Set number: 1744

  • Cyclagelosphaera paez rayesii 67311 1
  • Cyclagelosphaera paez rayesii 67312 2
  • Cyclagelosphaera paez rayesii 67316 3
  • Cyclagelosphaera paez rayesii 67315 4
  • Cyclagelosphaera paez rayesii 67318 5
  • Cyclagelosphaera paez rayesii 67319 6
  • Cyclagelosphaera paez rayesii 67317 7
  • Cyclagelosphaera paez rayesii 67320 8
  • Cyclagelosphaera paez rayesii 67307 9
  • Cyclagelosphaera paez rayesii 67306 10
  • Cyclagelosphaera paez rayesii 67295 11
  • Cyclagelosphaera paez rayesii 67298 12
  • Cyclagelosphaera paez rayesii 67308 13
  • Cyclagelosphaera paez rayesii 67305 14
  • Cyclagelosphaera paez rayesii 67296 15
  • Cyclagelosphaera paez rayesii 67297 16
  • Cyclagelosphaera paez rayesii 67302 17
  • Cyclagelosphaera paez rayesii 67303 18
  • Cyclagelosphaera paez rayesii 67299 19
  • Cyclagelosphaera paez rayesii 67310 20
  • Cyclagelosphaera paez rayesii 67304 21
  • Cyclagelosphaera paez rayesii 67301 22
  • Cyclagelosphaera paez rayesii 67309 23
  • Cyclagelosphaera paez rayesii 67300 24
    10µm
DSDP Leg 25, Site 245, Mozambique Channel (Davie Ridge), Indian Ocean

Holotype, in the mobile mount

Final Epithet
Cyclagelosphaera paez-rayesii Varol, 2025
Basionym

Cyclagelosphaera paez-rayesii Varol, 2025

Diagnosis

Circular placoliths have equal-diameter, single-tiered concave-convex distal and proximal shields, along with a double tube cycle that protrudes distally, leaving a narrow open central area.

Etymology

In honour of Dr M. Paez-Rayes, Bogota, Colombia, in recognition of his contributions to the stratigraphy and geology of Colombia.

Dimensions Of Holotype

Diameter of shields = 6.76 μm; Width of tube cycle = 0.97 μm; Width of central opening = 1.06 μm; Thickness = 3.14 μm.

Description

Optical Properties: In the plan view, all except the outer tube cycle exhibit inclined extinction lines, displaying length-fast (-) elongation. The extinction lines are dextrogyre on the distal side, and their typical angles are typically around 73° on the distal shield and 53° on the tube cycles on the distal side. These measurements of the tube cycle differ from those of Cyclagelosphaera species from the Cretaceous period. In the plan view, the outer tube cycle remains in constant extinction because the optic and c-axis are vertical relative to the microscope stage.

Remarks

Cyclagelosphaera paez-rayesii is the only species of Cyclagelosphaera with an open central area in Paleocene sediments. Cyclagelosphaera jiangii and Cyclagelosphaera lacuna also have an open central area but are restricted to Early Cretaceous and Jurassic sediments, respectively.

References

Varol, O. 2025a. A practical guide to optical studies of calcareous nannofossils. Grzybowski Foundation Special Publication. 29: 1-222