Globigerinelloides blowi Bolli 1959 from: Leckie, M.R. (1990): Middle Cretaceous Planktonic Foraminifers of the Antarctic Margin: Hole 693A, ODP Leg 113. In: Proceedings of the Ocean Drilling Programme Vol. 113 Eds: Parker, P.F..Kennett, J.P.O'Connell, S..Pisias, N.G. p. 319-324 . |
Notice: This catalogue page may contain unedited data.
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Species Globigerinelloides blowi Bolli 1959 |
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Diagnosis / Definition: |
Leckie (1990):
Test small (0.10-0.15 mm), evolute. Five to six smooth,
inflated, subspherical to ovoid chambers in the final whorl. Chambers increase gradually in size as added. Umbilicus wide. Aperture a low arch with thin lip; relict apertures not discernible. |
Discussion / Comments: |
Caron (1985):
Bolli (1959) distinguished two species on the basis of spherical as against laterally compressed chambers, as did Chevalier (1961) with his two species.
G. blowi differs from G. subcarinata in the absence of an acute axial margin, from G. ultramicra in having fewer chambers.
Leckie (1990):
Typical specimens of Globigerinelloides blowi s.l. have
four to five chambers in the final whorl (Masters, 1977; Leckie, 1984),although Longoria (1974, pl. 4, fig. 7) illustrates a specimen with as many as seven. Specimens from Hole 693A have five to six chambers in the final whorl.
Six-chambered forms bear a strong resemblance to G. aptiense Longoria (see illustrations by Longoria, 1974, and Leckie, 1984). G. blowi s.l. is characterized by its distinctive small size, smooth surface, and inflated chambers. G. aptiense tends to be larger, up to 0.40 mm according
to Longoria (1974). In addition, the overall chamber shape and arrangement differ from G. blowi s.l., and G. aptiense lacks the smooth surface of G. blowi s.l. Therefore, despite having as many as six chambers in the final whorl, the specimens from Hole 693A are assigned to the G. blowi group.
Leckie (1984) noted that G. blowi s.l. is particularly common through the upper Aptian of DSDP Site 545 (eastern North Atlantic), and then becomes rare in lower and middle Albian strata.
Pflaumann & Krasheninnikov (1977):
Five to six chambers form the involute last coil. Umbilicus
shallow, wide.
This species had been recorded from Aptian strata of Trinidad,
France, Bavaria, Mexico, and Spain. Longoria (1974) reported its
range from early Aptian to Hedbergella gorbatchikae Zone (late
Aptian). |
Systematics: |
5 Classis Foraminifera
Familia Planomalinidae
Genus Globigerinelloides
Species Globigerinelloides blowi
22 Superfamilia Globigerinaceae
Familia Schackoinidae
Genus Globigerinelloides
Species Globigerinelloides blowi
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Synonym list: |
Caron (1985):
Leckie (1990):
Pflaumann & Krasheninnikov (1977):
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Was used in synonym list of: |
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References: |
Bolli,H.M. (1959): Planktonic foraminifera from the Cretaceous of Trinidad, B.W.I. . Bulletins of American Paleontology Vol. 39 p. 257-277
Chevalier,J. (1961): Quelques nouvelles espèces dans le Cretaceinférieur méditerranéen . Revue de Micropaléontologie Vol. 4 p. 30-36
Longoria,J.F. (1974): Stratigraphic, morphologic and taxonomic studies of Aptian planktonic Foraminifera . Revista Espanola de MicropaleontologíaNo extraord p. 1-107
Pflaumann,U. and Krasheninnikov,V.. (1977): Early Cretaceous planktonic foraminifers from eastern North Atlantic, DSDP Leg 41 . In: Initial Reports of the Deep Sea Drilling Project 41 , Abidjan, Ivory Coast, to Malaga, Spain, February-April 1975 Eds: Gardner, J..Herring, J.. p. 539-564
Leckie,M.R. (1984): Mid-Cretaceous planktonic foraminiferal biostratigraphy off Morocco, Deep Sea Drilling Project Leg 79, Sites 545 and 547 . Initial Reports of the Deep Sea Drilling Project Vol. 79 p. 579–620
Caron,M. (1985): Cretaceous planktic foraminifera. In: Plankton stratigraphy Eds: Bolli, H.M.Saunders, J.B.Perch-Nielsen, K. p. 17–86
Leckie,M.R. (1990): Middle Cretaceous Planktonic Foraminifers of the Antarctic Margin: Hole 693A, ODP Leg 113. In: Proceedings of the Ocean Drilling Programme Vol. 113 Eds: Parker, P.F..Kennett, J.P.O'Connell, S..Pisias, N.G. p. 319-324
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