Catalog - Globigerina increbescens Catalog - Globigerina increbescens

CATALOG OF ORIGINAL DESCRIPTIONS: Globigerina increbescens Bandy 1949

This page provides data from the catalog of type descriptions. The catalog is sorted alphabetically. Use the current identification link to go back to the main database.

Higher levels: pf_cat -> G -> Globigerina -> Globigerina increbescens
Other pages this level: << < G. hoelzli, G. hofkeri, G. hornibrooki, G. horrida, G. hoterivica, G. hybrida, G. inaequispira, G. inaequispira angusta, G. inaequispira incluta, G. inaequispira testata, G. inaequispira transversa, G. inaequispira universa, G. incisa, G. incompta, G. inconstans, G. increbescens, G. incretacea, G. inflata, G. infracretacea, G. infracretacea gargasiana, G. infracretacea trochoidea, G. intermedia, G. isahayensis, G. jurassica, G. juvenilis, G. kelleri, G. khadumica, G. kochi, G. kondoi, G. konkensis, G. kozlowskii> >>

Globigerina increbescens

Citation: Globigerina increbescens Bandy 1949
taxonomic rank: Species
Type specimens: Plate 23, figs. 3a-c; Holotype.—No. 4904; desc p. 120-1
Type sample (& lithostrat): Jackson
Type age (chronostrat): Eocene
Type locality: Little Stave Creek, Clarke County, Alabama, locality 58
Type repository: Indiana University Micropaleontological collections,

Current identification/main database link: Turborotalia increbescens (Bandy 1949)

Original Description

Test helicoid, dorsal side slightly-convex. ventral side very deep as a result of a rapid increase in height of the chambers; periphery moderately lobulate: edge evenly rounded ; whorls about three, the last with four chambers; sutures depressed, slightly curved; wall coarsely and conspicuously perforate; aperture a moderately high arch on the ventral side extending- from near umbilicus to near peripliery, with upper lip. Abundant.

Diameter 0.48 mm.; height, 0.38 mm.

Extra details from original publication
This form is more coarsely perforate than G. inflata d'Orbigny, 1839 (p134, pl. 2, figs. 7-9) and is not so high, the spire is more rounded, and the aperture is much shorter.


Bandy, O. L. (1949). Eocene and Oligocene foraminifera from Little Stave Creek, Clarke County, Alabama. Bulletins of American Paleontology. 32(131): 1-210. gs

d'Orbigny, A. (1839b). Foraminifères des Iles Canaries. In, Barker-Webb, P. & Berthelot, S. (eds) Histoire naturelle des Iles Canaries. 120-146. 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 O

Pearson, P. N., Olsson, R. K., Spezzaferri, S. & Leckie, R. M. (2018a). Taxonomy, biostratigraphy, and phylogeny of Oligocene Globanomalinidae (Turborotalia and Pseudohastigerina). 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 14): 403-414. gs


Globigerina increbescens compiled by the pforams@mikrotax project team viewed: 21-7-2024

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