C stavrotos Hattner SEM a

SEM photo of Calculites stavrotos from Hatter & Wise, 1980 (Pl. 27, Fig. 9)

Set number: 3001

  • Calculites stavrotos 15749 1
  • Calculites stavrotos 15745 2
  • Calculites stavrotos 15742 3
  • Calculites stavrotos 15756 4
  • Calculites stavrotos 15750 5
  • Calculites stavrotos 15746 6
  • Calculites stavrotos 15743 7
  • Calculites stavrotos 15755 8
  • Calculites stavrotos 15752 9
  • Calculites stavrotos 15748 10
  • Calculites stavrotos 15744 11
  • Calculites stavrotos 15754 12
  • Calculites stavrotos 15751 13
  • Calculites stavrotos 15747 14
  • Calculites stavrotos 15753 15
    10µm
Calculites stavrotos, Late Campanian, DSDP Leg 36, Site 327A, The Maurice Ewing Bank, Falkland Plateau
Final Epithet
Calculites stavrotos
Basionym

Calculites stavrotos Varol, in prep.

Etymology

From the Greek stavrotos, meaning “cross”, referring to the cross-forming struts that support the distal process.

Description

Elliptical species of Calculites are constructed of a narrow outer wall and four central crystalline blocks that support a large, solid distal process, round in cross-section. The distal process is supported by four to five struts, which produce large depressions between adjacent struts. The scanning electron microscope image illustrated in Plate 27, Figure 9, of Hattner & Wise (1980) provides the best example of this detailed structure.

The sutures between the crystalline blocks meet at the centre, forming a cross that is rotated slightly relative to the long axis of the ellipse.

Optical Properties

In plan view under crossed polars, the outer wall and the crystalline blocks display first-order whitish-yellow interference colours, whereas the distal process exhibits second-order bluish-red interference colours.

Calculites stavrotos exhibits parallel extinction (extinction angle 0°) and length-slow (+) elongation in its natural position.

References

Hattner, J. G. & Wise, S. W. 1980. Upper Cretaceous calcareous nannofossil biostratigraphy of South Carolina. South Carolina Geology 24: 41-117.