A Beautiful example of Birkenia elegans from the Birkenhead Burn locality
Many
important collections of Silurian arthropods and vertebrates have been
made near Lesmahagow since the mid to late 1800’s. The Geological Society
of Glasgow set up a camp in the 1890’s, which was aptly named “Camp
Siluria”, from which members of the society collected a number of
rare and complete specimens of fossil fish and eurypterids. It is now
very difficult to obtain permission to collect from these rocks as a
result of inappropriate collecting. It is still possible to find fossils
from these rocks, but all fossils are rare and some may be usefully donated
to a museum for research.
The
Lesmahagow Inlier is a block of Silurian sediments surrounded by sediments
of Carboniferous age. The inlier consists of shales and sandstones with
occasional pebble conglomerates of a lagoon or lake. The lower parts
of the succession contain occasional marine fossils, including trilobites
and brachiopods, but the higher parts of the succession lack any evidence
of marine incursions becoming influenced more by river and deltaic conditions.
The sequence seen here is part of a general regression that can be traced
from western Ireland to Scandinavia. The earlier (Cambro-Ordovician)
terrane accretion of the Midland Valley Terrane to the Laurentian continent
by sinistral strike-slip controlled basin development, sedimentary facies
and deformation from Llandovery through until the early Devonian times.
Birk
Knowes SSSI (Site of Special Scientific Interest and has special protection
under Scots law) is also known as the Jamoytius Horizon named after
the rare soft-bodied fish found from this locality. Sadly, due to overzealous
collecting, this site has been made off-limits to all collecting for
the time being. From the debris, we might be able to find a number of
the rare fossil animals found at this locality such as Loganellia
scotica (thelodont fish), Jamoytius kerwoodi (agnathan fish),
Ainiktozoon loganense (?concavicarid arthropod), Ceratiocaris
papilio (pod-shrimp), Pterygotus bilobus and Slimonia
acuminata (eurypterids) as well as a number of other rare animals
(see the images below). The silts and shales represented here are all from
the Patrick Burn Formation and probably represent a shallow brackish-water
lagoon with occasional marine incursions and high sediment input. The
sediments are thought to be of Llandovery (Silurian) age. The sediments continue
up sequence into blue slatey shales that contain eurypterids and pod-shrimps,
but rarely any fish remains. These rocks can be found in the Kip Burn, Logan
Water, Blaeberry Burn and at Dunside.
Pterygotus claw |
Scorpion-like eurypterid |
Ceratiocaris from Dunside |
Ceratiocaris from Dunside |
|
Email comments to Dr Neil
Clark
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