Set number: 906

  • Sphenolithus philippinensis 27834 1
  • Sphenolithus philippinensis 27831 2
  • Sphenolithus philippinensis 27836 3
  • Sphenolithus philippinensis 27833 4
  • Sphenolithus philippinensis 27832 5
  • Sphenolithus philippinensis 27835 6
    10µm
Sphenolithus philippinensis, Early Miocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean

Set number: 905

  • Sphenolithus philippinensis 193 1
  • Sphenolithus philippinensis 192 2
  • Sphenolithus philippinensis 190 3
  • Sphenolithus philippinensis 191 4
    10µm
Sphenolithus philippinensis, Early Oligocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean

Set number: 903

  • Sphenolithus cf dissimilis 189 1
  • Sphenolithus cf dissimilis 188 2
  • Sphenolithus cf dissimilis 187 3
  • Sphenolithus cf dissimilis 186 4
    10µm
Sphenolithus philippinensis, Early Oligocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean
Final Epithet
Sphenolithus philippinensis Varol, in prep.
Basionym

Sphenolithus philippinensis Varol, in prep.

Etymology

After the Philippines, where I first noted this species.

Description

Medium to large size (>5.0µm), elongated cylindrical species of Sphenolithus Deflandre in Grassé, 1952 having segments arranged in three cycles. The cylindrical proximal cycle predominates the low lateral cycle and the diminutive biconical clustered apical spine. In cross-polarised light, the apical spine is extinct (dim) at 0° and shows maximum birefringence at 45°.

In the axial section, the inner ends of the segments in the proximal cycle joined most of their length along the longitudinal axis but not joined nearer the proximal end thus creating a shallow conical proximal cavity.

Remarks

Sphenolithus philippinensis is easy to identify from Sphenolithus disbelemnos Fornaciari & Rio, 1996 by being larger and having a biconical clustered apical spine whereas the latter has a bouquet shape clustered apical cycle.

Sphenolithus philippinensis differ from Sphenolithus quasibelemnos Varol, in prep. by being larger and cylindrical whereas the latter has a triangular shape in the axial section.

References

Deflandre, G., 1952. Classe des Coccolithophoridés. (Coccolithophoridae. Lohmann, 1902). In: Grassé, P. P. (ed.), Traité de Zoologie. Masson, Paris 439-470.

Fornaciari, E., Rio, D., 1996. Latest Oligocene to early Middle Miocene quantitative calcareous nannofossil biostratigraphy in the Mediterranean region. Micropaleontology 42(1), 1-37