Ballagan Formation

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Ballagan Formation
Formation
Unit ofInverclyde Group
UnderliesClyde Sandstone Formation
OverliesKinnesswood Formation
AreaCentral Lowlands, Northern England
Thickness~900 m
Lithology
Primarymudstone, cementstone, siltstone
Othersandstone
Location
RegionScotland
CountryUnited Kingdom
Type section
Named forBallagan Glen
Named byBrowne, 1980

The Ballagan Formation is a

Visean).[1] Its name comes from the "Ballagan Beds" of Ballagan Glen, near Strathblane, which has a good example of this geological formation.[2]

The Ballagan Formation was historically known as the Cementstone Group,

cementstone-rich "drab beds" in the middle of the group were renamed to the Ballagan Formation.[6] In Lothian, the Ballagan and Clyde Sandstone formations are sometimes known as the Tyninghame Formation.[7]

Fossil sites

Many localities of the Ballagan Formation preserve exceptional fossils. The majority of fossiliferous sites are in the

Midland Valley (particularly the Scottish Borders and East Lothian), in the southeast corner of Scotland.[5][8]

One of the earliest sites to be studied was the fish bed at

Willie's Hole, near Chirnside, is another site known for its high quality of preservation. It was initially recognized for its crustacean fossils, forming "shrimp beds" akin to those observed throughout the later Scottish Carboniferous.[19] Willie's Hole has continued to produce well-preserved fossils of arthropods, fish, and partial tetrapod skeletons.[5][20][21][22]

Ballagan Formation outcrop at Spouts Burn, in southwest Scotland near Auchenrock Glen and Dumbarton

By far the largest exposures of the Ballagan Formation occur along the coastal end cliffs of Burnmouth.[5][23][24] Tetrapod, fish, and arthropod fragments are common in several layers at Burnmouth, not just in fine-grained overbank deposits[20][22][25][26] but also coarse river channel conglomerates, an unusual mode of preservation.[27][28]

Tetrapod fossils have been found in the vicinity of Tantallon Castle.[5][29] Additional Midland Valley sites include Crumble Edge (along Whiteadder Water),[30] Coldstream,[5][31] Cockburnspath,[32][5] Cove (in Berwickshire),[31] and Whitrope Burn (near Hawick).[33] A few locales in nearby Northumberland, England encompass fossil-bearing outcrops of the Ballagan Formation, such as Berwick-upon-Tweed[34][35] Barrow Scar (near Alwinton),[31] and a borehole core at Norham.[23][24]

Some sites are also found along the west coast of Scotland. Auchenreoch Glen, near Dumbarton, was the collection site for the nearly complete type fossil of Pederpes finneyae, which was the oldest named tetrapod of the Carboniferous upon its discovery.[36] Diverse assemblages of fish teeth and other microfossils have been found at Ayrshire[37][31] and at Hawk's Nib and Mill Hole, on the Isle of Bute.[38]

Paleobiota

The Ballagan Formation preserves a plethora of tetrapod, fish, and invertebrate fossils, reconstructing one of the most diverse continental ecosystems known from the Tournaisian stage. A variety of plant megafossils and spores are known from the Ballagan Formation.[11][39][37][40][41]

Tetrapods

Fish

Invertebrates

See also

References

  1. ^ British Geological Survey. "Ballagan Formation". BGS Lexicon of Named Rock Units. Retrieved 8 March 2018.
  2. ^ MacDonald, Hugh (1910). Rambles Round Glasgow (New ed.). Glasgow: John Smith. p. 382.
  3. S2CID 140699667
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  6. ^ a b c d Brown, M.A.E. (1980). "The Upper Devonian and Lower Carboniferous (Dinantian) of the Firth of Tay, Scotland". Report of the Institute of Geological Sciences. 80 (9): 1–13.
  7. S2CID 129170097
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