6-rayed discoasters with bifurcations. This is the predominant group of Neogene 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 small er 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.
Jeremy Young - I have
Jeremy Young - I have amended this page by adding the tables so it can act as a sort of key to the taxa
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