FAMILY DISCOASTERACEAE TAN, 1927
Description. Discoidal nannoliths of 3-40 elements radiating from a common centre. C-axes vertical, so nannoliths appear dark in plane-polarised light. Some early forms also include a cycle of birefringent units.
Taxa included: Discoaster, Catinaster.
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6-rayed discoasters with bifurcations. |
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Discoaster brouweri group 6-rayed discoasters without bifurcations, and forms closely related to D. brouweri with 3 to 5 rays |
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Discoaster pentaradiatus group symmetric 5-rayed discoasters |
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6-rayed discosters in which the birfurcations meet to form a rim, which extends proximally |
Original description:
Nannoliths - informal grouping. Used here in the sense of Young & Bown (1987)
Description - the following groups of Neogene nannofossils are thought to be related to coccolithophores, but produce structures which are neither heterococcoliths nor holococcoliths.
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| Braarudosphaeraceae | Ceratolithaceae | Discoasteraceae | Sphenolithaceae | Triquetrorhabdulaceae |
The term nannolith has been used, especially by palaeontologists, as a convenient term for structures about the same size as coccoliths and occurring with coccoliths, but lacking definite coccolith affinities. In the modern nannoflora, there are fewer groups of cryptic origins, and the term has been less widely used. However, it is useful for calcareous structures that are thought to be formed by haptophytes, but probably by a different biomineralisation process to either heterococcoliths or holococcoliths (Young et al. 1999).
NB The first use of the term in this sense appears to have been by Haq (1978, in Introduction to Marine Micropaleontology), and this was followed by Perch-Nielsen (1985, in Plankton Stratigraphy). By contrast, Aubry (1988 et seq., Handbook of Calcareous Nannofossils) places most of these groups in the Ortholithae.