Set number: 4611

  • Sphenolithus apoxis VR 31144 1
  • Sphenolithus apoxis VR 31145 2
  • Sphenolithus apoxis VR 31146 3
  • Sphenolithus apoxis VR 31147 4
  • Sphenolithus apoxis VR 31148 5
  • Sphenolithus apoxis VR 31149 6
  • Sphenolithus apoxis VR 31150 7
  • Sphenolithus apoxis VR 31151 8
  • Sphenolithus apoxis VR 31152 9
  • Sphenolithus apoxis VR 31153 10
  • Sphenolithus apoxis VR 31154 11
  • Sphenolithus apoxis VR 31155 12
  • Sphenolithus apoxis VR 31156 13
  • Sphenolithus apoxis VR 31157 14
  • Sphenolithus apoxis VR 31158 15
  • Sphenolithus apoxis VR 31159 16
  • Sphenolithus apoxis VR 31160 17
  • Sphenolithus apoxis VR 31161 18
  • Sphenolithus apoxis VR 31162 19
  • Sphenolithus apoxis VR 31163 20
  • Sphenolithus apoxis VR 31164 21
  • Sphenolithus apoxis VR 31165 22
  • Sphenolithus apoxis VR 31166 23
  • Sphenolithus apoxis VR 31167 24
  • Sphenolithus apoxis VR 31168 25
  • Sphenolithus apoxis VR 31169 26
  • Sphenolithus apoxis VR 31170 27
  • Sphenolithus apoxis VR 31171 28
  • Sphenolithus apoxis VR 31172 29
  • Sphenolithus apoxis VR 31173 30
  • Sphenolithus apoxis VR 31174 31
  • Sphenolithus apoxis VR 31175 32
  • Sphenolithus apoxis VR 31176 33
  • Sphenolithus apoxis VR 31177 34
  • Sphenolithus apoxis VR 31178 35
  • Sphenolithus apoxis VR 31179 36
    10µm
Sphenolithus apoxis, Middle Eocene, DSDP Leg 39, Sites 356, Sào Paulo Plateau, South Atlantic Ocean

Set number: 866

  • Sphenolithus apoxis 28026 1
  • Sphenolithus apoxis 28024 2
  • Sphenolithus apoxis 28028 3
  • Sphenolithus apoxis 28032 4
  • Sphenolithus apoxis 28027 5
  • Sphenolithus apoxis 28025 6
  • Sphenolithus apoxis 28029 7
  • Sphenolithus apoxis 28030 8
    10µm
Sphenolithus apoxis, Early Oligocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean

Set number: 863

  • Sphenolithus apoxis 76 1
  • Sphenolithus apoxis 77 2
  • Sphenolithus apoxis 74 3
  • Sphenolithus apoxis 75 4
    10µm
Sphenolithus apoxis, Early Miocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean

Set number: 864

  • Sphenolithus apoxis 97 1
  • Sphenolithus apoxis 98 2
  • Sphenolithus apoxis 95 3
  • Sphenolithus apoxis 96 4
    10µm
Sphenolithus apoxis, Early Miocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean

Set number: 865

  • Sphenolithus apoxis 28105 1
  • Sphenolithus apoxis 28102 2
  • Sphenolithus apoxis 28106 3
  • Sphenolithus apoxis 28110 4
  • Sphenolithus apoxis 28104 5
  • Sphenolithus apoxis 28103 6
  • Sphenolithus apoxis 28107 7
  • Sphenolithus apoxis 28109 8
    10µm
Sphenolithus apoxis, Late Oligocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean

Set number: 920

  • Sphenolithus tintinnabulum 2315 1
  • Sphenolithus tintinnabulum 2314 2
  • Sphenolithus tintinnabulum 2312 3
  • Sphenolithus tintinnabulum 2313 4
    10µm
Sphenolithus apoxis, Late Oligocene, Angola, West Africa
Final Epithet
Sphenolithus apoxis Bergen & de Kaenel in Bergen et al., 2017
Basionym

Sphenolithus apoxis Bergen & de Kaenel in Bergen et al., 2017

Description

The dome shape Sphenolithus Deflandre in Grassé (1952) is taller than wider and has three cycles of segments (proximal, lateral and apical).

The longitudinal extinction line is evident at 0° and always greater than the lateral extinction line. Entirely birefringent species at side and plan views.

The three cycles can be better seen in well-preserved specimens at 45° with the help of the gypsum plate.

The bouquet shape clustered apical cycle with axial c-axis is not forming a true apical spine.

The hollow frustum shape proximal cycle is creating a conical proximal cavity. The opposite side of the proximal cycle is better seen at 45° and displays an axial c-axis.

Remarks

Sphenolithus apoxis is difficult to identify consistently from Sphenolithus abies Deflandre, 1953 ex Deflandre in Deflandre & Fert (1954) and Sphenolithus moriformis (Brönnimann & Stradner, 1960) Bramlette & Wilcoxon (1967), particularly at plan view.

The shallower dome shape Sphenolithus moriformis has a longer lateral extinction line than the longitudinal extinction line. Sphenolithus apoxis is taller than wider.

Sphenolithus apoxis has a bouquet shape cluster apical cycle, whereas Sphenolithus abies has a biconical apical cycle best seen at 45°.

Sphenolithus apoxis differ from Sphenolithus alatus Varol, in prep. by having a relatively larger apical cycle, lateral cycle with radial segment and much shallower proximal depression.

References

Bergen, J. A., de Kaenel, E., Blair, S. A., Boesiger, T. M. & Browning, E. 2017. Oligocene-Pliocene taxonomy and stratigraphy of the genus Sphenolithus in the circum North Atlantic Basin: Gulf of Mexico and ODP Leg 154. Journal of Nannoplankton Research 37(2-3): 77-112.

Bramlette, M. N. & Wilcoxon, J. A. 1967. Middle Tertiary calcareous nannoplankton of the Cipero section, Trinidad, W.I. Tulane Studies in Geology and Paleontology 5: 93-131.

Brönnimann, P. & Stradner, H. 1960. Die Foraminiferen- und Discoasteriden-zonen von Kuba und ihre interkontinentale Korrelation. Erdoel-Zeitschrift 76(10): 364-369.

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

Deflandre, G., 1953. Hétérogénéité intrinsèque et pluralité des éleménts dans les coccolithes actuels et fossiles. Comptes Rendus Hebdomadaires des Séances de l'Académie des Sciences, Paris 237, 1785-1787.

Deflandre, G. & Fert, C. 1954. Observations on current and fossil coccolithophorids in ordinary and electron microscopy. Annales de Paléontologie 40: 115-176.