We have observed extreme variants in ODP Site 865 (equatorial mid Pacific Ocean – see Pl. 15.1, Fig. 11). Morphometric studies (P .N. Pearson, unpublished data) show that it is a separate species from T. pomeroli, although the two intergrade in the lower part of the range of altispiroides. Its extinction in Zone E14 may prove to be a useful marker horizon, although it needs further documentation. [Pearson et al. 2006]
Catalog entries: Turborotalia altispiroides
Type images:Distinguishing features:
Parent taxon (Turborotalia): Trochospiral with umbilical-extraumbilical aperture.
Wall smooth pustulose, can be weakly cancellate, & may defoliate.
This taxon: Like T. pomeroli but higher spire, dorso-ventrally extended chambers, usually more chambers in the final whorl, and more umbilically-centered aperture.
Morphology:
Wall type:
cancellate, especially on earlier chambers; tendency to defoliate. [Pearson et al. 2006]
Size:
Character matrix
test outline: | Subcircular | chamber arrangement: | Trochospiral | edge view: | Spiroconvex | aperture: | Umbilical-extraumbilical |
sp chamber shape: | Petaloid | coiling axis: | Moderate-high | periphery: | N/A | aperture border: | Thin lip |
umb chbr shape: | Subtriangular | umbilicus: | Wide | periph margin shape: | Broadly rounded | accessory apertures: | None |
spiral sutures: | Weakly depressed | umb depth: | Deep | wall texture: | Moderately pustulose | shell porosity: | Finely Perforate: 1-2.5µm |
umbilical or test sutures: | Moderately depressed | final-whorl chambers: | 4.5-6 | N.B. These characters are used for advanced search. N/A - not applicable |
Geographic distribution
Aze et al. 2011 summary: Cosmopolitan; based on Pearson et al. (2006)
Isotope paleobiology
Aze et al. 2011 ecogroup 2 - Open ocean mixed-layer tropical/subtropical, without symbionts. Based on _13C lighter than species with symbionts; also with relatively light _18O. Sources cited by Aze et al. 2011 (appendix S3): Pearson et al. (2001a)
Phylogenetic relations
Most likely ancestor: Turborotalia pomeroli - at confidence level 4 (out of 5). Data source: Pearson et al. (2006), fig 15.1.
Geological Range:
Notes: Middle Eocene, upper Zone E11 to lower Zone E14. [Pearson et al. 2006]
Last occurrence (top): in lower part of E14 zone (30% up, 37.4Ma, in Priabonian stage). Data source: Pearson et al. (2006), fig. 15.1
First occurrence (base): in upper part of E11 zone (80% up, 40.7Ma, in Bartonian stage). Data source: Pearson et al. (2006), fig. 15.1
Plot of occurrence data:
Primary source for this page: Pearson et al. 2006 - Eocene Atlas, chap. 15, p. 438
Beckmann, J. P. (1953). Die Foraminiferen der Oceanic Formation (Eocaen-Oligocaen) von Barbados, Kl. Antillen. Eclogae Geologicae Helvetiae. 46(2): 301-412. gs O Bermudez, P. J. (1937b). Nuevas especies de Foraminiferos del Eoceno de Cuba. Memorias de la Sociedad Cubana de Historia Natural “Felipe Poey”. 11: 137-150. gs Bermudez, P. J. (1961). Contribucion al estudio de las Globigerinidea de la region Caribe-Antillana (Paleoceno-Reciente). Editorial Sucre, Caracas. (3): 1119-1393. gs Bolli, H. M. (1957a). Planktonic foraminifera from the Eocene Navet and San Fernando formations of Trinidad. 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: 155-172. gs Pearson, P. N., Premec-Fucek, V. & Premoli Silva, I. (2006b). Taxonomy, biostratigraphy, and phylogeny of Eocene Turborotalia. In, Pearson, P. N., Olsson, R. K., Hemleben, C., Huber, B. T. & Berggren, W. A. (eds) Atlas of Eocene Planktonic Foraminifera. Cushman Foundation for Foraminiferal Research, Special Publication . 41(Chap 15): 433-460. gs OReferences:
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Turborotalia altispiroides compiled by the pforams@mikrotax project team viewed: 6-2-2025
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