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Species Globorotalia tumida Brady 1877



Discussion / Comments:
Chaisson & Leckie (1993):
Remarks: Globorotalia tumida s.s. is swollen ("tumid") at the end opposite its final chamber. Its keel is consistently heavy and often wide. The texture of the test is rough and encrusted with secondary calcite, particularly around the umbilicus. The general outline of the umbilical view of this species is consistently oblate. Similar species: Especially tumid Globorotalia menardii are common in some samples. These specimens are distinguished from G. tumida by any combination of the the following characteristics: greater symmetry of biconvexity, smoother wall texture, and/or more circular equatorial outline. G. merotumida is smaller with a smoother test wall and thinner keel. See G. plesiotumida.
Systematics:

1
 Superregnum Eukaryota
  Regnum Protoctista
   Phylum Ciliophora
    Subphylum Postciliodesmatophora
     Ordo Globigerinida
      Superfamilia Globorotaliaceae
       Superfamilia Nonionacea
        Familia Globorotaliidae
         Genus Globorotalia
          Species Globorotalia tumida
Synonym list:
Chaisson & d'Hondt (2000):
1877 Pulvinulina menardii var. tumida Brady. - Brady : pl 103 figs 4-6
1983 Globorotalia tumida tumida Brady. - Kennett & Srinivasan : p.158 pl 38 figs 1-3
Chaisson & Pearson (1997):
1877 Pulvinulina menardii var. tumida Brady. - Brady : pl. 103; fig. 4-6
1983 Globorotalia (Globorotalia) tumida tumida Brady. - Kennett & Srinivasan : p.158 pl. 36; fig. 1 pl. 38; fig. 1-3
Chaisson & Leckie (1993):
1877 Pulvinulina menardii var. tumida Brady. - Brady : pl. 103; fig. 4-6
1983 Globorotalia (Globorotalia) tumida tumida Brady. - Kennett & Srinivasan : p.158 pl. 36, fig. 1; pl. 38, fig. 1-3
1993 Globorotalia tumida Brady. - Chaisson & Leckie : p.175 pl. 7; fig. 3-5
Was used in synonym list of:
Globorotalia tumida tumida Brady 1877
Stratigraphy - absolute ages:
FAD: 5.6 ± 0 [Ma], Berggren et al. (1995)
FAD: 5.6 ± 0 [Ma], Berggren et al. (1995)
FAD: 5.82 ± 0 [Ma], Chaisson & Pearson (1997) ODP Leg 154 Site 925
References:

Brady,H.B. (1877):
Supplementary note on the foraminifers of the Chalk (?)of the New Britain Group . Geological Magazine London Vol. 4

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

Berggren,W.A.; Hilgen,F.J.; Langereis,C.G.; Kent,D.V.; Obradovich,J.D.; Raffi,I.; Raymo,M.E. and Shackleton,N.J. (1995):
Late Neogene chronology: New perspectives in high-resolution stratigraphy . Geological Society of America Bulletin Vol. 107(11)

Berggren,W.A.; Kent,D.V.; Swisher,C.C. and Aubry,M.P. (1995):
A revised Cenozoic Geochronology and Chronostratigraphy.
In: Geochronology Time Scales and Global Stratigraphic Correlation, SEPM Special Publication Vol. 54

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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