Heliodiscus riedeli, Dumitrica, 2019
publication ID |
https://doi.org/ 10.35463/j.apr.2019.01.04 |
DOI |
https://doi.org/10.5281/zenodo.10520630 |
persistent identifier |
https://treatment.plazi.org/id/1F21C405-C343-FF82-3D28-C9CDB0DDA14D |
treatment provided by |
Felipe |
scientific name |
Heliodiscus riedeli |
status |
sp. nov. |
Heliodiscus riedeli nov. sp.
Figures 8b, e, f View Fig ; 9a View Fig
Description. Shell large, disc-shaped with a small double medullary shell and a wide cortical shell. Microsphere very small, eccentric in the outer medullary shell and connected to it through a few cylindrical beams of different length. Outer medullary shell spherical or slightly prunoid with wide circular or polygonal pores separated by thin intervening bars and included in the cavity of the cortical shell to which it is connected with the two faces of this shell by a bunch of very short rays. Cortical shell flat, very thin and perforated by numerous very small polygonal pores arranged either disorderly or, partly, radially. Periphery of disc armed with numerous threebladed, short, and pyramidal spines disposed in several planes.
Material. Eight specimens in sample PROA 96 P, 241- 243 cm, late middle Miocene .
Holotype. Figure 8b View Fig , coll. MGL 103559 View Materials .
Dimensions. Diameter of microsphere 17-19 μm, of outer medullary shell 47-54 μm, of cortical shell 241-295 μm.
Etymology. The species is named for William R. Riedel for his great contribution to the study of Cenozoic radiolarians. It is also in the sample provided by him that this species was found.
Remarks. This species differs from all the other species of this genus in having a large, completely flat disc-shaped cortical shell and many short pyramidal spines on periphery.
Range and occurrences. Late middle Miocene, central Pacific.
R |
Departamento de Geologia, Universidad de Chile |
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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