Daughter taxa (time control age-window is: 0-800Ma) | ||||
Plectodiscus bergontianus neptune records: | ||||
Plectodiscus sp. neptune records: |
Catalog entries: Plectodiscus
Original description: Thin, biconvex skeleton, with oval, less frequently circular outline, consisting of frontal, equatorial, and sagittal girdles. The closed-spiral structure of girdles is of the Spironium type: wings of the same type of girdle form a one-half turn of the spiral, and at the point of their junction overlap each other. Fist system has fully developed girdles, its dimensions are 40-50µm; in the rest of the girdles only the equatorial girdle is fully developed, both sagittal and frontal girdles terminating at the point of their junction with the previous system. Distance between rings is greater than is the diameter of the central chamber. Inner spines are indistinct; rim of the disc is smooth or is covered by numerous short spines.
Depending on the degree of inclination of the plane of the girdles in relation to the main axes of the skeleton, the equatorial girdles appear from the surface (rest of girdles in corresponding cross-section) in the form of rings, as a single or double spiral, or in the form of rings connected by zigzag radial lines.
Geological Range:
Last occurrence (top): at top of Neogene Period (100% up, 2.6Ma, in Piacenzian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within Neogene Period (2.59-23.03Ma, base in Aquitanian stage). Data source: Total of ranges of species in this database
Plot of occurrence data:
Plectodiscus compiled by the radiolaria@mikrotax project team viewed: 20-9-2024
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