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Current identification:
Original Description
Measurements based on 30 specimens from 171B-1051A-8H-5, -16H-5 and -17H-2. Length (excluding horn) 125-190 µm; length of horn 50-100 µm; breadth of thorax 85-110 µm; breadth of peristome usually 12 µm. Distinguishing characters (rw): It differs from other co-occurring two-segmented forms in the arrangement of the thoracic pores and the somewhat constricted hyaline peristome. The length of the thorax is somewhat variable. In the early part of its range the distal thoracic pores are slightly larger than the proximal ones. Phylogeny (rw): Although no transitional forms have been observed, it seems clear that S. chrysallis n. sp. evolved rapidly from S. austellus n. sp. in the uppermost part of the Podocyrtis (Podocyrtoges) ampla Zone by loss of the abdominal segment.
Translation:
Size:
Etymology:
Extra details from original publication
Editors' Notes
Sethocyrtis sp. Chen 1975, p. 459, pl. 1, figs. 4, 5; Takemura 1992, p. 747, pl. 7, figs. 14, 15; Strong et al. 1995 (in part), p. 209, fig. 11w; Takemura & Ling 1997, p. 114, pl. 1, fig. 11.
Sethocyrtis sp. A Hollis et al. 1997, p. 65, pl. 6, fig. 7.
Sanfilippo, A. & Blome, C. D. (2001). Biostratigraphic implications of mid-latitude Palaeocene-Eocene radiolarian faunas from Hole 1051A, ODP Leg 171B, Blake Nose, western North Atlantic. Geological Society of London, Special Publications. 183: 185-224. gsReferences:
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Sethocyrtis chrysallis compiled by the radiolaria@mikrotax project team viewed: 1-7-2022
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