The Narva Formation was formed during the Middle Devonian transgression maximum as the Devionian sea expanded. The formation is made up of three members being the Vadja, Leivu, and Kernave members. The total depth of the formation is 74.5 (244 ft) meters with the composition of the formation changing heavily between the individual members[1]:
Member
Composition
Vadja
Dolomitic marl, Clayey dolomitic marl, Clay with imbedded siltstone
Leivu
Siltsone, Siltstone with calcitic cement, Clayey dolomitic marl, Clay with gypsum inclusions
A cheiracanthid known from both Batic and Scottish formations, it had a long body with a dorsal fin positioned in-between the pelvic and anal spines.[4]
^ abcdefghijklmnopqrstuvwxMark-Kurik, Elga (2000). "The Middle Devonian fishes of the Baltic States (Estonia, Latvia) and Belarus". CFS Courier Forschungsinstitut Senckenberg. 223.
^Plax, D. P. (2019). "A NEW SPECIES OF THE ACANTHODIAN FISH FROM THE KOSTYUKOVICHI REGIONAL STAGE (MIDDLE DEVONIAN, EIFELIAN) OF BELARUS". Bulletin of BarSU Series "Biological Sciences. Agricultural Sciences.
^ abYoung, Gavin C. (2005). "Early Devonian arthrodire remains (Placodermi, ?Holonematidae) from the Burrinjuck area, New South Wales, Australia". Geodiversitas. 27 (2).
^Denison, Robert Howland (1978). Placodermi. Handbook of paleoichthyology (1. Aufl ed.). Stuttgart ; New York: Fischer. ISBN978-0-89574-027-4.