Catalog entries: Globorotalia crassula, Globorotalia hirsuta aemiliana, Globorotalia crotonensis
Type images:Distinguishing features:
Parent taxon (truncatulinoides lineage): G. crasula - crassaformis - tosaensis - truncatulinoides lineage, predominantly conicotruncate
This taxon: Like G. cibaoensis but with more nearly planoconvex test and more strongly angled periphery
Morphology:
Wall type:
Character matrix
test outline: | Lobate | chamber arrangement: | Trochospiral | edge view: | Planoconvex | aperture: | Umbilical-extraumbilical |
sp chamber shape: | Crescentic | coiling axis: | Low | periphery: | N/A | aperture border: | Thin lip |
umb chbr shape: | Subtriangular | umbilicus: | Narrow | periph margin shape: | Subangular | accessory apertures: | None |
spiral sutures: | Flush | umb depth: | Shallow | wall texture: | Smooth | shell porosity: | Macroperforate: >2.5µm |
umbilical or test sutures: | Weakly depressed | final-whorl chambers: | 4-4 | N.B. These characters are used for advanced search. N/A - not applicable |
[SCOR WG138]
Geographic distribution
Isotope paleobiology
Phylogenetic relations
Globorotalia aemiliana Colalongo and Sartoni, and Globorotalia crotonensis Conato and Follador are morphologically similar to Gr. (T.) crassula and probably represent no more than phenotypic variants or subspecies of this form.
Gr. ( T.) crassula may have evolved from Gr. (H.) cibaoensis in temperate-Subantarctic areas of the South Pacific and is the possible ancestor of Gr. (T.) crassaformis (Galloway and Wissler). At DSDP Site 281, we have observed gradation between Gr. (H.) cibaoesis and Gr. (T.) crassula. A possible ancestry between Gr. (T.) crassula and Gr. (T.) crassaformis is inferred. [Kennett & Srinivasan 1983]
Most likely ancestor: Globorotalia cibaoensis - at confidence level 3 (out of 5). Data source: Kennett & Srinivasan 1983, fig 16Stewart 2003 fig. 6.10; Aze et al. 2011, appendix 5.
Likely descendants: Globorotalia crassaformis;
plot with descendants
Geological Range:
Last occurrence (top): within N21 zone (1.93-3.10Ma, top in Gelasian stage). Data source: Chaisson & Pearson (1997)
First occurrence (base): within N18 zone (5.20-5.72Ma, base in Messinian stage). Data source: Chaisson & Pearson (1997)
Plot of occurrence data:
Primary source for this page: Kennett & Srinivasan 1983, p.144
Banner, F. T. & Blow, W. H. (1960a). Some primary types of species belonging to the superfamily Globigerinaceae. Contributions from the Cushman Foundation for Foraminiferal Research. 11: 1-41. gs O Blow, W. H. (1969). Late middle Eocene to Recent planktonic foraminiferal biostratigraphy. In, Bronnimann, P. & Renz, H. H. (eds) Proceedings of the First International Conference on Planktonic Microfossils, Geneva, 1967. E J Brill, Leiden 380-381. gs Cita, M. B. (1973). Pliocene biostratigraphy and chronostratigraphy. Initial Reports of the Deep Sea Drilling Project. 13: 1343-1379. gs Cushman, J. A., Stewart, R. E. & Stewart, K. C. (1930). Tertiary foraminifera from Humboldt county, California. Transactions of the San Diego Society of Natural History. 6(2): 41-94. gs Kennett, J. P. & Srinivasan, M. S. (1983). Neogene Planktonic Foraminifera. Hutchinson Ross Publishing Co., Stroudsburg, Pennsylvania. 1-265. gs Lam, A. & Leckie, R. M. (2020a). Late Neogene and Quaternary diversity and taxonomy of subtropical to temperate planktic foraminifera across the Kuroshio Current Extension, northwest Pacific Ocean. Micropaleontology. 66(3): 177-268. gs Shackleton, N. J. & Vincent, E. (1978). Oxygen and carbon isotope studies in Recent Foraminifera from the southeast Indian Ocean. Marine Micropaleontology. 3: 1-13. gsReferences:
Globorotalia crassula compiled by the pforams@mikrotax project team viewed: 11-10-2024
Short stable page link: https://mikrotax.org/pforams/index.php?id=104098 Go to Archive.is to create a permanent copy of this page - citation notes |