Non-pollen palynomorphs from the Devonian (Givetian/Frasnian) of south-central Poland

The first report of the Devonian non-pollen palynomorphs (NPP) from the Givetian/Frasnian of ­Poland reveals diverse assemblages that contain chitinozoans, scolecodonts, organic tentaculitoids, animal remains, phytoplankton, plant debris, nematophytes and fungi. Analysed material provided the first documentation of chitinozoans from this time interval in Poland and the world oldest occurrence of organic tentaculitoids. These palynomorphs hold significant palaeoenvironmental value. The differentiated palynomorph assemblage indicates a deposition in a shallow water-marine environment with high terrestrial input. The age of the analysed deposits was established as “Geminospora” extensa (Ex) Miospore Zone to Geminospora aurita (Aur) Miospore Zone (conodont zones hemiansatus to lower falsiovalis).

Authors

Publication Details

Journal
Comptes Rendus Palevol
Published
2025-09-16
DOI
https://doi.org/10.5852/cr-palevol2025v24a22
Primary Topic
Paleontology and Stratigraphy of Fossils
Type
article
Field-Weighted Citation Impact
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article

Non-pollen palynomorphs from the Devonian (Givetian/Frasnian) of south-central Poland

Marcelina Kondas, Paweł Filipiak, Sonia C. Camina, Petra Tonarová
Comptes Rendus Palevol
Paleontology and Stratigraphy of Fossils
article

Non-pollen palynomorphs from the Devonian (Givetian/Frasnian) of south-central Poland

Marcelina Kondas, Paweł Filipiak, Sonia C. Camina, Petra Tonarová
article en

Abstract

The first report of the Devonian non-pollen palynomorphs (NPP) from the Givetian/Frasnian of ­Poland reveals diverse assemblages that contain chitinozoans, scolecodonts, organic tentaculitoids, animal remains, phytoplankton, plant debris, nematophytes and fungi. Analysed material provided the first documentation of chitinozoans from this time interval in Poland and the world oldest occurrence of organic tentaculitoids. These palynomorphs hold significant palaeoenvironmental value. The differentiated palynomorph assemblage indicates a deposition in a shallow water-marine environment with high terrestrial input. The age of the analysed deposits was established as “Geminospora” extensa (Ex) Miospore Zone to Geminospora aurita (Aur) Miospore Zone (conodont zones hemiansatus to lower falsiovalis).

Comptes Rendus PalevolVol. 24(22)
Openalex Percentile: Top 89%
Paleontology and Stratigraphy of Fossils
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