NB Globorotalia crassaformis ronda Blow, 1969 and Globorotalia crassaformis viola Blow 1969, and Globorotalia crassaformis hessi Bolli and Premoli Silva, 1973 have also been considered as variants but were separated as distinct species by Aze et al. (2011).
Lam & Leckie (2020) stated that "we do not recognize the different subspecies of Globorotalia crassaformis (e.g., G. viola, G. ronda, G. oceanica). Determining if these subspecies are actually valid are outside the scope of this study, so we refrain from completely synonymizing them with G. crassaformis. Instead, we apply a wide range of intra-species variability to the G. crassaformis species."
Catalog entries: Globigerina crassaformis, Globorotalia (Turborotalia) oceanica, Globorotalia crotonensis, Globorotalia crassacrotonensis
Type images:Distinguishing features:
Parent taxon (truncatulinoides lineage): G. crasula - crassaformis - tosaensis - truncatulinoides lineage, predominantly conicotruncate
This taxon: No keel & flat spiral side
Morphology:
Wall type:
Character matrix
test outline: | Subquadrate | chamber arrangement: | Trochospiral | edge view: | Planoconvex | aperture: | Umbilical-extraumbilical |
sp chamber shape: | Subrectangular | 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 |
Geographic distribution
Most likely ancestor: Globorotalia crassula - at confidence level 2 (out of 5). Data source: Kennet & Srinivasan (1983). NB Stewart (2003 fig. 6.10) & Aze et al. (2011, appendix 5) derive G. crassaformis from G. cibaoensis, however this appears to be in large part due to their adopting an incorrect age for the base of G. crassaformis, hence we revert here to the interpretation of Kennett & Srinivasan (1983) .
Likely descendants: Globorotalia crassaconica; Globorotalia ronda; Globorotalia viola;
plot with descendants
Geological Range:
Last occurrence (top): Extant. Data source: present in the plankton (SCOR WG138)
First occurrence (base): near base of PL2 zone (12% up, 4.3Ma, in Zanclean stage). Data source: Wade et al. (2011), additional event; position within zone determined by linear interpolation from data in table 1 of Wade et al. (2011).
Plot of occurrence data:
Primary source for this page: Kennett & Srinivasan 1983, p.146
Aze, T. et al. (2011). A phylogeny of Cenozoic macroperforate planktonic foraminifera from fossil data. Biological Reviews. 86: 900-927. gs 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 Bolli, H. M. & Premoli Silva, I. (1973). Oligocene to Recent planktonic foraminifera and stratigraphy of the Leg 15 sites in the Caribbean Sea. Initial Reports of the Deep Sea Drilling Project. 15: 475-497. gs Brummer, G. J. A. & Kucera, M. (2014). SCOR/ICBP 138 taxonomy and key to species of modern planktonic foraminfera v2.1. In, Chart distributed at TMS FNG meeting Texel, The Netherlands, June 2014. 1-. gs Brummer, G-J. A. & Kucera, M. (2022). Taxonomic review of living planktonic foraminifera. Journal of Micropalaeontology. 41: 29-74. gs Cifelli, R. & Glacon, G. (1979). New Late Miocene and Pliocene occurrences of Globorotalia species from the North Atlantic; and a paleogeographic review. Journal of Foraminiferal Research. 9(3): 210-227. gs Conato, V. & Follador, U. (1967). Globorotalia crotonensis e Globorotalia crassacrotonensis nuove species del Pliocene Italiano. Bollettino della Societa Geologica Italiana. 84: 555-563. gs Crundwell, M. P. (2018). Globoconella pseudospinosa, n. sp.: A new Early Pliocene planktonic foraminifera from the Southwest Pacific. Journal of Foraminiferal Research. 48(4): 288-300. gs Cushman, J. A. & Bermudez, P. J. (1949). Some Cuban species of Globorotalia. Contributions from the Cushman Laboratory for Foraminiferal Research. 25: 26-45. gs O Galloway, J. J. & Wissler, S. G. (1927). Pleistocene foraminifera from the Lomita Quarry, Palos Verdes Hills, California. Journal of Paleontology. 1(1): 35-87. 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 Loeblich, A. & Tappan, H. (1994). Foraminifera of the Sahul shelf and Timor Sea. Cushman Foundation for Foraminiferal Research, Special Publication. 31: 1-661. gs O Norris, R. D. (1998). Planktonic foraminifer biostratigraphy: Eastern Equatorial Atlantic. Proceedings of the Ocean Drilling Program, Scientific Results. 159: 445-479. gs O Postuma, J. A. (1971). Manual of planktonic foraminifera. Elsevier for Shell Group, The Hague. 1-406. gs Siccha, M. & Kucera, M. (2017). ForCenS, a curated database of planktonic foraminifera census counts in marine surface sediment samples. Scientific Data. 4(1): 1-12. gs Stewart, D. R. M. I. (2003). Evolution of Neogene globorotaliid foraminifera and Miocene climate change. PhD thesis, Bristol University. 1-269. gs OReferences:
Globorotalia crassaformis compiled by the pforams@mikrotax project team viewed: 10-12-2024
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