Set number: 892

  • Sphenolithus compactus 125 1
  • Sphenolithus compactus 124 2
  • Sphenolithus compactus 123 3
  • Sphenolithus compactus 122 4
    10µm
Sphenolithus compactus, Early Miocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean

Set number: 867

  • Sphenolithus compactus 89 1
  • Sphenolithus compactus 90 2
  • Sphenolithus compactus 87 3
  • Sphenolithus compactus 88 4
    10µm
Sphenolithus compactus, Early Miocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean

Set number: 891

  • Sphenolithus disbelemnos 116 1
  • Sphenolithus disbelemnos 115 2
  • Sphenolithus disbelemnos 113 3
  • Sphenolithus disbelemnos 114 4
    10µm
Sphenolithus disbelemnos_Sphenolithus_compactus, Early Miocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean

Set number: 921

  • Sphenolithus tintinnabulum 80 1
  • Sphenolithus tintinnabulum 81 2
  • Sphenolithus tintinnabulum 78 3
  • Sphenolithus tintinnabulum 79 4
    10µm
Sphenolithus compactus, Early Miocene, DSDP Leg 25, Site 242, Mozambique Channel (Davie Ridge), Indian Ocean
Final Epithet
Sphenolithus compactus Backman, 1980
Basionym

Sphenolithus compactus Backman, 1980

Synonyms

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

Holotype

The precise age of the holotype sample was obtained from the chart provided by Perch-Nielsen, 1972b.

Description

Very small (2.0-4.0µm), elongated species of Sphenolithus Deflandre in Grassé, 1952 having a diminutive clustered apical cycle resembles a bouquet of flower at 45° [its segments radiating outward distally]. The apical cycle shows maximum birefringence at 45° but extinct (dim) at 0° (parallel extinction).

The lateral cycle is diminutive and its segments are aligned longitudinally at 0° in cross-polarised light.

The height of the elongated cylindrical proximal cycle with a concave base is always distinctly greater than the height of the apical cycle.

In the cylindrical proximal cycle, the inner ends of segments joined most of their length along the longitudinal axis but not joined nearer the proximal end thus forming a very shallow conical proximal cavity.

In the light microscope, in the axial section, the segments of the proximal cycle are irregular quadrilateral.

Remarks

Sphenolithus compactus differs from Sphenolithus disbelemnos Fornaciari and Rio,1996 by being smaller than 3.0µm.

Sphenolithus compactus is distinguished from Sphenolithus tintinnabulum Maiorano & Monechi 1997 by having a cylindrical proximal cycle. In contrast, the latter has a frustum shape proximal cycle, thus producing a truncated triangular appearance in the axial section.

References

Backman, J., 1980. Miocene-Pliocene nannofossils and sedimentation rates in the Hatton-Rockall Basin, NE Atlantic Ocean. Stockholm Contributions in Geology 36, 1-91.

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.

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

Maiorano, P., Monechi, S., 1997. New Early Miocene species of Sphenolithus Deflandre, 1952 from the North Atlantic Ocean. Journal of Nannoplankton Research 19(2), 103-107.

Perch-Nielsen, K., 1972b. Remarks on Late Cretaceous to Pleistocene coccoliths from the North Atlantic. Initial Reports of the Deep Sea Drilling Project 12, 1003-1069.