A new subfamily classification of the Coskinolinidae Moullade, 1965, Middle Jurassic-Paleogene Larger Benthic Foraminifera

The Coskinolinidae are a family of Middle Jurassic to Paleogene, typically orbitoliniform, Larger Benthic Foraminifera (LBF) characterized by a pseudokeriothecal wall structure. The type genus, Coskinolina Stache, 1875, lacks an exoskeleton (i.e., beams, rafters), resulting in an undivided marginal chamber zone. However, other taxa within the family, such as the Upper Cretaceous Lepinoconus Cruz-Abad et al., 2017, or the Paleogene Coleiconus Hottinger & Drobne, 1980, are genera with vertical partitions (beams) that subdivide the marginal chamber zone. In the currently accepted classification of agglutinated benthic foraminifera, the nature of the exoskeleton is a criterion for distinction at subfamily level, e.g., Cyclamminidae Marie, 1941. Thus, here, the presence or absence of an exoskeleton in the marginal chamber lumen is treated as a criterion at the subfamily level within the classification of the Coskinolinidae, leading to a division into two subfamilies: the Coskinolininae Moullade, 1965 (lacking an exoskeleton), and the newly proposed Coleiconinae subfam. nov. (with an exoskeleton of vertical partitions), as exemplified by Coleiconus Hottinger & Drobne, 1980.

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Publication Details

Journal
Carnets de géologie (Notebooks on geology)
Published
2024-11-27
DOI
https://doi.org/10.2110/carnets.2024.2412
Primary Topic
Paleontology and Stratigraphy of Fossils
Type
article
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article

A new subfamily classification of the Coskinolinidae Moullade, 1965, Middle Jurassic-Paleogene Larger Benthic Foraminifera

Félix Schlagintweit
Carnets de géologie (Notebooks on geology)
Paleontology and Stratigraphy of Fossils
article

A new subfamily classification of the Coskinolinidae Moullade, 1965, Middle Jurassic-Paleogene Larger Benthic Foraminifera

Félix Schlagintweit
article en

Abstract

The Coskinolinidae are a family of Middle Jurassic to Paleogene, typically orbitoliniform, Larger Benthic Foraminifera (LBF) characterized by a pseudokeriothecal wall structure. The type genus, Coskinolina Stache, 1875, lacks an exoskeleton (i.e., beams, rafters), resulting in an undivided marginal chamber zone. However, other taxa within the family, such as the Upper Cretaceous Lepinoconus Cruz-Abad et al., 2017, or the Paleogene Coleiconus Hottinger & Drobne, 1980, are genera with vertical partitions (beams) that subdivide the marginal chamber zone. In the currently accepted classification of agglutinated benthic foraminifera, the nature of the exoskeleton is a criterion for distinction at subfamily level, e.g., Cyclamminidae Marie, 1941. Thus, here, the presence or absence of an exoskeleton in the marginal chamber lumen is treated as a criterion at the subfamily level within the classification of the Coskinolinidae, leading to a division into two subfamilies: the Coskinolininae Moullade, 1965 (lacking an exoskeleton), and the newly proposed Coleiconinae subfam. nov. (with an exoskeleton of vertical partitions), as exemplified by Coleiconus Hottinger & Drobne, 1980.

Carnets de géologie (Notebooks on geology)Vol. 24(12)
Slovenska Akademija Znanosti in Umetnosti
Life below water
Openalex Percentile: Top 93%
Paleontology and Stratigraphy of Fossils
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A new subfamily classification of the Coskinolinidae Moullade, 1965, Middle Jurassic-Paleogene Larger Benthic Foraminifera — Félix Schlagintweit · Carnets de géologie (Notebooks on geology) (2024) | TGRS Research Map | TGRS