Globigerinatheka euganea Proto Decima & Bolli 1970 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 euganea Proto Decima & Bolli 1970 |
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| Diagnosis / Definition: |
Pearson et al. (2006):
DESCRIPTION.
Type of wall: Spinose, cancellate, with rather
dense pores, about 0.08 mm in diameter.
Test morphology: Test almost spherical, mainly
2 to possibly 2 1/2 early whorls coiled in a low trochospire
consisting of four to six inflated chambers; chambers
initially increase very slowly in size as they are added,
then more rapidly, becoming more globular; the last 3
chambers, which increase very rapidly in size, are
streptospirally coiled with the last chamber tending to
be hemispherical and covering the umbilicus of previous
whorls; the last chamber may be of the same size as the
penultimate one or larger; sutures distinct, weakly
depressed in the earlier whorl becoming clearly
depressed in the intermediateflhorls, tending to be less
depressed between the last chambers; primary aperture
covered in the adult stage; two to three, occasionally
four small arched to subcircular secondary apertures
along the base of the last chamber at the junctions of
previous chambers, that may be covered by small bullae.
Size: Maximum diameter of holotype 0.53 mm. |
| Discussion / Comments: |
Pearson et al. (2006):
DISTINGUISHING FEATURES.-
Globigerinatheka
euganea has a compact, spherical test, with small,
numerous secondary apertures in some specimens. It
differs from G. curryi by having a more compact test, a
tighter inner coil and more numerous and smaller
secondary apertures. It differs from G. luterbacheri by
having a more spherical test and less depressed sutures;
it differs from beckmanni by less numerous, slightly
larger secondary apertures, rarely recorded along the
inner spire, and by the absence of area1 openings.
DISCUSSION.-
At first sight G. euganea looks similar
to Cushman's original drawing of the G. mexicana holotype, as redrawn by Blow and Saito (1968a).
However, the SEM photographs of the mexicana
holotype clearly show that the two species are not
conspecific.
PHYLOGENETIC RELATIONSHIPS.-
According to
Bolli (1972), G. euganea is the intermediate member of
the curryi - euganea - beckmanni lineage.
GEOGRAPHIC DISTRIBUTION.-
Low to midlatitudes.
Large specimens mainly in tropical regions or
warmer mid latitudes.
STABLE ISOTOPE PALEOBIOL0GY.-
No data available. |
| Systematics: |
35 Ordo Foraminiferida
Superfamilia Globigerinaceae
Familia Globigerinidae
Genus Globigerinatheka
Species Globigerinatheka euganea
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| Synonym list: |
Pearson et al. (2006):
p 1953 Globigerinoides mexicana Cushman. - Beckmann : p.395 pl. 25; fig. 15, 16 (not figs. 17-19 =
0. beckmanni); [Eocene, Oceanic Fm., Barbados]; [Not
Cushman, 1925]
1960 Globigerapsis mexicana Cushman. - Todd & Low : pl. 259; fig. 7 [drill hole, Eniwetok, central Pacific
Ocean]
1962 Globigerapsis mexicana Cushman. - Saito : pl. 34; fig. 7a-c (not 6a-b) [Eocene, Hahajima, Hillsborough Island, Japan]; [Not
Cushman, 1925]
1970 Globigerinatheka euganea Proto Decima & Bolli. - Proto Decima & Bolli : p.894 pl. I, fig. 6-11;
pl. III, fig. 3-5;
text-fig. 8-15, 31-31a, 43-45b (holotype);
pl. I, fig. 7 (paratype);
pl. I, fig. 8;
pl. III, fig. 4;
text-fig. 40-42a [middle Eocene Orbulinoides
beckmanni Zone, Euganei marls, Cava Zillo, northern
Italy]
1970 Globigerapsis cf. kugleri Bolli et al.. - Baumann : pl. 1; fig. 13a, b [middle Eocene
Glohorotalia centralis Zone, probably P12, Bottaccione
Section, Gubbio, central Italy]; [Not Bolli, Loeblich and
Tappan, 1957]
1970 Globigerinatheka barri Brönnimann. - Baumann : pl. 3; fig. 1 [middle Eocene Globigerapsis mexicana Zone,
Scalette Section, Umbria, central Italy]; [Not Bronnimann,
1952]
1972 Globigerinatheka subconglobata euganea Proto Decima & Bolli. - Bolli : p.132 text-fig. 31-34 (redrawn from Proto Decima and Bolli, 1970);
text-fig. 35 (redrawn from Cushman, 1927);
text-fig. 36-38 (redrawn from Beckmann, 1953); text-fig. 39 (redrawn from Todd and Low, 1960);
text-fig. 40-42 (redrawn from Saito, 1962)
1975 Globigerinatheka euganea Proto Decima & Bolli. - Toumarkine : pl. 4; fig. 13, 14 [middle
Eocene Orbulinoides beckmanni Zone, DSDP Site 3 13,
Mid-Pacific Mountains]
p 1979 Globigerapsis kugleri euganea Decima & Bolli. - Blow : p.1149 pl. 181, fig. 6;
pl. 183, fig. 5, 6;
pl. 185, ?fig. 6 [middle Eocene Zone P1l, DSDP Hole 21A, South Atlantic Ocean];
pl. 186 (partim), ?fig. 4 (not fig. 5 = G. euganea), [middle Eocene Zone P12, DSDP Site 19,
South Atlantic Ocean];
pl. 192 (partim), fig. 4 (not fig. 2, 3), [middle Eocene Zone P13, Kilwa area, Tanzania]
1979 Globigerapsis beckmanni Saito. - Blow : p. 1137-1138 pl. 192; fig. 6-9, ?fig. 5 [middle Eocene Zone P13, Kilwa
area, RS.3 11, Tanzania]; [Not Saito, 1962]
1983 Globigerinatheka subconglobata euganea Proto Decima & Bolli. - Toumarkine : pl. 21; fig. 8-10 [fig. 8, middle Eocene Orbulinoides beckmanni Zone,
DSDP Site 313, Mid Pacific Mountains; fig. 9, middle
Eocene Morozovella lehrzeri zone, DSDP Site 313, Mid
Pacific Mountains; fig. 10, middle Eocene Orbulinoides
beckmanni Zone, DSDP Site 363, S
? 1983 Globigerinatheka barri Brönnimann. - Pujol : pl. 8; fig. 12 [upper Eocene Zone P15-16, DSDP Hole 516F.
Rio Grande Rise, South Atlantic Ocean]. [Not
Bronnimann, 1952]
2006 Globigerinatheka euganea Proto Decima & Bolli. - Pearson et al. : p.182 pl. 7.4; fig. 1-8, 11, 12 (Pl. 7.4, Figs. l, 2: reillustration of holotype and
paratype of Globigerinatheka euganea Proto Decima
and Bolli)
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| Specimen: |
National Museum of Natural History, Basel, Inventory number: C 26543
National Museum of Natural History, Basel, Inventory number: C 26529
National Museum of Natural History, Basel, Inventory number: C 26530
National Museum of Natural History, Basel, Inventory number: C 26531
National Museum of Natural History, Basel, Inventory number: C 26544
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| References: |
Cushman,J.A. (1927): Some characteristic Mexican fossil foraminifera . Journal of Paleontology Vol. 1 p. 147-172
Beckmann,J.P. (1953): Die Foraminiferen der Oceanic Formation (Eocaen-Oligocaen) von Barbados. KI. Antillen . Eclogae Geologicae Helvetiae Vol. 46 p. 301-412
Todd,R. and Low,D. (1960): Smaller foraminifera from Eniwetok drill hole . U.S. Geological Survey, Professional paper 260-X p. 799-861
Saito,T. (1962): Eocene planktonic foraminifera from Hahajima (Hillsborough Island) . Trans. Proc. Paleontol. Soc. Japan, news series Vol. 45 p. 209-225
Baumann,P.. (1970): Mikropalaentologische und stratigraphische Untersuchungen der obereozaenen-oligozaenen Scaglia im zentralen Apennin (Italien) . Eclogae Geologicae Helvetiae Vol. 63 p. 1133-1211
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
Toumarkine,M. (1975): Middle and Late Eocene planktonic foraminifera from the northwestern Pacific, Leg 32 of the Deep Sea Drilling Project. In: Initial Reports of the Deep Sea Drilling Project Vol. 32 Eds: Larson, R.L.Moberly, R. p. 735-751
Toumarkine,M. (1978): Planktonic Foraminiferal Biostratigraphy of the Paleogene of Sites 360 to 364 and the Neogene of Sites 362A, 363, and 364 Leg 40. In: Initial Results of the Deep Sea Drilling Project Vol. 40
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
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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