Catalog - Rugoglobigerina milamensis Catalog - Rugoglobigerina milamensis

CATALOG OF ORIGINAL DESCRIPTIONS: Rugoglobigerina milamensis Smith&Pessagno 1973

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 -> R -> Rugoglobigerina -> Rugoglobigerina milamensis
Other pages this level: R. alpina, R. jerseyensis, R. kingi, R. lobatula, R. macrocephala macrocephala, R. macrocephala ornata, R. mexicana, R. milamensis, R. praehelvetica, R. pseudorugosa, R. reicheli hexacamerata, R. reicheli pustulata, R. reicheli reicheli, R. rugosa pennyi, R. rugosa rotundata, R. spinosa, R. tradinghousensis

Rugoglobigerina milamensis

Citation: Rugoglobigerina milamensis Smith&Pessagno 1973
Taxonomic rank: species
Described on page(s) : 56-7
Type specimens: Plate 24, figures 4-7; 170544
Type sample (& lithostrat): TX9AD, dark gray, conchoidal fracturing, calcareous mudstone, about 8.5 feet above base of expo­sure.
Type age (chronostrat): Maastrichtian
Type locality: Bluff along the southern bank of Walkers Creek, 5.6 miles N. 21 degrees East of Cameron, Milam County, TX, USA.
Type repository: Washington; USNM

Linked specimens: USNM-170546 USNM-170545 USNM-170544

Current identification/main database link: Rugoglobigerina milamensis Smith and Pessagno 1973


Original Description

Test trochospiral, strongly spiroconvex, early whorls offset in a higher plane than ultimate whorl; peripheral margin subcircular, lobate; 5-6 chambers in the final whorl spherical to subspherical, in apertural and abapertural views slightly elongate axially, ultimate chamber slightly offset umbilically; initial chambers on spiral side increasing rapidly in size as added, chambers of final whorl increasing only slightly in size; sutures radial, curved, strongly, depressed; chambers of ultimate whorl heavily rugose, rugosities or costellae closely spaced, aligned in a meridional pattern, ultimate chamber generally more finely rugose; wall finely perforate; umbilicus large, subrectangular, deep; primary aperture interiomarginal, umbilical; spiral system of tegilla with intralaminal and infralaminal accessory apertures poorly preserved in specimens examined.

Size:
Holotype measures 435 µm in length, 415 µm in width, and 340 µm in maximum thickness.

Etymology:
named after Milam County, Texas.

Extra details from original publication
Remarks.-Rugoglobigerina milamensis, n. sp., has been previously figured (see synonymy) as R. rugosa (Plum­mer). It differs from the latter species in being much more strongly trochospiral, and in having a slight rather than rapid increase in chamber size. Rugoglobigerina milamen­sis differs from R. rotundata Bronnimann in being more trochospiral, in having chambers which, in apertural view, are not strongly elongate axially, in having coarse and well­ developed meridional rugosities, and in having a large rather than small umbilicus. It differs from R. trading­ housensis Pessagno (= ? R. pilula Belford) in having strongly developed meridional rugosities or costellae on all chambers of the ultimate whorl, and in having a much larger umbilicus.

Range.-G. contusa-stuartiformis Assemblage Zone, G. gansseri Subzone, lower part of G. aegyptiaca Zonule, to upper part of A. mayaroensis Subzone (insofar known).

Occurrence.-Rugoglobigerina milamensis, n. sp., has been figured previously as R. rugosa from the Maestrich­tian of Denmark (Berggren, 1962); Pemberger Folge (Maestrichtian) of Austria (van Hinte, 1963); and the Redbank and Mt. Laurel Formations (Maestrichtian) of New Jersey (Olsson, 1964). Douglas and Sliter (1966) figured this form as R. rotundata Bronnimann from the Marsh Creek Formation of Contra Costa County, Cali­fornia.

During the present investigation, this species was ob­served in the Corsicana Formation (middle Maestrichtian, G. aegyptiaca Zonule) along Onion Creek, Travis County, Texas; Corsicana Formation (middle Maestrichtian, R. fructicosa Zonule) of North Central Texas; Papagallos Shale (middle Maestrichtian, R. fructicosa Zonule) of Mexico (see Appendix, Pessagno sample MXI74); Men­dez Shale (late Maestrichtian, A. mayaroensis Subzone) of Mexico (Pessagno sample MX78); and the Guayaguay­ are Formation (late Maestrichtian, A. mayaroensis Sub­zone) of Trinidad.

References:

Smith, C. C. & Pessagno, E. A. (1973). Smith, C. C. & Pessagno, E. A. (1973). Planktonic foraminifera and stratigraphy of the Corsicana formation (Maestrichtian) North-central Texas. Cushman Foundation for Foraminiferal Research, Special Publication. 12: 1-67. Cushman Foundation for Foraminiferal Research, Special Publication. 12: 1-67. gs O


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Rugoglobigerina milamensis compiled by the pforams@mikrotax project team viewed: 18-7-2025

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