptneri VR 05344 7
  • Helicosphaera carteri kamptneri VR 05349 8
  • Helicosphaera carteri kamptneri VR 05347 9
  • Helicosphaera carteri kamptneri VR 05346 10
  • Helicosphaera carteri kamptneri VR 05345 11
  • Helicosphaera carteri kamptneri VR 05348 12
    10µm
Helicosphaera kamptneri, Middle Pleistocene, DSDP Leg 23, Site 229A, Red Sea
Final Epithet
Helicosphaera kamptneri (Hay & Mohler, 1967) Locker, 1973
Basionym

Helicopontosphaera kamptneri Hay & Mohler, 1967

Remarks

A helicolith with a Type III (Helicosphaera carteri type) blanket, an expanded flange termination, and a central area featuring tiny pores hardly visible. Helicosphaera kamptneri differs from Helicosphaera carteri and Helicosphaera epimikeisporous by its tiny pores. It is distinguished from Helicosphaera paleocarteri and Helicosphaera dyotrypes by having both tiny pores aligned along the axial suture. In Helicosphaera
paleocarteri
, both pores aligned off the longitudinal suture, and in Helicosphaera dyotrypes, only one of the pores aligned with the axial suture. Helicosphaera kamptneri exhibits inclined extinction angles of about 52° on the blanket on the distal side and shows length-fast (−) elongation.

References

Hay, W. W., Mohler, H. P., 1967, Calcareous nannoplankton from Early Tertiary rocks at Point Labau, France and Paleocene-Early Eocene correlations. Journal of Paleontology 41(6), 1505-1541.