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Scaat Craig
Scaat Craig, a section of the Longmore Burn near Elgin, has been a site for
fossil collecting since the 1820's. Although there are many sites in the Moray
Firth area where fossil fish have been found, Scaat Craig was one of the first
to be discovered. It was extensively worked during the 1830's and 1840's and
was featured in the works of several famous historical geologists such as Hugh
Miller and Louis Agassiz (1807 - 1873). The site however is now very overgrown.
The fossils are found in rocks that are Upper Old
Red Sandstone in age (late Devonian).
At this time, the Moray Firth area lay in a basin that was bounded to the
south by a mountain range. The rocks at Scaat Craig are generally sandstones
and conglomerates, formed when powerful rivers and flash floods carried large
amounts of sediment from the mountians into the surrounding basins and valleys.
At Scaat Craig, it is the sandstones that have yielded the fossils.
The rocks are friable, which unfortunately means that fossilised material
is also easily fragmented. This has hampered the interpretation of the evolution
of the fish at the site as the fish were usually found as fragments. However,
the site has yielded abundant remains that include: Bothriolepis paradoxa (type
locality), B. major, Cosmacanthus malcolmsoni (type locality), Conchodus
ostrieformis (type locality), Traquairosteus pustulatus, Psammosteus
cf. falcatus, Rhizodonts, Holoptychius nobilissimus and H. giganteus.
Incomplete amphibian remains have also been found which represent some of
the earliest known tetrapod specimens. These remains were collected in the
early days, but their significance was not realised until recent work on the
collections.
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