Eyam_Limestone

Eyam Limestone

Eyam Limestone

Geologic formation in England


The Eyam Limestone (formerly known as the Cawdor Group, Cawdor Limestone or Eyam Group) is a geologic formation in the Peak District, England. It preserves fossils dating back to the Viséan stage of the Carboniferous period, and represents a marine environment.[2]

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Depositional environment

At the time of deposition, Britain was just south of the equator (<5° S) and part of the Euramerica continent. Study of the growth rings of fossil wood from other localities indicate that the British Isles had a monsoonal climate during the early Carboniferous, with tropical rainfall seasonality.[3] The Eyam Limestone was deposited on an extensive, thick carbonate ramp and platform on the northeast margin of the Widmerpool Gulf (an extensive basin which existed as an area of open water during the time of deposition). Reefs and their associated fore-reef and lagoonal environments are represented in the Eyam Limestone, with crinoids dominating the reef and providing habitats for other animals. The presence of photosymbiotic coral and micritic envelopes on some crinoid ossicles indicates the formation was deposited within the photic zone in a marine environment of normal salinity. The presence of the xenacanth Bransonella has been suggested to imply freshwater influence as xenacanths live mainly in freshwater habitats, however its presence in other marine formations suggests that Bransonella was a marine animal unlike its relatives.[1]

Apatite crystals formed by the recrystallization of phosphatic overgrowths are present on some conodont elements from the formation. As phosphatogenesis only occurs in the anoxic-oxic boundary while apatite precipitation occurs in the top few centimeters of the sediment column, this reveals that shallow sediment with low geothermal temperatures and dysoxic conditions were present in the Eyam Limestone.[1][4]

Fossil content

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Cartilaginous fish

More information Cartilaginous fish reported from the Eyam Limestone, Genus ...

Conodonts

More information Conodonts reported from the Eyam Limestone, Genus ...

Invertebrates

Arthropods

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Brachiopods

More information Brachiopods reported from the Eyam Limestone, Genus ...

Bryozoans

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Cnidarians

More information Cnidarians reported from the Eyam Limestone, Genus ...

Echinoderms

More information Echinoderms reported from the Eyam Limestone, Genus ...

Molluscs

More information Molluscs reported from the Eyam Limestone, Genus ...

See also


References

  1. Smith, Roy; Martill, David M.; Duffin, Christopher (1 June 2017). "The shark-beds of the Eyam Limestone Formation (Lower Carboniferous, Viséan) of Steeplehouse Quarry, Wirksworth, Derbyshire, UK". Proceedings of the Geologists' Association. 128 (3): 374–400. doi:10.1016/j.pgeola.2017.04.004. ISSN 0016-7878.
  2. "BGS Lexicon of Named Rock Units - Result Details". webapps.bgs.ac.uk. Retrieved 1 September 2023.
  3. Ginter, Michał; Duffin, Christopher; Dean, Mark; Korn, Dieter (2014). "Late Viséan pelagic chondrichthyans from northern Europe". Acta Palaeontologica Polonica. doi:10.4202/app.00084.2014.
  4. Duffin, Christopher J.; Ward, David J. (19 July 2017). "A new janassid petalodont chondrichthyan from the Early Carboniferous of Derbyshire, UK". Proceedings of the Geologists' Association. 128 (5–6): 809–814. doi:10.1016/j.pgeola.2017.06.008.
  5. Duffin, C. (1985). "Revision of the hybodont selachian genus Lissodus BROUGH (1935)". Palaeontographica Abteilung A-palaozoologie-stratigraphie. S2CID 233061921.
  6. Tilsley, J. W. (December 1988). "New data on Carboniferous (Dinantian) trilobites from the Peak District, Derbyshire, England". Proceedings of the Yorkshire Geological Society. 47 (2): 163–176. doi:10.1144/pygs.47.2.163. ISSN 0044-0604.

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