1968 Dendrospyris binapertonis - Goll p. 1420; pl. 173, fig. 5, 6, 10, 11
From Suzuki Paleotax db:
1968 Dendrospyris binapertonis n. sp. Goll p. 1420, pl. 173, figs. 5, 6, 10, 11, text-fig. 8
1972 Dendrospyris binapertonis Goll Goll p. 963, pl. 49, figs. 1, 2
1974 Dendrospyris sp. aff. D. binapertonis Goll Renz p. 790, pl. 19, fig. 11
1981 Dendrospyris binapertonis Goll De Wever pl. 3, fig. 4
1994 Dendrospyris binapertonis Goll Mahapatra & Sharma p. 159, pl. 1, fig. 1
1999 Dendrospyris aff. binapertonis Goll O'Connor p. 31, pl. 10, fig. 30
2013 Dendrospyris sp. aff. D. binapertonis Goll Kochhann et al. p. 539, pl. 2, fig. P
Catalog entries: Dendrospyris binapertonis
Original description: Diagnosis: A species of Dendrospyris characterized by six basal pores, sternal pore, and a lattice shell that is joined directly to the front, apex, and back of the sagittal ring and does not extend below the basal ring.
Description: Sagittal ring subcircular; 54 to 70μ high; 28 to 48μ thick; joined directly to front, apex, and back of lattice shell. Apical and vertical spines short; no frontal or axial spines. Some specimens have no sternal bar; in other skeletons, all eight basal-connector bars joined to basal ring. Basal ring oval, having lateral and sagittal indentations ; 33 to 64μ wide; 27 to 37μ thick; encloses six basal pores. Three or four basal spines circular in cross section; 12 to 55μ long; project from basal ring; taper to simple point or have irregularly branched ends. Basal spine adjacent to each of frontal and primary-lateral bars; some specimens have basal spine adjacent to sternal bar. In some forms, short auxiliary spines project laterally from proximal ends of basal spines adjacent to primary-lateral bars. Lattice shell 75 to 100μ wide; not extending below basal ring; slightly constricted sagittally; has appearance of smooth, thin sheet perforated by subcircular, widely spaced lattice pores 4 to 28μ in diameter. Variable number of lattice bars joined to sagittal or basal rings. Sternal pore present; frontal and vertical pores absent.
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:
Goll, M. R. (1968). Classification and phylogeny of Cenozoic Trissocyclidae (Radiolaria) in the Pacific and Caribbean Basins. Part I. Journal of Paleontology. 42(6): 1409-1432. gsReferences:
Dendrospyris binapertonis compiled by the radiolaria@mikrotax project team viewed: 6-10-2024
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