Fossil remains of ciliates (phylum Ciliophora): A recommendation for their treatment under the International Code of Nomenclature for algae, fungi and plants

Ciliates (phylum Ciliophora) are a diverse group of ciliated protists common in marine, freshwater, and terrestrial environments. Ciliates are traditionally treated under the International Code of Zoological Nomenclature (ICZN) as “animals” although many are non-constitutive phototrophs. As alveolates, ciliates are closely related to the dinoflagellates, which are treated today under the International Code of Nomenclature for algae, fungi and plants (ICN). The fossil remains of ciliates, primarily the resting cysts and loricae, are frequently encountered in palynological preparations of modern and older marine and nonmarine deposits. They have strong potential for use in paleoenvironmental reconstructions but most cannot be linked unequivocally to their corresponding non-fossil motile stage. A separate taxonomy is required for fossil ciliate remains and a corresponding formal nomenclature to track their occurrences. The ICZN explicitly prohibits separate names for different stages in the life cycle of a single organism. We therefore recommend placing these fossils under the governance of the ICN, which allows the names of fossil-typified species to coexist with those of their non-fossil-typified equivalent stages (dual nomenclature). We return the ciliate fossil-genus Halodinium Bujak, 1984 to the ICN and recommend the establishment of equivalent fossil-genera for the important non-fossil genera Hexasterias Cleve, 1900 and Radiosperma Meunier, 1910, which are now known to be ciliate cysts. The acritarch genus Cyclopsiella Drugg and Loeblich, 1967 most likely represents ciliate resting cysts and extends to the Jurassic. Placing fossil ciliates under the ICN is a practical solution given that nomenclature serves taxonomy, not the other way around. • Fossil remains of ciliates especially their resting cysts. • The plant–animal divide in phylogenetic classification. • A dual nomenclature approach to fossil ciliates.

Authors

Institutions

Publication Details

Journal
Marine Micropaleontology
Published
2026-02-22
DOI
https://doi.org/10.1016/j.marmicro.2026.102557
Primary Topic
Protist diversity and phylogeny
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Fossil remains of ciliates (phylum Ciliophora): A recommendation for their treatment under the International Code of Nomenclature for algae, fungi and plants

Vera Pospelova, Kenneth Neil Mertens, Vincy Winifred, Audrey Limoges et al.
Marine Micropaleontology
Protist diversity and phylogeny
article

Fossil remains of ciliates (phylum Ciliophora): A recommendation for their treatment under the International Code of Nomenclature for algae, fungi and plants

Vera Pospelova, Kenneth Neil Mertens, Vincy Winifred, Audrey Limoges, Anne de Vernal, Pieter Gurdebeke, Martin J. Head, Nicolas Van Nieuwenhove, Pjotr Meyvisch, Iria García‐Moreiras, Taoufik Radi, Ophélie David, Aurélie Penaud, Vincent Iratçabal
article en

Abstract

Ciliates (phylum Ciliophora) are a diverse group of ciliated protists common in marine, freshwater, and terrestrial environments. Ciliates are traditionally treated under the International Code of Zoological Nomenclature (ICZN) as “animals” although many are non-constitutive phototrophs. As alveolates, ciliates are closely related to the dinoflagellates, which are treated today under the International Code of Nomenclature for algae, fungi and plants (ICN). The fossil remains of ciliates, primarily the resting cysts and loricae, are frequently encountered in palynological preparations of modern and older marine and nonmarine deposits. They have strong potential for use in paleoenvironmental reconstructions but most cannot be linked unequivocally to their corresponding non-fossil motile stage. A separate taxonomy is required for fossil ciliate remains and a corresponding formal nomenclature to track their occurrences. The ICZN explicitly prohibits separate names for different stages in the life cycle of a single organism. We therefore recommend placing these fossils under the governance of the ICN, which allows the names of fossil-typified species to coexist with those of their non-fossil-typified equivalent stages (dual nomenclature). We return the ciliate fossil-genus Halodinium Bujak, 1984 to the ICN and recommend the establishment of equivalent fossil-genera for the important non-fossil genera Hexasterias Cleve, 1900 and Radiosperma Meunier, 1910, which are now known to be ciliate cysts. The acritarch genus Cyclopsiella Drugg and Loeblich, 1967 most likely represents ciliate resting cysts and extends to the Jurassic. Placing fossil ciliates under the ICN is a practical solution given that nomenclature serves taxonomy, not the other way around. • Fossil remains of ciliates especially their resting cysts. • The plant–animal divide in phylogenetic classification. • A dual nomenclature approach to fossil ciliates.

Marine MicropaleontologyVol. 204
University of New Brunswick (CA), HOGENT University of Applied Sciences and Arts (BE), Centre National de la Recherche Scientifique (FR), University of Minnesota (US), Planetary Science Institute (US), Johns Hopkins University (US), University of Liverpool (GB), Ifremer (FR), Université du Québec à Montréal (CA), Université de Bretagne Occidentale (FR), Brock University (CA), Ghent University Hospital (BE), Université de Bretagne Sud (FR), Ghent University (BE), University of Baltimore (US), Universidade de Vigo (ES)
Life below water
Openalex Percentile: Top 46%
Protist diversity and phylogeny
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.