Set number: 800

  • Zygrhablithus bijugatus 49341 1
  • Zygrhablithus bijugatus 49339 2
  • Zygrhablithus bijugatus 49346 3
  • Zygrhablithus bijugatus 49343 4
  • Zygrhablithus bijugatus 49342 5
  • Zygrhablithus bijugatus 49340 6
  • Zygrhablithus bijugatus 49347 7
  • Zygrhablithus bijugatus 49344 8
    10µm
Zygrablithus bijugatus, Early Eocene, Santos Basin, Brazil

Set number: 798

  • Zygrablithus bijugatus S6 5 1
  • Zygrhablithus bijugatus S3a 17 2
  • Zygrablithus bijugatus S9 26 3
  • Zygrhablithus bijugatus S7 14 4
  • Zygrablithus bijugatus S9 21 5
  • Zygrablithus bijugatus S3a 20 6
  • Zygrablithus bijugatus S6 6 7
Zygrhablithus bijugatus, Early Eocene, Sile, Northern Turkey
Final Epithet
Zygrhablithus bijugatus (Deflandre in Deflandre & Fert, 1954) Deflandre, 1959
Basionym

Zygolithus bijugatus Deflandre in Deflandre & Fert, 1954 [Invalid ICN Art. 35.1] but valid according to ICZN.

Synonyms

Zygrhablithus bijugatus (Deflandre in Deflandre & Fert, 1954) Deflandre, 1959

Pseudozygrhablithus altus Haq, 1971

Pseudozygrhablithus latus Haq, 1971

Semihololithus kerabyi Perch-Nielsen, 1971

Variants

Rhabdolithus costatus Deflandre in Deflandre & Fert, (1954) = Zygrhablithus bijugatus maximus Bown (2010); having a large distal process

Zygrhablithus bijugatus crassus Locker (1967); having a short, truncated distal process

Zygrhablithus bijugatus cornutus Bown (2005); having short lateral protrusions or horns at its distal end

Description

Medium to large spinose holococcolith having a proximal base and a distal process. The distal process has four quadrants divided by X-shape septa [can be seen in plan view] and tapering uniformly to blunt termination.

The base has a large cavity that opens proximally, whilst the distal process has a narrow axial canal. The entire specimen is birefringent at the side view

Remarks

Zygrhablithus bijugatus is distinguished from Zygrhablithus sileensis Varol (1989) by lacking cone shape termination.

References

Bown, P. R., (2005): Palaeogene calcareous nannofossils from the Kilwa and Lindi areas of coastal Tanzania (Tanzania Drilling Project 2003-4). - Journal of Nannoplankton Research. 27(1): 21-95.

Bown, P. R., (2010): Calcareous nannofossils from the Paleocene/Eocene Thermal Maximum interval of southern Tanzania (TDP Site 14). - Journal of Nannoplankton Research. 31(1): 11-38.

Deflandre, G. & Fert, C., (1954): Observations sur les coccolithophoridés actuels et fossiles en microscopie ordinaire et électronique. - Annales de Paléontologie. 40: 115-176.

Deflandre, G., (1959): Sur les nannofossiles calcaires et leur systématique. - Revue de Micropaléontologie. 2: 127-152.

Haq, B. U., (1971): Paleogene calcareous nannoflora. Parts I-IV. - Stockholm Contributions in Geology. 25: 1-158.

Locker, S., (1967):. Neue, statigraphisch wichtige Coccolithophoriden (Flagellata aus dem norddeutschen Altetiar). - Monatsberichte der Deutschen Akademie der Wissenschaften zu Berlin. 9(9-10): 758-769.

Perch-Nielsen, K., (1971): Einige neue Coccolithen aus dem Paläozän der Bucht von Biskaya und dem Eozän der Labrador See. - Bulletin of the Geological Society of Denmark. 21: 347-361.

Varol, O., (1989): Eocene calcareous nannofossils from Sile (northwest Turkey). - Revista Española de Micropaleontología. 21: 273-320