From Suzuki Paleotax db:
1969 Cromyatractus elegans Dogiel n. sp. Petrushevskaya p. 138, pl. 4, fig. 2
1973 Cromyatractus elegans Dogiel Dumitrica p. 834, pl. 20, fig. 8
1984 Ellipsoxiphium palliatum Haeckel [nomen nudum] Nishimura & Yamauchi p. 23, pl. 5, figs. 4, 5, pl. 51, figs. 5a, 5b
1991 Ellipsoxiphium palliatum Haecker [sic] Takahashi p. 75-76, pl. 14, figs. 11-17
Catalog entries: Cromyatractus elegans
Original description: Very elegant representative of the genus, with 4 lattice ellipsoidal shells. Longitudinal axis of the internal ellipsoid: 20µm, of the second shell: 55µm, of the third shell 140µm, of the cortical shell 160µm. Small axis of the cortical shell 150µm. The ellipsoid shell is, thus, slightly elongated. Polar spines round, smooth, without sides, of a length of 60µm, and with a basis as broad as 12µm. Third shell robust, with regularly distributed pores of 9-10µm diameter, shaped as 6-sided funnels. On the sides of the funnels there are small delicate spines that give at a distance of 15µm some tangential apophyses that are anastomosed in a fine superficial network shaped as a spider web. (In Russian. Translated by J.P.C.)
Remarks on original description: [Described by Petrushevskaya after the papers left by Dogel.]
Geological Range:
Last occurrence (top): within Neogene Period (2.59-23.03Ma, top in Piacenzian stage). Data source: Lazarus et al. 2015 - "N age group"
First occurrence (base): within Neogene Period (2.59-23.03Ma, base in Aquitanian stage). Data source: Lazarus et al. 2015 - "N age group"
Plot of occurrence data:
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Cromyatractus elegans compiled by the radiolaria@mikrotax project team viewed: 21-6-2025
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