Set number: 2325

  • Bomolithus elegans 62321 1
  • Bomolithus elegans 62318 2
  • Bomolithus elegans 62325 3
  • Bomolithus elegans 62352 4
  • Bomolithus elegans 62320 5
  • Bomolithus elegans 62324 6
  • Bomolithus elegans 62319 7
  • Bomolithus elegans 62354 8
  • Bomolithus elegans 62334 9
  • Bomolithus elegans 62333 10
  • Bomolithus elegans 62338 11
  • Bomolithus elegans 62349 12
  • Bomolithus elegans 62335 13
  • Bomolithus elegans 62332 14
  • Bomolithus elegans 62339 15
  • Bomolithus elegans 62348 16
  • Bomolithus elegans 62330 17
  • Bomolithus elegans 62331 18
  • Bomolithus elegans 62337 19
  • Bomolithus elegans 62336 20
  • Bomolithus elegans 62356 21
  • Bomolithus elegans 62355 22
  • Bomolithus elegans 62351 23
    10µm
Bomolithus elegans, Late Paleocene, DSDP Leg 25, Site 245, Mozambique Channel (Davie Ridge), Indian Ocean
Final Epithet
Bomolithus elegans Roth, 1973
Basionym

Bomolithus elegans Roth, 1973

Description

Emended by Bowman & Varol, 2021: Medium size (5.5–8.0μm) circular species of Bomolithus consisting of two discs and a column. The discs are equal (or approximately equal) in diameter and appear relatively flat to very slightly convex (clearly seen in the side-view). The segments of the median disc are “wedge-shaped” in the side-view. The high column is wide and parallel-sided or cylindrical and possesses a cone-like distal depression and a narrow canal that is closed with a central plug. The discs and column contain a similar number of segments (about 24–32), and the width of the disc segments is much broader than the width of the column segments.

Optical Properties

In plan view, the discs appear a shade of white, the column appears shades of yellow, and the plug is smooth with unresolvable segments. In the distal view, the extinction lines are dextrogyre, whereas the extinction lines are laevogyre in the proximal view. When viewed using a gypsum plate, the horizontal axis of the coccolith lies within the blue sector on the distal/column-side. Still, the vertical axis of the coccolith lies within the blue sector on the proximal/disc side. The discs and column are birefringent in plan view and side view.

Remarks

The wedge-shaped character of the median disk (as seen in the side-view) is most apparent in this species of Bomolithus. The relatively high column of Bomolithus is the diagnostic criterion for separating it from Heliotrochus. Bomolithus elegans possesses discs of equal or almost equal diameter, whereas the discs of Bomolithus cantabriae are of unequal diameter (the median disc is much narrower). The column of Bomolithus elegans is high and cylindrical, but the column of Bomolithus dydimolofous appears relatively low and dome-shaped. In the side-view, the median disc of Bomolithus elegans appears wedge-like, whereas Bomolithus dydimolofous possesses a lath-like median disc. In plan-view, the number of segments characterising Bomolithus elegans (about 24–32) is less than the number of segments representing Bomolithus dydimolofous (about 32–40). The disc and column segments are unequal in Bomolithus elegans (disc segments are much broader than column segments). In contrast, the disc and column segments are of approximately equal width in Bomolithus dydimolofous.

References

Bowman, A. R. & Varol, O. 2021. A Taxonomic Revision of Heliolithaceae - Applications in Resolving the Problematic Calcareous Nannofossil Biostratigraphy of the Paleocene. In: M. Montenary, M. (Ed.). Calcareous nannofossil biostratigraphy of the Stratigraphy and timescales. 6: 43-223.

Roth, P. H. 1973. Calcareous nannofossils: Leg 17 of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project. 17: 695-795.