Globoturborotalita ouachitaensis Howe & Wallace 1932 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 Globoturborotalita ouachitaensis Howe & Wallace 1932 |
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Diagnosis / Definition: |
Pearson et al. (2006):
DESCRIPTION.
Type of wall: Cancellate, normal perforate,
spinose, sacculijer-type wall structure.
Test morphology: Test moderately low
trochospiral, globular, lobulate in outline, chambers
globular; in spiral view 4 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 thickened rim;
in edge view chambers globular in shape, slightly embracing, initial spire of chambers slightly elevated. Size: Maximum diameter of holotype 0.19 mm. |
Discussion / Comments: |
Pearson et al. (2006):
DISTINGUISHING FEATURES.-
This specics is
characterized by its small size, 4 globular, slightly embracing, chambers in the ultimate whorl, umbilical aperture, and cancellate, spinose wall texture. It is distinguished from G. bassriverensis by lacking the thick, prominent lip of that species.
DISCUSSION.-
Globoturborotalita ouachitaensis first appears in the middle Eocene where it is a minor component of planktonic foraminiferal assemblages. It is apparently the stem species for the late Eocene radiation of Globoturborotalita. Globigerina turcmenica of Khalilov (1 956) may be a synonym, but due to confusion over the specimens in the collections of Khalilov that are not the same as the illustration of the holotype, and the apparent loss of the holotype, it is
recommended that turcmenica be considered nomen
dubium non consewandum.
PHYLOGENETIC RELATIONSHIPS.-
Globoturborotalita
ouachitaensis is derived fiom Globoturborotalita
bassriverensis n. sp. by an increase in the size of the
aperture and a reduction of the umbilical lip in G.
bassriverensis to an umbilical rim. Conical spine bases
for support of spines are observed in G. ouachitaensis
and may represent a further porphological adaptation.
GEOGRAPHIC DISTRIBUTION.-
Distributed in mid to low latitudes.
STABLE ISOTOPE PALEOBIOLOGY.-
No Eocene data are currently available. |
Systematics: |
35 Ordo Foraminiferida
Superfamilia Globigerinaceae
Familia Globigerinidae
Genus Globoturborotalita
Species Globoturborotalita ouachitaensis
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Synonym list: |
Pearson et al. (2006):
p 1932 Globigerina ouachitaensis Howe & Wallace. - Howe & Wallace : p.74 pl. 10; fig. 5a-b [upper Eocene, Jackson Fm., Danville Landing, Louisana]
1970 Globigerina ouachitaensis Howe & Wallace. - Samanta : p.191 pl. 1; fig. 10-12 [middle Eocene Zone E1 2, Lakhpat, Cutch, western India]
1970 Globigerina officinalis Subbotina. - Samanta : p.191 pl. 1; fig. 2, 3 [middle Eocene Zone E12, Lakhpat, Cutch,
western India]. [Not Subbotina, 1953 .]
1991 Globigerina ouachitaensis Howe & Wallace. - Spezzaferri & Premoli Silva : p.237 pl. 6; fig. 5a-c [upper Oligocene Zone 06, DSPD Hole 538A,
Gulf of Mexico]
2001 Globigerina ouachitaensis Howe & Wallace. - Warraich & Ogasawara : p.46 fig. 15: 3-5 [Zone E14, Kirthar Fm., Sulaiman Range, Pakistan]
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Specimen: |
Smithsonian Museum of Natural History, Washington, D.C., Inventory number: USNM CC18946
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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
Samanta,B.K. (1970): Middle Eocene Planktonic Foraminifera from Lakhpat, Cutch, Western India . Micropaleontology Vol. 16
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
Spezzaferri,S. and Premoli Silva,I. (1991): Oligocene planktonic foraminiferal biostratigraphy and paleoclimatic interpretation from Hole 538A, DSDP Leg 77, Gulf of Mexico . Palaeogeography, Palaeoclimatology, Palaeoecology Vol. 83 p. 217-263
Warraich,M.Y.. and Ogasawara,K.. (2001): Tethyan Paleocene-Eocene planktic foraminifera from the Rakhi Nala and Zinda Pir land sections of the Sulaiman Range, Pakistan . Science Reports of the Institute of Geoscience University of Tsukuba, section B Vol. 22 p. 1-59
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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