Set number: 2919

  • Chiastozygus fessus 13956 1
  • Chiastozygus fessus 13961 2
  • Chiastozygus fessus 13965 3
  • Chiastozygus fessus 13952 4
  • Chiastozygus fessus 13957 5
  • Chiastozygus fessus 13962 6
  • Chiastozygus fessus 13966 7
  • Chiastozygus fessus 13953 8
  • Chiastozygus fessus 13960 9
  • Chiastozygus fessus 13964 10
  • Chiastozygus fessus 13968 11
  • Chiastozygus fessus 13954 12
  • Chiastozygus fessus 13959 13
  • Chiastozygus fessus 13963 14
  • Chiastozygus fessus 13967 15
  • Chiastozygus fessus 13955 16
    10µm
Chiastozygus litterarius, Late Campanian, DSDP Leg 25, Site 249, Mozambique Channel (Davie Ridge), Indian Ocean

Set number: 2924

  • Chiastozygus fessus 3932 1
  • Chiastozygus fessus 3931 2
  • Chiastozygus fessus 3929 3
  • Chiastozygus fessus 3930 4
    10µm
Chiastozygus litterarius, Late Campanian, The specific location cannot be disclosed.
Final Epithet
Chiastozygus litterarius (Górka, 1957) (Reinhardt & Górka, 1967) Manivit, 1971
Basionym

Discolithus litterarius Górka, 1957

Synonyms

sensu Chiastozygus litterarius Bown et al. in Bown 1998; Pl. 5.7, Fig.3

sensu Chiastozygus litterarius Burnett in Bown 1998; Pl. 6.3, Fig.5

sensu Chiastozygus fessus Salomon, 1999; The Calcite Palace. Website

sensu Chiastozygus litterarius Lees & Bown, 2005; Pl.1, Figs. 25-26.

sensu Chiastozygus litterarius Kanungo et al., 2020; Fig.4.1

Holotype

Lectotype: Zygolithus litterarius (Górka, 1957) Reinhardt & Górka, 1967

Description

Species of Chiastozygus are characterised by a single wall and a proto inner wall enclosing a broad central area traversed by a symmetrical diagonal cross with widened, thickened termini adjacent to the wall. Each cross arm consists of three longitudinal rows of segments, with the median row positioned slightly distal to the bordering rows. This arrangement produces a subtle but consistent relief differentiation, visible in bright-field images.

Optical Properties

In plan view under crossed polars, the wall and proto inner wall remain in constant extinction, indicating that the optic axis (c-axis) is oriented perpendicular to the microscope stage. Within the crossbars, the median row of longitudinal segments is optically distinct from the bordering rows and exhibits symmetrical extinction at an angle of approximately 45°. The thickened termini of the diagonal cross display interference colours.

Remarks

The similar forms are commonly assigned to Chiastozygus litterarius (see synonymy), although their conformity with the lectotype designated by Reinhardt & Górka (1967) remains uncertain.

References

Bown, P. R. & Cooper, M. K. E. 1998. Jurassic. In: Bown, P. R. (Ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series. 34-85.

Burnett, J. A. 1998. Upper Cretaceous. In: Bown, P. R. (Ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series. 132-199.

Górka, H. 1957. Les Coccolithophoridés du Maestrichtien supérieur de Pologne. Acta Palaeontologica Polonica. 2: 239-284

Kanungo, S., Bown, P. R. & Gale, A. S. 2020. Cretaceous (Albian-Turonian) calcareous nannofossil biostratigraphy of the onshore Cauvery Basin, southeastern India. Cretaceous Research. 118 (2021): 1-22

Lees, J.A., Bown, P.R. 2005. Upper Cretaceous calcareous nannofossil biostratigraphy, ODP Leg 198 (Shatsky Rise, Northwest Pacific Ocean). Proceedings of the Ocean Drilling Program. Scientific Results. 198: 1-60.

Manivit, H. 1971. Nannofossiles calcaires du Crétacé francais (Aptien-Maestrichtien). Essai de Biozonation appuyée sur les stratotypes. PhD thesis, Université de Paris pp. ?-?

Reinhardt, P. & Górka, H. 1967. Revision of some Upper Cretaceous Coccoliths from Poland and Germany. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen. 129(3): 240-256.

Salomon, R. 1999. The Calcite Palace. Website - https://ina.tmsoc.org/gallerie