Chaisson & Leckie (1993):
Remarks: A temperate zone species found in low numbers at this
tropical site.
Similar species: Globorotalia challengeri looks like a tiny, delicate Paragloborotalia
mayeri. In addition to being distinctly smaller, G. challengeri has a more
circular equatorial profile and a lower arched aperture than P. mayeri. It differs
from early forms of Neogloboquadrina acostaensis in lacking the distinctive
apertural flap or kümmerform-like final chamber commonly developed on N.
acostaensis, and in having a final chamber that is distinctly ovate in equatorial
view as compared with the spherical chambers developed in species of Neogloboquadrina.
In addition, the wall of G. challengeri is coarsely perforate on the
early whorls and on the earliest chambers of the final whorl, and then becomes
more finely perforate with each successive chamber. N. acostaensis, on the other
hand, is more or less uniformly perforate throughout its ontogeny. |
Srinivasan,M.S. and Kennett,J.P. (1981): Neogene planktonic foraminiferal biostratigraphy and evolution: equatorial to subantarctic, South Pacific. . Marine Micropaleontology Vol. 6 p. 499-533
Kennett,J. and Srinivasan,M.S. (1983): Neogene Planktonic Foraminifera - A Phylogenetic Atlas.
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
Turco,E.; Bambini,A.M.; Foresi,L.; Iaccarino,S.; Lirer,F.; Mazzei,R. and Salvatorini,G. (2002): Middle Miocene high-resolution calcareous plankton biostratigraphy at Site 926 (Leg 154, equatorial Atlantic Ocean): palaeoecological and palaeobiogeographical implications . GeobiosMemoire spec. 24 p. 257-276
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