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.
Linked specimens: USNM-626474
Current identification:
Original Description
Wall.- calcareous, perforate; covered with numerous heavy spines on umbilical side; nearly smooth on spiral side.
Chambers.- angular truncate, 5-6 in final whorl. In- creasing gradually in size as added.
Sutures. -spiral side: gently curved, beaded, raised. Umbilical side: slightly curved somewhat depressed.
Umbilicus.-small, narrow, deep.
Apertures.-primary apertures interiomarginal, umbilical covered by tegilla, and with infralaminal and intralaminal accessory apertures.
Coiling-dominantly dextral.
Size:
Extra details from original publication
Occurrence.-The species occurs commonly in the Navesink formation. It is less common in the Redbank at Atlantic Highlands and New Egypt. It also is lower New Egypt in the Whitesville, Glendola, and Clementon wells
Olsson, R. K. (1960). Olsson, R. K. (1960). Foraminifera of late Cretaceous and earliest Tertiary age in the New Jersey Coastal Plain. Journal of Paleontology. 34(1): 1-58. Journal of Paleontology. 34(1): 1-58. gsReferences:
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Globotruncana monmouthensis compiled by the pforams@mikrotax project team viewed: 18-6-2025
Short stable page link: https://mikrotax.org/pforams/index.php?id=132532 Go to Archive.is to create a permanent copy of this page - citation notes |
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