Discoaster variabilis Martini and Bramlette, 1963
Description: 6-rayed discoaster with birfucate tips; central-area with proximal and distal ridges, but weak bosses. Bifurcations well developed. Slightly concavo-convex and proximal and distal sides well-differentiated.
Remarks: D. variabilis differs from D. exilis primarily in having stronger differentiation of the proximal and distal surfaces, and stronger bifurcations. On the distal side there is normally a distinct central area, with scalloped depressions on the beginning of each ray, and often a central boss, mid-Miocene discoasters rarely have well-developed distal areas of this type.
According to Young (1998) D. variabilis evolved from D. exilis during the early Late Miocene (NN9-10), but the first occurrence is gradational, and of no use for high resolution biostratigraphy. By contrast, Prins (1971) and Theodoridis (1984), derive D. variabilis directly from the D. deflandrei group, and record it throughout the Middle Miocene.
D. variabilis varies considerably (hence the name) in form, in particular the bifurcations vary considerably in length, from less than the width of the ray to two or three times it. Several variants have been described as species or subspecies, as listed below.
Original description:
Variants:
Neogene: Discoaster; Discoaster variabilis
Discoaster variabilis group
6-rayed discoasters with bifurcations. This is the predominant group of Early and Middle Miocene discoasters. N.B. Asymmetric 5-rayed specimens of all these species occasionally occur, and, especially in the Early Miocene, 7-rayed forms.
The dominant species are succesively D. deflandrei (NN1-5), D. exilis (NN6-10), and D. variabilis + D. surculus (NN10-16) but they intergrade and are of limited proven biostratigraphic value, except for the LOs of D. variabilis and D. surculus.
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| D. deflandrei |
D. exilis | D. variabilis |
D. surculus |
The following forms mostly intergrade with the dominant Discoaster species but represent distinctive end-member morphologies which are of biostratigraphic value:
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- asymmetric bifurcations (NN10-11A) |
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- wide central area and large bosses (NN8-9) |
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- wide flat central area, short free rays with notched tips (NN7) |
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D. musicus (variant D. sanmiguelensis - wide central area with large distal boss and sutural ridges (NN5-6) |
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- large distal and proximal bosses, triangular bifuractions (NN4-5) |
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- large variant of D. deflandrei (NN2-3) |
NB Discussion of species concepts in this group is very welcome.
Mike Styzen - In the GOM D. sanmiguelensis is used as a marker and is distinguished as being somewhat smaller than D. musicus with shorter rays. One might argue that what we're using is just a specific morphotype of D. musicus, but in any case it's a distinction that has stratigraphic function. Richard Howe was kind enough to let me use an image of our D. sanmiguelensis concept.
Neogene: D. variabilis group; Discoaster variabilis
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: