Globigerinatheka kugleri Bolli et al. 1957 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.
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Species Globigerinatheka kugleri Bolli et al. 1957 |
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Diagnosis / Definition: |
Pearson et al. (2006):
DESCRIPTION.
Type of wall: Spinose, cancellate with pores
0.04-0.05 mm in diameter.
Test morphology: Test subtriangular in outline,
rather lobate; 2-3 whorls; initial coil very tight, composed
of an unknown number of very small globular chambers;
second coil much looser with 4 globular chambers
increasing gradually but rather rapidly in size as added;
last coil consisting of 4 very rapidly enlarging globular
chambers; the antepenultimate chamber is twice as large
as the previous one and about half the size of the last
formed chamber; sutures in the inner coil initially not
visible, then straight and radial, rather depressed; primary
aperture an umbilical low arch; two to three rather small
arched secondary apertures at the base of the last chamber; primary and secondary apertures may be
covered by small slightly inflated bullae.
Size: Greatest diameter of holotype 0.44 mm,
greatest thickness 0.47 mm; paratypes range from 0.36
to 0.47 mm in diameter. |
Discussion / Comments: |
Pearson et al. (2006):
DISTINGUISHING FEATURES.-
Test subtriangular
in outline, rather lobate, with three chambers in the outer
whorl rapidly increasing in size as added, sutures
depressed in the outer whorl; low arched primary and
secondary sutural apertures that may be covered by
slightly inflated bullae. G. kugleri differs from G.
mexicana by the subtriangular outline, its distinct sutures
and low arched apertures.
DISCUSSION.-
Bolli (1957) included a large
specimen in G. kugleri, which Proto Decima and Bolli
(1970) selected as the holotype of their new species G.
curuyi. Bolli (1 972) considered G. kugleri as a subspecies
of G. mexicana. According to him, G. kugleri differs
from mexicana and barri in having larger, more globular
chambers arranged in a loosely coiled initial spire,
resulting in less compact shape. However, Bolli (1972)
also included two specimens that have typical kugleri
morphology (his pl. 2, figs. 15-16) in G. barri because of the presence of bullae. In disagreement with Bolli
(1 972), we consider these two specimens as belonging
to G. kugleri. In fact, G. kugleri differs from mexicana
and barri in having a much less compact test, which is
subtriangular in outline, becoming subglobular only
because of bullae, more depressed sutures, a much looser
coiling-mode and more rapidly enlarging globular
chambers in the last whorl. It differs from G. curryi by
its subtriangular and more lobate outline, shorter initial
spire with less numerous chambers, and smaller size
which never exceeds 0.5 mm. The specimen illustrated
by Bronnimann (1952) in text-figs. 3d-f as G. barri was
later included in G. kugleri (Globigerapsis) by Bolli and
others (1957, p. 34), an attribution followed here, even
though Bolli (1972) included the same specimen in G.
mexicana mexicana, as suggested by Saito (1962).
Some specimens identified by Blow (1979) as
G. mexicana mexicana (pl. 198, figs. 2, 4-5) and G.
mexicana howei (pl. 198, fig. 6) show a subtriangular
test outline and the last two chambers are almost of the
same size. Both these features are more typical of G.
kugleri than of G. mexicana, whereas the specimen
attributed to G. howei does not possess a bulla;
consequently, they are all included under G. kugleri. Blow (1979) considered G. subconglobata as a junior
synonym of G. kugleri (p. 8 19), but according to our
researches, these two species are discrete, separate taxa.
PHYLOGENETIC RELATIONSHIP.-
According to
Bolli (1972), G. kugleri is related to the G. mexicana
group, but this relationship is not fully proved. On the
other hand, Blow (1979) considered G. kugleri as the
ancestral member of the lineage evolving to beckmanni
via G. curyi and G. euganea in the middle Eocene, a
hypothesis followed here. Blow (1979) also suggested
that G. kugleri is linked through transitional forms to G.
index. However, the specimens representing the so-called
transitions (Blow, 1979, pl. 174, figs. 7-8) do not support
Blow's view.
GEOGRAPHIC DISTRIBUTION.-
Tropical to temperate regions.
STABLE ISOTOPE PALEOBIOL0GY.-
Boersma
and others (1987) recorded relatively negative ň18O for
this species from DSDP Sites 357 and 548, indicating a
shallow planktonic habitat. This is supported by boron
isotopic data (Pearson and Palmer, 1999). |
Systematics: |
35 Ordo Foraminiferida
Superfamilia Globigerinaceae
Familia Globigerinidae
Genus Globigerinatheka
Species Globigerinatheka kugleri
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Synonym list: |
Pearson et al. (2006):
1952 Globigerinatheka barri Brönnimann. - Brönnimann : text-fig. 3d-f [upper Eocene, Mount Moriah, Trinidad].
[Not Brönnimann, 1952]
1957 Globigerapsis kugleri Bolli et al.. - Bolli et al. : p. 34-35 pl. 6; fig. 6a-c [partim; Eocene Globigerinatheka barri
Zone, Navet Fm., Penitence Hill marl, from a block in the
Oligocene Nariva Fm., Pointe-a-Pierre, Trinidad]
1959 Globigerina mexicana Cushman. - Mallory : pl. 22; fig. 9a-c [fide Bolli, 1972]; [Not Cushman, 1925]
1962 Globigerapsis index Finlay. - Blow & Banner : pl. 15; fig. H [middle Eocene, Kilwa district, Tankanyika];
[Not Finlay, 1939]
1970 Globigerapsis kugleri Bolli et al.. - Samanta : pl. 2; fig. 11-13 [middle Eocene
Orbulinoides beckmanni Zone, Lakhpat, Cutch, India].-
Postuma, 1971: 138, figs. on p. 139 [Trinidad]
1972 Globigerinatheka mexicana barri Brönnimann. - Bolli : pl. 2; fig. 15, 16 (bullate kugleri); [middle Eocene
Orbulinoides beckmanni Zone, Navet Fm., Pointe-a-
Pierre, Trinidad]; [Not Brönnimann, 1952]
1975 Globigerinatheka kugleri Bolli et al.. - Stainforth et al. : fig. 59.1a-c (refigured holotype);
fig. 59.2-3 [middle Eocene
Orbulinoides beckmanni Zone, Navet Fm., Trinidad]
1979 Globigerapsis kugleri kugleri Bolli et al.. - Blow : pl. 175, fig. 1, ?fig. 2 [middle Eocene Zone P l l, Kilwa area, Tanzania];
pl. 181, fig. 2, 4 (not figs. 3,
5, and 6) [middle Eocene Zone P1 1, DSDP Hole 21A,
Rio Grande Rise, South Atlantic Ocean].
non 1979 Globigerapsis kugleri Bolli et al.. - Blow : pl. 181; fig. 3 [middle Eocene Zone P1 1,
DSDP Hole 21A, South Atlantic Ocean]; (= G. korotkovi)
1983 Globigerinatheka mexicana kugleri Bolli et al.. - Toumarkine : pl. 20; fig. 18-19 (from Bolli, 1972), fig. 20-22 [middle Eocene Orbulinoides
beckmanni Zone, Navet Fm., Pointe-á-Pierre, Trinidad]
? 1983 Globigerinatheka kugleri Bolli et al.. - Pujol : pl. 7; fig. 4 [middle Eocene Zone PI 1-13,
DSDP Hole 5 16F, Rio Grande Rise, South Atlantic
Ocean]
2003 Globigerinatheka mexicana kugleri Bolli et al.. - Warraich & Nishi : pl. 2; fig. 15a-b [middle Eocene
Zone P12, Rakhi Nala Section, Sulaiman Range, Indus
Basin, Pakistan]
2006 Globigerinatheka kugleri Bolli et al.. - Pearson et al. : p.193 pl. 7.7; fig. 1-16 (Pl. 7.7, Figs. 1,2: new SEMs of holotype of
Globigerapsis kugleri Bolli, Loeblich and Tappan)
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Specimen: |
Smithsonian Museum of Natural History, Washington, D.C., Inventory number: USNM 4220
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References: |
Brönnimann,P. (1952): Globigerinoita and Globigerinatheka, new genera from the Tertiary of Trinidad, B.W.I. . Contributions from the Cushman Foundation for Foraminiferal Research Vol. 3 p. 25-28
Bolli,H.M.; Loeblich,A.R. and Tappan,H. (1957): The Planktonic foraminiferal families Hantkeninidae, Orbulinidae, Globorotaliidae, and Globotruncanidae . U.S. National Museum Bull. Vol. 215 p. 3-50
Bolli,H.M. (1957): Planktonic Foraminifera from the Eocene Navet and San Fernando formations of Trinidad, B.W.I. . Bull. U.S. natl. Mus. Vol. 215 p. 155-172
Mallory,V.S. (1959): Lower Tertiary Biostratigraphy of the California Coast Ranges. p. 146
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
Samanta,B.K. (1970): Middle Eocene Planktonic Foraminifera from Lakhpat, Cutch, Western India . Micropaleontology Vol. 16
Proto Decima,F. and Bolli,H.M. (1970): Evolution and variability of Orbulinoides beckmanni (Saito) . Ecoglae geologicae Helvetiae Vol. 63 p. 883-905
Bolli,H.M. (1972): The Genus Globigerinatheka Brönnimann . Journal of Foraminiferal Research Vol. 2 p. 109-136
Stainforth,R.M.; Lamb,J.L.; Luterbacher,H.P.; Beard,J.H. and Jeffords,R.M. (1975): Cenozoic planktonic foraminiferal zonation and characteristics of index forms . Paleontological ContributionsArticle 62 p. 425
Blow,W.H. (1979): The Cainozoic Globigerinida. 3 Vols p. 1413 pp
Toumarkine,M. (1983): Les Foraminiferes planctoniques de l'Eocéne moyen et supérieur des regions tropicales ŕ temperées chaudes. In: Thése de Doctorat d'Etat čs Sciences Vol. 6(83-05) p. 219
Pujol,C. (1983): Cenozoic Planktonic Foraminiferal Biostratigraphy of the Southwestern Atlantic (Rio Grande Rise): Deep Sea Drilling Project Leg 72. In: Initial Reports of the Deep Sea Drilling Project Vol. 72 Eds: Barker, P.F.Johnson, D.A. p. 623-673
Warraich,M.Y.. and Nishi,H.. (2003): Eocene planktic foraminiferal biostratigraphy of the Sulaiman range, Indus Basin, Pakistan . Journal of Foraminiferal Research Vol. 33 p. 219-236
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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