Monday, 2 February 2026

ALBERTONIA FROM THE CRANBROOK MUSEUM COLLECTION

Albertonia sp., Cranbrook Museum Collection
This beauty, with its graceful sail-like fins and armour of lustrous, diamond-shaped scales, is Albertonia sp., an Early Triassic ganoid fish from the ancient seas of what is now British Columbia and Alberta. 

Belonging to the family Parasemionotidae—among the most advanced and abundant of the Triassic subholosteans—Albertonia is one of the real showstoppers of Canada’s Early Triassic fossil record.

Specimens of this lovely are known from the Vega-Phroso Siltstone Member of the Sulphur Mountain Formation near Wapiti Lake in northeastern British Columbia, as well as from the Lower Triassic Montney Formation of Alberta. These units are part of the Western Canada Sedimentary Basin, a region that preserves some of the finest Early Triassic fish faunas anywhere on Earth.

The Wapiti Lake exposures, in particular, are world-class. Here, a rich assemblage of exquisitely preserved bony fishes—armoured in heavy ganoid and cosmoid scales—has been uncovered. Four genera dominate these ancient marine beds: the ray-finned actinopterygians Albertonia, Bobasatrania, and Boreosomus, alongside the lobe-finned coelacanth Whiteia

Together, they form a window into life during a time of ecological recovery following the end-Permian mass extinction.

Albertonia is easily one of my favourites. Most specimens measure around 35–40 cm in length and display a striking, streamlined silhouette. The most distinctive feature is the tall, sail-shaped dorsal fin, paired with long, elegant pectoral fins that also flare like miniature sails. The ventral fins are comparatively small, giving the fish a unique balance and profile unlike anything in today’s oceans.

These fishes inhabited deeper marine waters, feeding on plankton and other small organisms drifting through the Early Triassic seas. 

The extraordinary preservation of many specimens—right down to the crisp geometry of each square-shaped ganoid scale—suggests rapid burial in calm, anoxic seafloor sediments where scavengers and decay could not disturb them. In some fossils, the sculptural quality of the ganoine coating is still visible, each scale a tiny gleaming tessera in a mosaic more than 245 million years old.

Together, Albertonia and its Triassic companions help tell a story of resilience and renewal. In the wake of Earth’s greatest extinction event, life returned to the oceans with new forms, new strategies, and unexpected beauty. And in the fine-grained rocks of Wapiti Lake and the Montney Formation, that beauty has been preserved in breathtaking detail, scale by scale, fin by fin, across deep time.