arrayname: original
(Note: This synonymy list is restricted to taxonomically important works and Oligocene occurrences) The holotype of D. globosa is from the lower Miocene, and Bolli’s original concept was that globosa was a more globular subspecies of D. altispira. The paratype (Pl. 11.6, Figs. 5-7) appears to be a juvenile specimen and may not belong to this species. Fleisher (1974) suggested that D. globosa was the ancestral form to altispira, and was itself derived from globularis in the Oligocene. We regard Globoquadrina pozonensis Blow as a junior synonym. [Wade et al. 2018]
Catalog entries: Globoquadrina altispira globosa, Globoquadrina pozonensis
Type images:Distinguishing features:
Parent taxon (Dentoglobigerina): Trochospiral test with umbilically restricted aperture and usually one or more umbilical teeth
This taxon: Like D. globularis but with 5-6 chambers in the final whorl leading to a more lobulate outline; also wider umbilicus.
This species is distinguished from D. globularis by having more chambers in the final whorl leading to a more lobulate outline, a wider umbilicus, and from D. altispira by its more rounded chambers. [Wade et al. 2018]
Diagnostic characters:
Morphology:
Wall type:
Character matrix
test outline: | Lobate | chamber arrangement: | Trochospiral | edge view: | Spiroconvex | aperture: | Umbilical |
sp chamber shape: | Globular | coiling axis: | High | periphery: | N/A | aperture border: | Teeth |
umb chbr shape: | Globular | umbilicus: | Wide | periph margin shape: | Broadly rounded | accessory apertures: | None |
spiral sutures: | Moderately depressed | umb depth: | Deep | wall texture: | Cancellate | shell porosity: | Finely Perforate: 1-2.5µm |
umbilical or test sutures: | Strongly depressed | final-whorl chambers: | 5-6 | N.B. These characters are used for advanced search. N/A - not applicable |
Geographic distribution
Isotope paleobiology
Phylogenetic relations
Most likely ancestor: Dentoglobigerina globularis - at confidence level 4 (out of 5). Data source: Wade et al. 2018.
Likely descendants: Dentoglobigerina altispira;
plot with descendants
Geological Range:
Notes: According to Fleisher (1974) this species first appeared in Zone P21. The oldest confirmed illustrated occurrence is from Spezzaferri (1994) from Subzone P21b (Zone O5). It persists through much of the Miocene and possibly part of the Pliocene (e.g., Chaisson and Leckie, 1993); the highest occurrence has not been determined in this study. [Wade et al. 2018]
Last occurrence (top): within Early Pliocene Sub-Epoch (3.60-5.33Ma, top in Zanclean stage). Data source: Kennett & Srinivasan 1983 f20
First occurrence (base): within O5 zone (26.93-28.09Ma, base in Chattian stage). Data source: Wade et al. 2018 f11.1
Plot of occurrence data:
Primary source for this page: Wade et al. 2018 - Olig Atlas chap.11 p.348; Kennett& Srinivasan 1983 p 189
Blow, W. H. (1959). Age, correlation, and biostratigraphy of the upper Tocuyo (San Lorenzo) and Pozon Formations, eastern Falcon, Venezuela. Bulletins of American Paleontology. 39(178): 67-251. gs Bolli, H. M. (1957b). Planktonic foraminifera from the Oligocene-Miocene Cipero and Lengua formations of Trinidad, B.W.I. In, Loeblich, A. R. , Jr., Tappan, H., Beckmann, J. P., Bolli, H. M., Montanaro Gallitelli & E. Troelsen, J. C. (eds) Studies in Foraminifera. U.S. National Museum Bulletin . 215: 97-123. gs Chaisson, W. P. & Leckie, R. M. (1993). High-resolution Neogene planktonic foraminifer biostratigraphy of Site 806, Ontong Java Plateau (Western Equatorial Pacific). Proceedings of the Ocean Drilling Program, Scientific Results. 130: 137-178. gs Fleisher, R. L. (1974a). Cenozoic planktonic foraminifera and biostratigraphy, Arabian Sea, Deep Sea Drilling Project, Leg 23A. Initial Reports of the Deep Sea Drilling Project. 23: 1001-1072. gs O Kennett, J. P. & Srinivasan, M. S. (1983). Neogene Planktonic Foraminifera. Hutchinson Ross Publishing Co., Stroudsburg, Pennsylvania. 1-265. gs Spezzaferri, S. & Premoli Silva, I. (1991). Oligocene planktonic foraminiferal biostratigraphy and paleoclimatic interpretation from Hole 538A, DSDP Leg 77, Gulf of Mexico. Palaeogeography Palaeoclimatology Palaeoecology. 83: 217-263. gs Spezzaferri, S. (1994). Planktonic foraminiferal biostratigraphy and taxonomy of the Oligocene and lower Miocene in the oceanic record. An overview. Palaeontographia Italica. 81: 1-187. gs Stainforth, R. M., Lamb, J. L., Luterbacher, H., Beard, J. H. & Jeffords, R. M. (1975). Cenozoic planktonic foraminiferal zonation and characteristics of index forms. University of Kansas Paleontological Contributions, Articles. 62: 1-425. gs O Wade, B. S., Pearson, P. N., Olsson, R. K., Fraass, A. J., Leckie, R. M. & Hemleben, C. (2018c). Taxonomy, biostratigraphy, and phylogeny of Oligocene and Lower Miocene Dentoglobigerina and Globoquadrina. In, Wade, B. S., Olsson, R. K., Pearson, P. N., Huber, B. T. & Berggren, W. A. (eds) Atlas of Oligocene Planktonic Foraminifera. Cushman Foundation for Foraminiferal Research, Special Publication . 46(Chap 11): 331-384. gs References:
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Dentoglobigerina globosa compiled by the pforams@mikrotax project team viewed: 21-4-2025
Short stable page link: https://mikrotax.org/pforams/index.php?id=104373 Go to Archive.is to create a permanent copy of this page - citation notes |
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