Globigerinitahowei Blow and Banner, 1962:109, pl. 14: figs. P-R (holotype) [Globigerapsissemi-involuta Zone, Sample FCRM 1645, Lindi, Tanzania].
Catapsydraxgolicynensis Menkes, 1975:281-282, pl. 1: figs. 1-2 [upper Eocene zone of large globigerinids, Borehole 1, Golitsyn depression, Black Sea].
Not Catapsydrax howei (Blow and Banner). Warraich and Ogasawara, 2001:44, fig. 12: 4-6.
Taxonomic discussion: The loosely coiled test with large circular, infralaminal apertures of Catapsydraxhowei somewhat resembles Recent Globigerinoides, suggesting a shallow habitat in the water column. We illustrate the holotype in SEM for the first time (Pl.5.2, Figs. 9-12) along with newly collected specimens from the type locality (Pl.5.2, Figs. 13-16). Catapsydraxgolicynensis Menkes from the upper Eocene of the Black Sea exhibits the large arched aperture of this species and is a probable synonym. The specimen figured by Warraich and Ogasawara (2001) is a five-chambered form that does not match the morphology of C. howei. [Olsson et al. 2006]
Distinguishing features: Parent taxon (Catapsydrax): Like Globorotaloides but more compact, radially compressed, with appressed inflated chambers in the final whorl, and always with bulla This taxon: Larger, loosely coiled test, with large globular bulla with 3 large, circular, infralaminal apertures
NB These concise distinguishing features statements are used in the tables of daughter-taxa to act as quick summaries of the differences between e.g. species of one genus. They are being edited as the site is developed and comments on them are especially welcome.
Description
Diagnostic characters: Catapsydraxhowei is distinguished from C. africanus by its larger, more loosely coiled test, large globular bulla with large, circular, infralaminal apertures. Catapsydraxglobiformis is smaller, has a spherical-shaped test with a low slightly inflated bulla with small circular, infralaminal apertures. [Olsson et al. 2006] Morphology: Low trochospiral, lobulate test with generally 3 chambers, somewhat loosely coiled, in the final whorl. Chambers inflated, globular increasing rapidly in size with a large globular, inflated bulla covering the umbilicus; in spiral view 3 globular chambers increasing rapidly in size, sutures straight to slightly curved, moderated depressed; in umbilical view dominated by a large inflated bulla with 3 large circular, infralaminal apertures with a continuous, thickened imperforate rim facing each suture; sutures straight, somewhat strongly depressed; in edge view globular in shape with bulla showing one infralaminal aperture opening onto the suture line. [Olsson et al. 2006] Wall type: Cancellate, probably spinose in life, ruber/sacculifer-type wall texture. [Olsson et al. 2006] Size: Holotype maximum diameter 0.54 mm, thickness 0.53 mm. [Olsson et al. 2006]
Character matrix
test outline:
Lobate
chamber arrangement:
Trochospiral
edge view:
Equally biconvex
aperture:
Umbilical
sp chamber shape:
Globular
coiling axis:
Low
periphery:
N/A
aperture border:
Bulla
umb chbr shape:
Globular
umbilicus:
Wide
periph margin shape:
Broadly rounded
accessory apertures:
Infralaminal
spiral sutures:
Strongly depressed
umb depth:
Deep
wall texture:
Cancellate
shell porosity:
Finely Perforate: 1-2.5µm
umbilical or test sutures:
Strongly depressed
final-whorl chambers:
3-3
N.B. These characters are used for advanced search. N/A - not applicable
Biogeography and Palaeobiology
Geographic distributionKnown from tropical to mid latitude sites. [Olsson et al. 2006]
Aze et al. 2011 summary: Low to middle latitudes; based on Olsson et al. (2006c) Isotope paleobiologyNo data available. [Olsson et al. 2006] Aze et al. 2011 ecogroup 4 - Open ocean sub-thermocline. Based on very light _13C and very heavy _18O. Sources cited by Aze et al. 2011 (appendix S3): Keller (1985) Phylogenetic relationsCatapsydraxhowei probably evolved from C. unicavus in the middle Eocene by becoming larger and more loosely coiled, and developing a large, globular, inflated bulla with large circular, infralaminal apertures. [Olsson et al. 2006]
Geological Range: Notes: Zone E9 to E16. [Olsson et al. 2006] Last occurrence (top): within E16 zone (33.90-34.68Ma, top in Priabonian stage). Data source: Olsson et al. 2006 f5.1 First occurrence (base): within E9 zone (43.23-43.85Ma, base in Lutetian stage). Data source: Olsson et al. 2006 f5.1
Plot of occurrence data:
Range-bar - range as quoted above, pink interval top occurs in, green interval base occurs in.
Triangles indicate an event for which a precise placement has been suggested
Histogram - Neptune occurrence data from DSDP and ODP proceedings. Pale shading <50 samples in time bin. Interpret with caution & read these notes
Primary source for this page: Olsson et al. 2006 - Eocene Atlas, chap. 5, p. 72
References:
Blow, W. H. & Banner, F. T. (1962). The mid-Tertiary (Upper Eocene to Aquitanian) Globigerinaceae. In, Eames, F. E., Banner, F. T., Blow, W. H. & Clarke, W. J. (eds) Fundamentals of mid-Tertiary Stratigraphical Correlation. Cambridge University Press, Cambridge 61-151. gs
Menkes, M. A. (1975). Representatives of the genus Catapsydrax in the Eocene deposits of the South Ukraine. Trudyi Instituta Geologii i Geogiziki, Sibiriskoe Otlodelenie, Akademiya Nauk SSSR (Nauka) Moscow. 333: 281-. gs
Olsson, R. K., Pearson, P. N. & Huber, B. T. (2006c). Taxonomy, biostratigraphy, and phylogeny of Eocene Catapsydrax, Globorotaloides, Guembelitrioides, Paragloborotalia, Parasubbotina, and Pseudoglobigerinella n. gen. 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 5): 67-110. gsO
Warraich, M. Y. & Ogasawara, K. (2001). Tethyan Paleocene-Eocene planktic foraminifera from the Rakhi Nala and Zinda Pir land sections of the Sulaiman Range, Pakistan. Science Reports of the Institute of Geosciences, University of Tsukuba. 22: 1-59. gs
Catapsydrax howei compiled by the pforams@mikrotax project teamviewed: 13-11-2025