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pf_mesozoic


Classification: pf_mesozoic
Sister taxa:
Daughter taxa (time control age-window is: 0-800Ma)Granddaughter taxa
triserial
Guembelitriidae
Early stage trochospiral, triserial, or biserial, later may show serial reduction or proliferation.
Guembelitria

biserial-multiserial
Heterohelicidae
Aperture symmetrical, ranging from a low slit to a high arch at the base of the final chamber, becoming terminal in uniserial taxa.

planispiral
Planomalinidae
Test planispiral, biumbilicate, periphery carinate, sutures strongly arched; aperture a low equatorial opening.
Planomalina
Pseudoplanomalina

Globigerinelloididae
Test planispiral, chambers globular to radially elongate; aperture at the base of the chamber face and equatorial in position, lateral portions of primary aperture may remain open as new chambers are added, forming relict openings around the umbilical region.
Eohastigerinella
Globigerinelloides
Hastigerinoides
Laeviella
Planohedbergella
Polycamerella
Pseudoschackoina

Schackoinidae
Test trochospiral to nearly planispiral, chambers with one or more hollow tubulospines; aperture equatorial and may have broad lip.
Leupoldina
Schackoina

trochospiral (in sequence of increasing complexity)
Conoglobigerinidae
Small (<200µm), microperforate wall, 3-4 globose chambers in final wall, aperture umbilical
Conoglobigerina
Globuligerina
Petaloglobigerina

Chilostomellidae

Gubkinella

Favusellidae
Test trochospirally coiled, chambers inflated, rounded to ovate; wall cancellate, with abundantly perforated fields bordered by imperforate ridges; primary aperture umbilical to slightly extraumbilical, with an imperforate lip; umbilicus narrow to wide and deep, margin noncarinate.
Favusella

Praehedbergellidae
Globigerinacea with trochspiral tests, in which the primary aperture is intraumblical or intraumbilical-extraumbilical and which possess a microperforate wall lacking muricae, crystallite pustules, or spine bases; differs from the Favusellacea in its lack of muricae (and in possessing a calcitic test) and from the Schackoinidae in not becoming planispiral.
Blefuscuiana
Gorbachikella

Hedbergellidae
Test trochospirally coiled, primary aperture interiomarginal, extraumbilical-umbilical, with prominent apertural lip, apertures of earlier chambers remain visible around the umbilical region; no sutural secondary apertures.

Rugoglobigerinidae
Test trochospiral, chambers inflated, periphery rounded, not carinate; wall with pustules, costellae, or other rugosities; aperture umbilical, with portici or tegilla.
Archaeoglobigerina
Bucherina
Kuglerina
Plummerita
Rugoglobigerina
Rugotruncana
Trinitella

Rotaliporidae
Test trochospirally enrolled, primary aperture umbilical-extraumbilical in position and with bordering lip, secondary sutural apertures on umbilical side open into posterior edge of chambers.
Anaticinella
Biticinella
Pseudothalmanninella
Rotalipora
Thalmanninella
Ticinella

Globotruncanidae
Test trochospiral, chambers angular, periphery truncate or carinate; primary aperture umbilical, covered by a spiral system of tegilla that is provided with accessory intralaminal and infralaminal apertures.
Abathomphalus
Contusotruncana
Dicarinella
Gansserina
Globotruncana
Globotruncanella
Globotruncanita
Loeblichella
Marginotruncana
Radotruncana

Taxonomy

Citation: Mesozoic Planktonic Foraminifera
Taxonomic discussion: The Mesozoic planktonic foraminifera are conventionally included in the Order Globigerinida. However, it is possible that the K/Pg extinction eliminated all planktonic foramnifera which then re-evolved from benthic ancestors. In this case the Cretaceous forms should be placed in a separate order as argued by Arenillas et al. 2022, who proposed the order Globotruncanida.

Original description: Diagnosis. Test trochospiral or planispiral. Peripheral margin without keel, or with one or two keel. Aperture bordered by a lip or protected by a porticus or a tegillum, rarely by a bulla. Finely perforate to macroperforate. Wall surface smooth, pore-mounded, pitted, reticulate, hispid, pustulate, muricate, rugose, or costate. Wall hyaline calcitic, but early forms may be aragonitic.

Entries in the Catalog of original descriptions: Globotruncanida

Geological Range:
Notes: upper Maastrichtian
Last occurrence (top): at top of (100% up, 0Ma, in "Holocene" stage). Data source: Total of ranges of the species in this database
First occurrence (base): within (-Ma, base in "Holocene" stage). Data source: Total of ranges of species in this database

Plot of range and occurrence data:

References:

Arenillas, I., Arz, J. A. & Gilabert, V. (2022). An updated suprageneric classification of planktic foraminifera after growing evidence of multiple benthic-planktic transitions. Spanish Journal of Palaeontology. 37(1): 1-34. gs O


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pf_mesozoic compiled by the pforams@mikrotax project team viewed: 13-10-2024

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Short stable page link: https://mikrotax.org/pforams/index.php?id=110389 Go to Archive.is to create a permanent copy of this page - citation notes



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Comments (2)

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Chengjie Liu(US)

It seems something is wrong with the Mesozoic part of the planktonic foram data, when I click a link to a Mesozoic taxon, the following message will occur. Any additional click will repeat the same message once more. Thanks for checking on this.

SOMETHING WENT WRONG WITH THE DATABASE ENTRY, (IS TAXON PATH SET?):

Error: SQLSTATE[42S02]: Base table or view not found: 1146 Table 'nannotax_mikrotax.YES' doesn't existarrayname: sessionpr Array

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Jeremy Young(UK)

Thank you for pointing that out - yes there was a database glitch here, it has been fixed now.

Jeremy