From Suzuki Paleotax db:
1968 Plectacantha cremastoplegma n. sp. Nigrini p. 55, pl. 1, fig. 3a, 3b, 3c, text-fig. 2
1981 Plectacantha cremastoplegma Nigrini Kruglikova fig. 3.12
1992 Plectacantha cremastoplegma Nigrini Nigrini & Caulet p. 146, pl. 1, fig. 11
2015 Plectacantha cremastoplegma Nigrini Matsuzaki et al. p. 43, figs. 7.3-7.5, 7.9
Catalog entries: Plectacantha cremastoplegma
Original description: One-segmented shell consisting of a basic spine structure connected distally by a thin, smooth, irregular lattice of straight bars and subangular to subcircular pores of varying size. Primary and secondary laterals, median bar, thorn-like axial rod, and apical spine present in the usual (Plagiocarpa, Popofsky, 1913, text-figure 2d) configuration. Primary laterals both fork distally, each forming 2 (sometimes 3) stout, 3-bladed spines. Secondary laterals strongly developed into stout, 3-bladed spines. Similar spines ("lateral apical") flank the apical spine, one on each side of it. Strong arches extend between the primary laterals, and from each primary lateral to its corresponding "lateral apical" spine and secondary lateral, Two, vertically directed, stout, 3-bladed spines originate at the points of bifurcation of the primary laterals, initially forming part of the arch structure.
Length of cephalis (excluding spines) 72-113µm. Maximum breadth of cephalis (excluding spines) 81-108µm.
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:
Nigrini, C. A. (1968). Radiolaria from eastern tropical Pacific sediments. Micropaleontology. 14(1): 51-63. gsReferences:

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Plectacantha cremastoplegma compiled by the radiolaria@mikrotax project team viewed: 5-10-2026
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