Dentoglobigerina pseudovenezuelana Blow & Banner 1962 from: Pearson, P.N.Olsson, R.K.Hemleben, C.Huber, B.T.Berggren, W.A. (2006): Atlas of Eocene Planktonic Foraminifera. p. 1-513 . |
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Species Dentoglobigerina pseudovenezuelana Blow & Banner 1962 |
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Diagnosis / Definition: |
Pearson et al. (2006):
DESCRIPTION.
Type of wall: Cancellate, normal perforate,
nonspinose, Globoquadrina-type wall texture.
Test morphology: Test trochospiral, compact,
globular, subcircular to subquadrate in outline, chambers
ovoid; in spiral view 3 1/2 ovoid chambers in ultimate
whorl, increasing moderately in size, sutures moderately
depressed, straight; in umbilical view 3-3 1/2 ovoid
chambers increasing moderately in size, sutures deeply
depressed, straight, umbilicus moderate in size,
sometimes overlapped by ultimate chamber, aperture
centered over the umbilicus, bordered by a thin irregular,
subtriangular-shaped lip that projects over the umbilicus,
pustules are concentrated in the apertural area; in edge
view chambers ovoid in shape, embracing, ultimate chamber extends over the umbilicus, oval to subcircular
in outline.
Size: Maximum diameter of holotype 0.5 1 mm, thickness 0.34 mm. |
Discussion / Comments: |
Spezzaferri & Silva (1990):
Very rare.
Pearson et al. (2006):
DISTINGUISHING FEATURES.-
The species is
characterized by its compact, subcircular to subquadrate
test, embracing chambers, and umbilically centered
aperture that is bordered by an irregular, subtriangular-shaped
lip that projects over the umbilicus, and
concentration of pustules in the apertural area. Its test is
more compact and the chambers are more flattened than in D. galavisi. Note that the holotype is slightly aberrant
in having a final chamber that is about the same size as
the penultimate chamber. More regular specimens with
proportionally large final chambers are more globular
in shape (see Plate 13.2).
DISCUSSION.-
Blow (1 979) included pseudovenezuelana
in his new genus Dentoglobigerina and
noted that the increased appression and embrace of the
chambers in the ultimate whorl of pseudovenezuelana
leads to a test whose equatorial outline becomes less
lobulate and more circular. He derived D.
pseudovenezuelana from Dentoglobigerina yeguaensis
(=Subbotina yeguaensis) and, in turn, derived yeguaensis
from D. galavisi (= Globoquadvina galavisi), based
essentially on middle Eocene morphotypes identified by
him as galavisi. As noted above in the discussion of G.
galavisi, he based his conclusion on a concept of a
"central type" for galavisi that differs considerably from
the holotype. Having derived yeguaensis from galavisi,
it appears that yeguaensis was chosen as the ancestor of
pseudovenezuelana. This scenario is rejected because
yeguaensis is a spinose subbotinid. It is more likely that
D. pseudovenezuelana evolved from D. galavisi, in an
evolutionary transition that partially mirrored the earlier
origin of Dentoglobigerina tripartita from D. galavisi.
PHYLOGENETIC RELATIONSHIPS.-
Dentoglobigerina
pseudovenezelelana evolved from D. galavisi in
the middle/late Eocene by developing more embracing
chambers, which led to a compact, subcircular or
subquadrate test.
STRATIGRAPHIC RANGE.-
Zone E14 to Zone 05?
(=P2 l b).
GEOGRAPHIC DISTRIBUTION.-
Known only from
a few low latitude locations.
STABLE ISOTOPE PALEOBI0LOGY.-
Recorded by
Poore and Matthews (1984) and Pearson and others
(200 1) with relatively positive ò18O and negative ò13C
indicating a deep planktonic habitat. |
Systematics: |
22 Genus Dentoglobigerina
Species Dentoglobigerina pseudovenezuelana
35 Ordo Foraminiferida
Superfamilia Globigerinaceae
Familia Globoquadrinidae
Genus Dentoglobigerina
Species Dentoglobigerina pseudovenezuelana
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Synonym list: |
Spezzaferri & Silva (1990):
Pearson et al. (2006):
1962 Globigerina yeguaensis pseudovenezuelana Blow & Banner. - Blow & Banner : p.100 pl. 11, fig. S-L (holotype)[upper Eocene
Cribrohantkenina danvillensis Zone, Lindi area, Tanzania];
fig. N, O (paratype)[lower Oligocene Globigerina oligocaenica Zone O1, Lindi Area, Tanzania,
Sample FCRM 1965]
2006 Dentoglobigerina pseudovenezuelana Blow & Banner. - Pearson et al. : p.407 pl. 13.2; fig. 1-16 (Pl. 13.2, Figs. 1-5: new SFMs of holotype of
Globigerina yeguaensis pseudovenezuelana Blow and
Banner)
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Specimen: |
Natural History Museum, London, Inventory number: P.44524
Natural History Museum, London, Inventory number: P.44526
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References: |
Bolli,H.M. (1957): Planktonic foraminifera from the Oligocene-Miocene Cipero and Lengua formations of Trinidad, B.W.I.. In: Studies in Foraminifery, Bulletin of the U.S. National Museum Vol. 215 Eds: Loeblich, A.R.Tappan, H.Beckmann, J.P.Bolli, H.M.Gallitelli, E.M.Troelsen, J.C. p. 97-123
Blow,W.H. and Banner,F.T. (1962): The Mid-Tertiary (Upper Eocene to Aquitanian) Globigerinaceae. In: Fundamentals of Mid‑Tertiary Stratigraphical Correlation Eds: Eames, F.E.Banner, F.T.Blow, W.H.Clarke, W.J. p. 61‑151
Blow,W.H. (1969): Late middle Eocene to Recent planktonic foraminiferal biostratigraphy. In: Proceedings of the First International Conference on Planktonic Microfossils, Geneva 1967 Vol. 1 Eds: Bronnimann, P.Renz, H.H. p. 199-422
Blow,W.H. (1979): The Cainozoic Globigerinida. 3 Vols p. 1413 pp
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
Spezzaferri,S. and Silva,I.S.. (1990): Oligocene planktonic foraminiferal biostratigraphy and paleoclimatic interpretation from Hole 538A, DSDP Leg 77, Gulf of Mexico . Palaeogeography, Palaeoclimatology, Palaeoecology Vol. 83 p. 217-263
Spezzaferri,S. and Premoli Silva,I. (1991): Oligocene planktonic foraminiferal biostratigraphy and paleoclimatic interpretation from Hole 538A, DSDP Leg 77, Gulf of Mexico . Palaeogeography, Palaeoclimatology, Palaeoecology Vol. 83 p. 217-263
Pearson,P.N.; Olsson,R.K.; Hemleben,C.; Huber,B.T. and Berggren,W.A. (2006): Atlas of Eocene Planktonic Foraminifera. p. 1-513
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