Globoturborotalita gnaucki 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 . |
Notice: This catalogue page may contain unedited data.
|
Species Globoturborotalita gnaucki Blow & Banner 1962 |
|
|
Diagnosis / Definition: |
Pearson et al. (2006):
DESCRIPTION.
Type of wall: Cancellate, normal perforate,
spinose, ruber-type wall structure.
Test morphology: Test moderately low
trochospiral, globular, lobulate in outline, chambers
globular; in spiral view 4112 globular, slightly embracing
chambers in ultimate whorl, increasing moderately in size, sutures depressed, straight; in umbilical view 4%
globular, slightly embracing chambers, increasing
moderately in size, sutures depressed, straight, umbilicus
large, open, enclosed by surrounding chambers, aperture
umbilical, a rounded arch, bordered by a thin thickened
rim; in edge view chambers globular in shape, slightly
embracing, initial spire of chambers slightly elevated.
Size: Maximum diameter 0.25-0.36 mm,
minimum diameter 0.23-30 mm, maximum width 0.19
mm. |
Discussion / Comments: |
Pearson et al. (2006):
DISTINGUISHING FEATURES.-
The species is
characterized by its small lobulate test, slightly
embracing, globular chambers, large umbilical aperture,
and cancellate wall texture.
DISCUSSION.-
The holotype of Globoturborotalita
gnaucki is illustrated in SEM for the first time (Pl. 6.4:
Figs. 1-4). Blow (1979) considered Globigerina gnaucki
as a possible junior synonmy of Globigerina fariasi
BerrnudCz, but that species has 5 to 6 chambers in the
ultimate whorl and a very large open umbilicus.
Globoturborotalita gnaucki is a distinctive form in the
upper Eocene and lower Oligocene and is here elevated
to species level. We include a paratype of Globigerina
ouachitaensis Howe and Wallace, illustrated in SEM for
the first time (PI. 6.4: Fig. 15) in this species. The species
originated during the late Eocene radiation of
Globotuvborotalita. We place Howe and Wallace's
(1932) paratype of Globigerina ouachitaensis in
synonymy.
PHYLOGENETIC RELATIONSHIPS.-
Globoturborotalita
gnaucki was derived from Globoturborotalita
ouachitaensis by an increase in the number
of chambers in the ultimate whorl to 4 1/2.
GEOGRAPHIC DISTRIBUTION .-
Distributed in mid- to low latitudes.
STABLE ISOTOPE PALEOBIOL0GY.-
No data available. |
Systematics: |
35 Ordo Foraminiferida
Superfamilia Globigerinaceae
Familia Globigerinidae
Genus Globoturborotalita
Species Globoturborotalita gnaucki
|
Synonym list: |
Pearson et al. (2006):
p 1932 Globigerina ouachitaensis Howe & Wallace. - Howe & Wallace : (paratype, not holotype) [Zone E15116, Danville
Landing, Louisana]. [Not Howe and Wallace, 1932.]
1962 Globigerina ouachitaensis gnaucki Blow & Banner. - Blow & Banner : p.91 pl. IX: fig. 1-n, holotype [lower Oligocene
Globigerina oligocaenica Zone, Sample FCRM 1965,
Lindi area, Tanzania]
1980 Globigerina ouachitaensis Howe & Wallace. - Charollais et al. : p.64 pl. 6; fig. 14-17 [lower Oligocene,
France].[Not Howe and Wallace, 1932.]
2006 Globoturborotalita gnaucki Blow & Banner. - Pearson et al. : p.124 pl. 6.4; fig. 1-15 (Pl. 6.4, Figs. 1-3: new SEMs of holotype of
Globigerina ouachitaensis gaaucki Blow and Banner)
|
Specimen: |
Natural History Museum, London, Inventory number: P44509
|
References: |
Howe,H.V. and Wallace,W.E. (1932): Foraminifera of the Jackson Eocene at Danville Landing on the Ouachita, Catahoula Parish, Louisiana . Bull. Louisiana Dept. Conservation Geol. Vol. 2 p. 18-79
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
Charollais,J..; Hochuli,P..; Oektlt,H..; Perch-Nielsen,K.; Toumarkine,M.; Rögl,F. and Pajris,-.J.. (1980): Les Marnes Foraminiféres et les Schistes a Meletta des Chaines Subalpines septentrionales (Haute-Savoie, France) . Eclogae Geologicae Helvetiae Vol. 73 p. 9-69
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
Pearson,P.N.; Olsson,R.K.; Hemleben,C.; Huber,B.T. and Berggren,W.A. (2006): Atlas of Eocene Planktonic Foraminifera. p. 1-513
|
This work is licensed under a Creative Commons Attribution 2.5 License.
|
|