Species: undulata PANDER, 1856
Etymology:
Neotype: No. 257/592
Locality: Ohesaare Cliff, Saaremaa Island, Estonia.
Horizon:
Biostratigraphy:
Age: Ohesaare Stage, Pridoli Epoch, Late Silurian.
Material:
Referred material:
MARSS, 2018
TUG 681-, 1384-1: Ventral and dorsal shield fragment.
Locality: Depths of 176.1 and 176.2 m, Ruhnu drill core, Ohesaare Cliff, Estonia.
Horizon:
Biostratigraphy:
Age: OhesaareStage, Late Silurian.
Material:
Number: Not given: Large dorsal and ventral shield fragments.
Locality: Depth of 401.8 mButkunai Drill core, Lithuania.
Horizon:
Biostratigraphy:
Age: Late Silurian.
Material:
Number: Not given: Anterior poart of the ventral shield.
Locality: Depth of 162.2 m, Kolka-54 drill core, Latvia.
Horizon:
Biostratigraphy:
Age: Late Silurian.
Material:
GIT 721-3: Dorsal shield.
Locality: Depth of 79.8 m, Velikaya River-81 drill core, North Timan.
Horizon:
Biostratigraphy: Thelodont Trimerolepis timanica vertebrae zone.
Age: Greben' Stage, Uppermost Pridoli Epoch, Late Silurian.
Material: Dorsal? shield fragment.
= Oniscolepis magnus PANDER, 1856
Etymology:Holotype:
Locality:
Horizon:
Biostratigraphy:
Age:
Material:
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Species: timanica KOSSOVOI & OBRUCHEV, 1962
Etymology:
Holotype:
Locality: Velikaya River, Timan.
Horizon: Eptarmenskaya Beds.
Biostratigraphy:
Age:
Material:
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Species: lenzi DINELEY & LOEFLER, 1976
Etymology:
Holotype: NMC 13768
Locality: CS (Chevron Standard Localities) YB10, 63°40’N, 129°23’W, 40 km north-west of June Lake, Northwest Territories Province, Canada.
Horizon: 9F is at 340 m in section, Formation unknown.
Biostratigraphy:
Age: Late Silurian.
Material: An almost complete dorsal shield.
Note: Shallow water, marine.
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Species: bedovensis MARSS, 2019
Etymology: In refernece to the River Bedovaya, where the specimen was found.
Holotype: GIT 721-7
Locality: The Bedovaya River secton, October Revolution Island, Severnaya Zemlya Archipelago.
Horizon: Lower part of the Krasnaya Bukhta Formation.
Biostratigraphy:
Age: Late Silurian.
Material: Ventral shield, broken postrolaterally and posterorly.