Globigerinatheka semiinvoluta Keijzer 1945 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 semiinvoluta Keijzer 1945 |
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Alternative name: |
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Diagnosis / Definition: |
Pearson et al. (2006):
DESCRIPTION.
Tvpe of wall: Spinose, cancellate, thin, with a
high density of pores, < 0.04 mm in diameter.
Test morphology: Test spherical with a very
large hemispherical last chamber embracing half or more
of the earlier chambers with one to four prominent,
circular, secondary apertures (commonly 3) mainly bordered by a marked rim; early chambers coiled in a
low and rather short trochospire, separated by poorly
visible sutures that become slightly more distinct and
slightly depressed in the adult.
Size: The size of specimens is highly variable.
Diameter may be up to 0.55 mm, however much smaller
specimens are common especially in mid latitudes. In
smaller morphotypes, the hemispherical last chamber
shows much smaller or even poorly visible secondary
apertures. |
Discussion / Comments: |
Toumarkine & Luterbacher (1985):
The main character of G. semiinvoluta is the final hemispherical chamber which embraces nearly half of the earlier test and the high-arched to circular sutural apertures with distinct rims. However, a great amount of intraspecific variability can be seen in the dimensions of the test as well as the size and the number and shape of the apertures. This variability is due to ecologic conditions: the typical specimens found in tropical areas (Figs. 39.8, 15, 17) are generally larger with better developed apertures than those of the temperate areas (Figs. 39.1-6, 12-14). The number of apertures (1 to 4, commonly 2 or 3) is not directly related to the size of the specimen.
G. semiinvoluta differs from G. index tropicalis by its larger and more embracing final chamber and its less incised sutures. It differs from G. mexicana mexicana by the same characters and also by its generally larger size, at least in tropical regions.
Pearson et al. (2006):
DISTINGUISHING FEATURES.-
Globigerinatheka
semiinvoluta differs from all the other globular
globigerinathekids by its very inflated enveloping last
chamber, its large and noticeably rimmed, circular
secondary apertures, much shorter initial trochospire and
mainly indistinct sutures. Globigerinatheka mexicana
and G. semiinvoluta differ by the circular apertures with
distinctive rims in G. semiinvoluta, which are not present
in G. mexicana. G. semiinvoluta is distinguished from
G. tropicalis by an embracing final chamber.
DISCUSSION.-
Originally described as Globigerinoides
semi-involutus by Keijzer, the hyphen has
been removed (ICZN, Art. 32.5) and the ending has been
changed to agree in gender with Globigerinatheka
(ICZN, Art. 31.2). Bolli (1957) designated hypotypes
of G. semiinvoluta from the type locality (Navet
Formation, Trinidad). Blow and Saito (1 968a) suggested
that G. semiinvoluta was synonymous with G. mexicana.
However, we recognise G. semiinvoluta and G. mexicana
as taxonomically and stratigraphically distinct, although
transitional forms occur in uppermost Zone E13 to
lowermost Zone E14. Blow (1979, p. 788) stated that
G. korotkovi is taxonomically indistinguishable from G.
semiinvoluta even though the former species is high
spired; he also included G. lindiensis (here considered a
synonym of G. tropicalis) saying it is not worth differentiating this species taxonomically from G.
semiinvoluta (p. 791) as well as G. rubriformis (here G.
korotkovi) that he considered as immature specimens of
G. semiinvoluta (p. 8 13). Blow (1 979) included G.
semiinvoluta in the genus Porticulasphaera, emended,
here considered a junior synonym of Globigerinatheka.
Toumarkine (1975) attributed to G. semiinvoluta (and
illustrated) two small specimens from Shatsky Rise that
exhibit a very rough surface.
PHYLOGENETIC RELATIONSHIPS.-
Blow and
Banner (1962) suggested that G. semiinvoluta evolved
from G. tropicalis, a relationship that is not supported
here. In the western North Atlantic (ODP Site 1052), G.
semiinvoluta appears to descend from G. mexicana, a
phylogeny also proposed by Bolli (1972) and Blow
(1979). The distinct rimmed apertures and less depressed
sutures developed in the upper middle Eocene to lower
upper Eocene with trandtional forms evident in
uppermost E1 3 to lowermost E1 4.
GEOGRAPHIC DISTRIBUTION.-
Globigerinatheka
semiinvoluta is common in low latitudes, with well
developed large specimens, and extends to temperate
latitudes with smaller specimens. It is absent in high
latitudes.
STABLE ISOTOPE PALEOBIOL0GY.-
Oxygen and
carbon isotopic data indicate that G. semiinvoluta
occupied a mixed layer habitat (Poore and Matthews,
1984; Pearson and others, 2001; Wade and Kroon, 2002,
referred to as G. mexicana).
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Systematics: |
15 Classis Foraminifera
Genus Globigerinatheka
Species Globigerinatheka semiinvoluta
35 Ordo Foraminiferida
Superfamilia Globigerinaceae
Familia Globigerinidae
Genus Globigerinatheka
Species Globigerinatheka semiinvoluta
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Synonym list: |
Toumarkine & Luterbacher (1985):
Pearson et al. (2006):
1953 Globigerinoides index Finlay. - Beckmann : pl. 25; fig. 14 [upper Eocene, Oceanic Fm., Barbados]; [Not Finlay,
1939]
1957 Globigerapsis semiinvoluta Keijzer. - Bolli : p.165 pl. 36; fig. 19-20 (hypotypes) [upper Eocene Globigerapsis semiinvoluta
Zone, Navet Fm., Trinidad]
1962 Globigerapsis semiinvoluta Keijzer. - Blow & Banner : p.125 pl. 15; fig. J-K, ?L [upper Eocene
Globigerapsis semi-involuta Zone, Lindi area, Tanzania]
non 1963 Globigerapsis semiinvoluta Keijzer. - Eckert : p.1063 pl. 7; fig. 1a-3c [upper Eocene, Schimberg
Section, Swiss Alps]; (= G. luterbacheri)
1968 Globigerapsis semiinvoluta Keijzer. - Samuel & Salaj : pl. 21; fig. 3a-c [upper Eocene Globigerapsis index
Zone, Kravany, Carpathians, Slovakia]
1969 Globigerapsis mexicana Cushman. - Blow : p.330 pl. 27; fig. 3-4 [upper Eocene Zone P15, Lindi area,
Tanzania]
1971 Globigerapsis mexicana Cushman. - Raju : pl. 11; fig. 1-6 [upper Eocene, Cauvery basin,
S. India]; [Not Cushman, 1925]
1972 Globigerinatheka semiinvoluta Keijzer. - Bolli : p.131 pl. 5, fig. 1-27;
pl. 6, fig. 1-17 [upper Eocene Globigerinatheka semiinvoluta Zone type locality, Navet Fm., Trinidad];
text-fig. 72-76 (redrawn holotype);
text-fig. 77-78 (from Bolli and others, 1957); text-fig. 79 (from Blow and Banner, 1962)
1975 Globigerinatheka semiinvoluta Keijzer. - Stainforth et al. : p. 223-225 fig. 83.1-2, 6 [upper Eocene, Navet Fm., Trinidad];
fig. 83.3-4 (from Bolli, 1972);
fig. 83.5, 7 (refigured from Blow and Banner, 1962)
1975 Globigerinatheka semiinvoluta Keijzer. - Toumarkine : pl. 4, ?fig. 17, 18 [upper Eocene Globigerinatheka
semiinvoluta Zone, DSDP Site 305, Shatsky Rise, northwest
Pacific Ocean]
1975 Globigerinatheka semiinvoluta Keijzer. - Toumarkine & Bolli : pl. 6; fig. 15-24 [upper Eocene Globigerinatheka
semiinvoluta Zone, Possagno Section, northern Italy]
1978 Globigerinatheka semiinvoluta Keijzer. - Toumarkine : pl. 5, fig. 1-14 [upper Eocene Globigerinatheka semiinvoluta Zone, DSDP Site 363, South Atlantic Ocean];
pl. 5, figs. 15-21 [upper Eocene Globorotalia cerroazulensis s.l. to Globigerinatheka
semiinvoluta Zone, DSDP Site 360, South Atlantic
Ocean]
1979 Porticulasphaera semiinvoluta Keijzer. - Blow : pl. 27, fig. 3-4 (new name for Globigerapsis mexicana of Blow, 1969);
pl. 240, figs. 9-10 [upper Eocene Zone P15, Lindi area, Tanzania]
1983 Globigerinatheka semiinvoluta Keijzer. - Toumarkine : pl. 20, fig. 1 [upper Eocene, Menton, Southern France];
fig. 2 [upper Eocene G. semiinvoluta Zone, Contes Section, Southern France];
fig. 3-4 [upper Eocene G. semiinvoluta Zone, Possagno Section, northern Italy];
fig. 7 [upper Eocene G. semiinvoluta Zone, DSDP
Site 522, South Atlantic Ocean];
fig. 8-11 (from Bolli, 1972);
fig. 12- 14 [upper Eocene G. semiinvoluta Zone,
DSDP Site 363, South Atlantic Ocean]
? 1983 Globigerinatheka semiinvoluta Keijzer. - Pujol : pl. 8; fig. 7, ?8 [upper Eocene Zone P 15-1 6, DSDP Hole
5 16F, Rio Grande Rise, South Atlantic Ocean]
1986 Porticulasphaera semiinvoluta Keijzer. - Molina et al. : pl. 1; fig. 6a-b [upper Eocene Porticulasphaera semiinvoluta
Zone, Fuente Caldera Section, south-east Spain]
non 1991 Globigerinatheka cf. semiinvoluta Keijzer. - Miller et al. : p.35 Appendix 1; fig. 1-8 [upper Eocene Zone
P15, DSDP Site 612, western North Atlantic]; (= G.
tropicalis)
1995 Globigerinatheka semiinvoluta Keijzer. - Poag & Commeau : pl. 5; fig. 14 [upper Eocene Zone P15, Exmore core, Salisbury
Embayment, Virginia-Maryland]
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Was used in synonym list of: |
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Specimen: |
Smithsonian Museum of Natural History, Washington, D.C., Inventory number: USNM 5726a
Smithsonian Museum of Natural History, Washington, D.C., Inventory number: USNM 5726b
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References: |
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Beckmann,J.P. (1953): Die Foraminiferen der Oceanic Formation (Eocaen-Oligocaen) von Barbados. KI. Antillen . Eclogae Geologicae Helvetiae Vol. 46 p. 301-412
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
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
Eckert,H.R.. (1963): Die obereeozaen Globigerinen-Schiefer (Stadund Schimbergerschiefer) zwischen Pilatus und Schrattenfluh . Eclogae Geologicae Helvetiae Vol. 56 p. 1001-1072
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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
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