Original descriptions of taxa. For coccolithophores, and many calcispheres, these are pages from the Farinacci & Howe Catalog of Calcareous Nannofossils. In other cases (e.g. non-calcifying haptophytes) the data is directly compiled on this site. The "Catalogue of Calcareous Nannofossils" was originally compiled by Prof A. Farinacci 1969-1989, since 2000 it has been updated and extended by Richard Howe - see The Farinacci and Howe Catalog - an Introduction.
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Citation: Calcidiscus salomonii da Gama & Varol 2013Taxonomic rank: speciesLanguage: ENDescribed on page(s) : 3Type specimens: Plate 2, figures 13-20Type sample (& lithostrat): Field Sample 458, Hatay, Southern TurkeyType age (chronostrat): NN6Standardised type level: 122_MIDDLE MIOCENEType locality: Hatay, Southern TurkeyType repository: authors collectionRepository Country: USAFarinacci catalog page (& compiler): n/a Current citation: Calcidiscus salomonii da Gama & Varol 2013
Original Description Diagnosis: Small, strictly circular Calcidiscus whose diameter of the central opening is always greater than the width of the shields.
Description: This small species (3-6μm) has a non-birefringent distal shield, a tube cycle and a birefringent monocyclic proximal shield. The diameter of the central area is always greater than the width of the shield. Size: holotype: Maximum diameter: 5.6μm Diameter of the central area: 1.6μm Diameter of the central area in polarised light: 3.6μm Width of the proximal shield: 1.6μm Etymology: In honour of the late Ralph Salomon, nannofossil specialist and very good friend. Extra details from original publication Remarks: Calcidiscus salomonii is distinguished from Calcidiscus tanianus by being much smaller and having a central opening always greater than the width of the shields. In C. tanianus, the central opening is smaller than the width of the shield. Calcidiscus tropicus (Syn. Calcidiscus macintyrei) is similar to C. tanianus but larger (>10μm). C. salomonii differs from Calcidiscus leptoporus by having a central opening, the latter has a closed central area. Some specimens, under polarised light, can artificially resemble Reticulofenestra rotaria, however C. salomonii is non-birefringent, whereas in R. rotaria the distal shield is birefringent. In addition, the Calcidiscus type structure is readily observed under phase contrast in C. salomonii.
Occurrence: C. salomonii is recorded from middle-upper Miocene sediments (Zone NN6 to NN11). It is reported in samples from Turkey, the Indian Ocean, the Gulf of Aden, Nigeria, Angola and offshore Vietnam.
References:
da Gama, R. O. B. P. & Varol, O. (2013). New Late Oligocene to Miocene Species. Journal of Nannoplankton Research. 33(1): 1-12. gs
Calcidiscus salomonii: Catalog entry compiled by Jeremy Young. Viewed: 8-2-2026