Northwestern Europe, Scotland, Orkney, Old Red Sandstone Formation, Middle Devonian, ca. 380 million years ago. This large stone displays two incredible fish fossils from rhipidistians, freshwater fish that eventually evolved into the earliest terrestrial tetrapods! These preserved remains are excellent and of fine quality. The largest is a primitive lungfish known as Gyroptychius agassizi - with a lengthy, streamlined body, and the other fish is a lobed-finned relative known as Osteolepis- both covered with armored plates in the head and heavy scales. This is a choice grade example of a Gyroptychius fossil due to its stunning state of completeness and size! The scale articulation is exceptional as well as is the full array of fins and tail, even the delicate caudal fin and thoracic fins are natural and well-preserved! Size (Gyroptychius fossil): 13.25" L (33.7 cm); (Osteolepis fossil): 5" L (12.7 cm); (matrix): 19" L x 13.25" W (48.3 cm x 33.7 cm)
At a period in time when vertebrates were scarce on Earth and trilobites thrived in enormous varieties and numbers, these fish of the Devonian, graced a freshwater lake in the region that is now Northern Scotland. The Devonian Period is the first era on Earth of fish emerging in the fossil record. Gyroptychius agassizi was a predatory lungfish, a lobe-finned bony fish that had the capability to breathe air by the use of their modified air bladder consisting of multiple chambers. They possessed odd large ridged toothplates designed to crush as much as chew their prey. Gyroptychius had a long, slender body with a shallow head and small eyes and arranged in diagonal rows were thick rhombic scales made up of a cosmine layer and a thin shiny ganoine layer. These primitive fish also possessed a bizarre rhomboid-shaped caudal fin.
The Old Red Sandstone layers of Northern Scotland are one of three of the world's most scientifically important and richest deposits yielding fossil fish from the Devonian. The other two sites are at Canowindra in New South Wales and Miguasha in Quebec. A wide variety of freshwater fish can be found in these layers in Scotland from a time when the very first four-limbed vertebrates were evolving. The Achanarras beds, named after the quarry where they were first discovered, can be found in the layers that were laid down in Lake Orcadie during the Devonian period, 380 million years ago. Achanarras Quarry is situated at the top of a hill and is not very large. Since the quarry is now closed, the main central portion is flooded and inaccessible. Many years ago, it was worked for the laminated limestone which was split for roofing slates. The site is littered with a vast amount of slabs, but whole fish are rare and easily broken when found.
Provenance: ex-private German collection before 2011
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#172847
Condition
Choice and intact, no repairs or restoration. Protective sealer applied to fossils.