Pulleniatina obliquiloculata Parker & Jones 1865 from: Vincent, E.Toumarkine, M. (1990): Neogene planktonic foraminifers from the Western Tropical Indian Ocean, Leg 115. In: Proceedings of the Ocean Drilling Program, Scientific Results Vol. 115 Eds: Duncan, R.A..Backman, J.Peterson, L.C. p. 795-836 . |
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Species Pulleniatina obliquiloculata Parker & Jones 1865 |
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Diagnosis / Definition: |
Kennett & Srinivasan (1983):
Test globose, initially trochospiral, later streptospiral almost involute, axial periphery broadly rounded, four to five broadly rounded chambers in the final whorl; sutures
almost flush; surface smooth, granular in apertural areas; umbilicus covered; aperture a low arch, extending from umbilical area to periphery and onto spiral side. |
Discussion / Comments: |
Bolli & Saunders (1985):
The type species for Pulleniatina, Pullenia sphaeroides obliquiloculata Parker & Jones (1865), is considered lost. Bolli et al. (1957) designated a lectotype to which Banner & Blow (1967) gave paralectotype status, claiming that the selected specimen is immature and comparable only to the inner whorls of the lectotype they erected at that time. Following the emended species description by Banner & Blow, P. obliquiloculata differs from P. primalis-P. praecursor in an overlap of the oppositely placed chamber on the umbilical end of the last chamber in such a way that they are joined by a distinct straight suture and not by a point as in P. praecursor. In overall test morphology P. obliquiloculata is distinctly higher in peripheral view, and the equatorial periphery less lobate. Spirally the intercameral sutures are less incised and chambers of early whorls less visible.
Chaisson & Pearson (1997):
The stratigraphic ranges of pulleniatinids are discontinuous in the Atlantic (Bolli and Saunders, 1985) and, moreover, the morphotypes do not have stratigraphic integrity, as they do in the western equatorial Pacific
(Chaisson and Leckie, 1993). P. obliquiloculata does not occur in the early Pliocene at Site 925 before the “Atlantic interim”, although its published range (Kennett and Srinivasan, 1983) suggests that it should. Furthermore, the primalis morphotype persists upsection at Site 925 beyond its published LO (Kennett and Srinivasan, 1983; Berggren et al., 1985), as it does in the eastern
equatorial Pacific (Chaisson, 1996).
Chaisson & Leckie (1993):
Remarks: This species is distinguished from earlier pulleniatinids by an
aperture that extends from the umbilical to the spiral side on the final chamber enclosing earlier chambers to varying degrees. Pulleniatina finalis is included
under the present species concept (cf. Orr and Jenkins, 1980, and Kennett and
Srinivasan, 1983).
Similar species: See Pulleniatina primalis. |
Systematics: |
1 Superregnum Eukaryota
Regnum Protoctista
Phylum Ciliophora
Subphylum Postciliodesmatophora
Ordo Globigerinida
Superfamilia Globorotaliaceae
Superfamilia Nonionacea
Familia Pulleniatinidae
Genus Pulleniatina
Species Pulleniatina obliquiloculata
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Synonym list: |
Kennett & Srinivasan (1983):
Chaisson & d'Hondt (2000):
Bolli & Saunders (1985):
Chaisson & Pearson (1997):
Vincent & Toumarkine (1990):
Chaisson & Leckie (1993):
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References: |
Parker,W.K. and Jones,T.R. (1865): On some foraminifera from the North Atlantic and Arctic Oceans, including Davis Straits and Baffin's Bay . Philosophical Transactions of the Royal Society Vol. 155 p. 325–441
Kennett,J. and Srinivasan,M.S. (1983): Neogene Planktonic Foraminifera - A Phylogenetic Atlas.
Bolli,H.M. and Saunders,J.B. (1985): Oligocene to Holocene low latitude planktic foraminifers. In: Plankton Stratigraphy Eds: Bolli, H.M.Saunders, J.B. p. 155-262
Vincent,E. and Toumarkine,M. (1990): Neogene planktonic foraminifers from the Western Tropical Indian Ocean, Leg 115. In: Proceedings of the Ocean Drilling Program, Scientific Results Vol. 115 Eds: Duncan, R.A..Backman, J.Peterson, L.C. p. 795-836
Chaisson,W.P. and Leckie,R.M. (1993): High-Resolution Planktonic Foraminifer Biostratigraphy of Site 806, Ontong Java Plateau (Western Equatorial Pacific). In: Proceedings of the Ocean Drilling Program, Scientific Results Vol. 130 Eds: Berger, W.H.Kroenke, L.W..Mayer, L.A..et al. p. 137-178
Chaisson,W.P. and Pearson,P.N. (1997): Planktonic foraminifer biostratigraphy at Site 925: middle Miocene–Pleistocene. In: Proceedings of the Ocean Drilling Program, Scientific Results Vol. 154 Eds: Shackleton, N.J.Curry, W.B.Richter, C.Bralower, T.J.
Chaisson,W.P. and d'Hondt,S.L. (2000): Neogene planktonic foraminifer biostratigraphy at Site 999, Western Caribbean Sea. In: Proceedings of the Ocean Drilling Program, Scientific Results Vol. 165 Eds: Leckie, R.M.Sigurdsson, H.Acton, G.D.Draper, G. p. 19-56
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