Pulsocauda igen. nov., a New Ichnotaxon from the Frasnian (Upper Devonian) of the East European Platform

New ichnogenus and ichnospecies Pulsocauda ankylon igen. et isp. nov. are established for single grooved crescent-shaped locomotion trails from the Frasnian (Upper Devonian) of European Russia. Earlier described trail from the Frasnian of the Onega Lake coast is assigned to this ichnospecies, and the one from the North Timan to the same ichnogenus. The similarity of these ichnofossils suggests that these trails could have been left by fishes with similar caudal fin morphology when touching the bottom. Through the use of three-dimensional models, a series of cross-sections were reconstructed, revealing modifications in their configuration that indicate a shift in the orientation of the terminal part of the caudal lobe during swimming. It is most likely that the tracks of Pulsocauda ankylon gen. et sp. nov. were produced by arthrodire placoderm fishes, which had the tail structure particularly suited to forming such distinctive trails.

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Publication Details

Journal
Paleontological Journal
Published
2025-12-01
DOI
https://doi.org/10.1134/s0031030125600465
Primary Topic
Geological formations and processes
Type
article
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article

Pulsocauda igen. nov., a New Ichnotaxon from the Frasnian (Upper Devonian) of the East European Platform

E. Yu. Baraboshkin, P. A. Beznosov, O. A. Lebedev, I. P. Bolshiyanov
Paleontological Journal
Geological formations and processes
article

Pulsocauda igen. nov., a New Ichnotaxon from the Frasnian (Upper Devonian) of the East European Platform

E. Yu. Baraboshkin, P. A. Beznosov, O. A. Lebedev, I. P. Bolshiyanov
article en

Abstract

New ichnogenus and ichnospecies Pulsocauda ankylon igen. et isp. nov. are established for single grooved crescent-shaped locomotion trails from the Frasnian (Upper Devonian) of European Russia. Earlier described trail from the Frasnian of the Onega Lake coast is assigned to this ichnospecies, and the one from the North Timan to the same ichnogenus. The similarity of these ichnofossils suggests that these trails could have been left by fishes with similar caudal fin morphology when touching the bottom. Through the use of three-dimensional models, a series of cross-sections were reconstructed, revealing modifications in their configuration that indicate a shift in the orientation of the terminal part of the caudal lobe during swimming. It is most likely that the tracks of Pulsocauda ankylon gen. et sp. nov. were produced by arthrodire placoderm fishes, which had the tail structure particularly suited to forming such distinctive trails.

Paleontological JournalVol. 59(8)
Lomonosov Moscow State University (RU), Institute of Paleontology A A Borisyak (RU), Institute of Geology, Komi Science Centre (RU)
Life below water
Openalex Percentile: Top 27%
Geological formations and processes
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