Subbotina gortanii Borsetti 1959 from: Spezzaferri, S.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 . |
Notice: This catalogue page may contain unedited data.
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Species Subbotina gortanii Borsetti 1959 |
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Diagnosis / Definition: |
Pearson et al. (2006):
DESCRIPTION.
Type of wall: Cancellate, normal perforate,
spinose, ruber/sacculifer-type wall texture.
Test morphology: High trochospiral, globular in
outline, chambers globular; in spiral view 4 globular,
loosely embracing chambers in ultimate whorl,
increasing moderately in size, sutures deeply depressed, straight; in umbilical view 4 globular, loosely embracing
chambers, increasing moderately in size, sutures deeply
depressed, straight, umbilicus large, enclosed by
surrounding chambers, aperture umbilical, bordered by
a thickened, narrow rim; in edge view chambers arranged
in a high, loosely coiled spire.
Size: Maximum diameter of holotype 0.60 mm,
thickness 0.63 mm. |
Discussion / Comments: |
Spezzaferri & Silva (1990):
Very rare.
Pearson et al. (2006):
DISTINGUISHING FEATURES.-
The species is
characterized by its trochospiral loosely coiled test,
globular chambers, and umbilical aperture.
DISCUSSION.-
Blow (1979) regarded Globigerina
gortanii gortanii as the senior synonym of Globigerina
turritilina turritilina Blow and Banner, but retained the
separation of this form from Globigerina turritilina
praeturritilina Blow and Banner. Blow and Banner
(1 962) separated Globigerina turritilina turritilina from
Globigerina turritilina praeturritilina on the basis of
slightly less inflated chambers, a broader umbilicus, and
a higher aperture in G. turritilina praeturritilina. The
holotypes of Blow and Banner's subspecies are
illustrated for the first time in SEM on Plate 6.10, Figs.
9-12 and show little difference between the two
morphotypes in these characters.
Khalilov's Globigerina pseudocorpulenta is a
high-spired form that Blow (1979) considered a possible
senior synonym of praeturritilina. The holotype was
viewed by WAB who was unable to place the specimen
unequivocally, hence we hold it in questionable
synonymy with gortanii but recommend suppression of the name.
PHYLOGENETIC RELATIONSHIPS.-
Subbotina
gortanii appears related to Subbotina yeguaensis, which
has a moderately elevated spire of loosely embracing,
globular chambers and a ruber/sacculifer-type wall texture. An increase in the height of the coil would lead to the development of the gortanii morphology.
GEOGRAPHIC D1STNBUTION.-
Apparently global in low to mid latitudes.
STABLE ISOTOPE PALEOBIOLOGY.-
Pearson and others (2001) recorded this species (as S. cf. S. praeturritilina) as a deep dwelling form in the upper Eocene. However Douglas and Savin (1978) and Boersma and others (1987) recorded relatively negative ň18O for this species from the Oligocene, suggesting that it might have migrated into shallower water habitats. |
Systematics: |
22 Species Subbotina gortanii
Species Turborotalia increbescens
Species Turborotalia pseudoampliapertura
35 Ordo Foraminiferida
Superfamilia Globigerinaceae
Familia Globigerinidae
Genus Subbotina
Species Subbotina gortanii
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Synonym list: |
Spezzaferri & Silva (1990):
Pearson et al. (2006):
1959 Catapsydrax gortanii Borsetti. - Borsetti : p.205 pl. 1; fig. 1a-d (1a-c = holotype) [lower Oligocene, Piacenza Province,
northern Italy]
1979 Globigerina gortanii gortanii Borsetti. - Blow : p.851 pl. 17, fig. 1 [reillustration of Blow, 1969, pl. 17: fig. l];
pl. 247, fig. 4 [lower Oligocene Zone 0213, DSDP Site 14, central South Atlantic Ocean];
pl. 251, fig. 9 [upper Oligocene Zone 06, DSDP Site 14, central South Atlantic Ocean]
1983 Globigerina gortanii Borsetti. - Pujol : p.651 pl. 11, fig. 4 [lower Oligocene Zone 03, DSDP Hole 5 16F, Rio Grande Rise, southwest South Atlantic Ocean];
pl. 15, fig. 4 [Zone N516, DSDP Site 516, Rio Grande Rise, southwest South Atlantic Ocean]
1985 Globigerina gortanii Borsetti. - Snyder & Waters : p.459 pl. 1; fig. 16-18 [upper Oligocene Zone 05,
DSDP Hole 549A, Goban Spur, eastern North Atlantic
Ocean]
2006 Subbotina gortanii Borsetti. - Pearson et al. : p.136 pl. 10; fig. 1-17 (Pl. 6.1 0, Figs. 1-3: new SEMs of holotype of
Globigerina turritilina turritilina Blow and Banner); (Pl. 6.10, Figs. 9- 12: new SEMs of holotype of
Globigerina turritilina praeturritilina Blow and
Banner)
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Specimen: |
Institute of Geology and Paleontology, University of Bologna, Italy, Inventory number: IF - 376
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References: |
Khalilov,D.M. (1956): O pelagicheskoy faune foraminifer Paleogenovykh otlozheniy Azerbaydzhana . Trudy Instituta Geologii, Akademiya Nauk Azerbaydzhanskoy SSR Vol. 17
Borsetti,A.M. (1959): Tre nouvi Foraminiferi planctonici dell'Oligocene piacentino . G. Geol. Vol. 27 p. 205-212
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
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
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
Snyder,S.W. and Waters,V.J. (1985): Cenozoic planktonic foraminiferal biostratigraphy of the Goban Spur region. In: Deep Sea Drilling Project Vol. 80
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
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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