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Globorotalia miocenica Palmer 1945 from: Bolli, H.M.Saunders, J.B. (1985): Oligocene to Holocene low latitude planktic foraminifers. In: Plankton Stratigraphy Eds: Bolli, H.M.Saunders, J.B. p. 155-262
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Species Globorotalia miocenica Palmer 1945



Alternative name:
Discussion / Comments:
Bolli & Saunders (1985):
G. miocenica differs from G. pseudomiocenica in an absolutely flat spiral side. Occasionally the surface may even tend to become slightly concave. Compared with G. pseudomiocenica, the umbilical side is still higher and in equatorial view the periphery more circular and less lobate. Because the transitional forms are often erroneously identified as G. miocenica it must be stressed that correct species identification allows for little variation, one of the prime characters, being the absolutely flat spiral side. Despite its name, G. miocenica is confined to the late Early and the Middle Pliocene.
Synonym list:
Bolli & Saunders (1985):
1945 Globorotalia menardii var. miocenica Palmer. - Palmer : p.70 pl.1, figs.10a-c
1985 Globorotalia miocenica Palmer. - Bolli & Saunders : 225, 229 figs. 33.2, 35.4-8; 6,10,11
Stratigraphy - absolute ages:
FAD: 3.55 ± 0 [Ma], Berggren et al. (1995) Atlantic Ocean
LAD: 2.3 ± 0 [Ma], Berggren et al. (1995) Atlantic Ocean
References:

Palmer,D.K. (1945):
Notes on the foraminifers from Bowden, Jamaica . Bulletins of American paleontology Vol. 29

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

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)

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