Set number: 48

  • Karoulimorfi asynithis 56097 1
  • Karoulimorfi asynithis 56100 2
  • Karoulimorfi asynithis 56124 3
  • Karoulimorfi asynithis 56104 4
  • Karoulimorfi asynithis 56125 5
  • Karoulimorfi asynithis 56099 6
  • Karoulimorfi asynithis 56102 7
  • Karoulimorfi asynithis 56105 8
  • Karoulimorfi asynithis 56117 9
  • Karoulimorfi asynithis 56116 10
  • Karoulimorfi asynithis 56113 11
  • Karoulimorfi asynithis 56103 12
  • Karoulimorfi asynithis 56118 13
  • Karoulimorfi asynithis 56115 14
  • Karoulimorfi asynithis 56114 15
  • Karoulimorfi asynithis 56106 16
  • Karoulimorfi asynithis 56112 17
  • Karoulimorfi asynithis 56111 18
  • Karoulimorfi asynithis 56110 19
  • Karoulimorfi asynithis 56107 20
    10µm
Karoulimorfi asynithis, Early Paleocene, DSDP Leg 25, Site 245A, Mozambique Channel (Davie Ridge), Indian Ocean

in mobile mount

Final Epithet
Karoulimorfi asynithis Varol, in prep.
Basionym

Karoulimorfi asynithis Varol, in prep.

Synonyms

Octolithus - Agnini et al., 2007, pl.1, fig.1

Octolithus-Sphenolithus integrate - Agnini et al., 2007, pl. 1, figs. 2-3.

Diagnosis

Circular species of Karoulimorfi have a reel like core with unequal ends surrounded by several segments.

Etymology

From Greek asynithis, unusual – referring to its unique shape.

Description

The coarse segments surround the distinctly narrower end of the reel, whereas the finely striated rim surrounds the wider end of the reel.

Remarks

Karoulimorfi asynithis is distinguished from Semihololithus by being circular in plan view, whereas the latter is elliptical in plan view. The central core is reel like with unequal ends in Karoulimorfi asynithis, but the central body has segmented only at the one end.

This unusual species is an excellent marker

Occurrence
Worldwide
References

Agnini, C., Fornaciari, E., Raffi, I., Rio, D., Röhl, U. & Westerhold, T., (2007): High-resolution nannofossil biochronology of middle Paleocene to early Eocene at ODP Site 1262: implications for calcareous nannoplankton evolution. - Marine Micropaleontology, 64: 215-248.