NB This site is under active development, current content in the main database is primarily from Bolli et al 1994, Hayward et al. 2012, Holbourn et al. 2013, Holbourn and Kaminski 1997, Alegret & Thomas 2001, and Katz et al. 2003. It is intended to expand and develop this to provide rather comprehensive coverage of Mesozoic and Cenozoic deep-sea benthic foraminifera.
Daughter taxa (time control age-window is: 0-800Ma)![]() | ||||
| Pseudonodosinella elongata | ||||
| Pseudonodosinella nodulosa | ||||
| Pseudonodosinella troyeri | ||||
| Pseudonodosinella sp. Specimens which cannot be assigned to established species | ||||
Catalog entries: Pseudonodosinella
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.
Wall composition:
| TEST: elongate-cylindrical, lobate outline, uniserial, APERTURE: circular, terminal, |
| Final whorl chambers: 1->1 |
Geological Range:
Last occurrence (top): Extant. Data source: Total of range of species in this database
First occurrence (base): within Barremian Stage (121.40-126.50Ma, base in Barremian stage). Data source: Total of range of species in this database
Plot of occurrence data:
NB The ranges given for genera and higher taxa are the total ranges of species included in that taxon in this database - so the true total range of the taxon will usually be longer
Saidova, K. M. (1970). Бентосные Фораминиферы раыона курило-Камчатского желоба - Benthic foraminifera of the Kurile-Kamchatka Trench based on the data of the 39th cruise of the R/V Vityaz. Труды Институт океанологии-Trudy Institut Oceanology. 86: 134-161. gsReferences:

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Pseudonodosinella compiled by the bforams@mikrotax project team viewed: 17-6-2026
Short stable page link: https://mikrotax.org/bforams/index.php?id=2000137 Go to Archive.is to create a permanent copy of this page - citation notes |
bforams@mikrotax has been supported by US IODP Science Support Program and by the Geologic TimeScale Foundation
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