Mendips header
 Overview maps
 Locality areas
  Cheddar Gorge
 Burrington Combe
 Shipham & Rowberrow
 Crook Peak & Axbridge
 Banwell to Churchill
 Harptree & Smitham Hill
 Draycott & Westbury-sub
 Wookey Hole & Ebbor
 Great Elm & Vallis Vale
 Mells & the Wadbury Valley
 The Vobster area
 The Whatley area
 Torr Works & Asham Wood
 Beacon Hill
 Stoke St Michael & Oakhill
 Holwell & Nunney
 Shepton Mallet & Maesbury
 Gurney Slade & Emborough
 The Nettlebridge valley
 Rocks of Mendips
 Geological timescale
 Ancient environments
 Geological structure
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  Minerals and mines
 Industrial archaeology
  Stone as a resource
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 Quarrying & the environment
 History of quarrying
 Caves and karst
 How caves form
 Dry valleys and gorges
 Dolines and sinkholes
 Mendip caves
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  Flora and fauna
 Typical Mendip habitats
 Special Mendip habitats
 Horseshoe bats
 Appendix of names
 Biodiversity of western
 Biodiversity of eastern
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  East Mendip quarries
 Biodiversity of eastern
  West Mendip quarries
 Biodiversity of western
 Site map
The fossils of Mendip
Silurian | Upper Devonian | Lower Carboniferous | Triassic | Lower to Middle Jurassic

Lower Carboniferous fossils (359 to 326 million years ago)

Avon Group (Lower Limestone Shale) The lowest part of the Avon Group has a rather restricted fauna that includes the brachiopod Lingula, gastropods, bivalves and fish, suggesting that fully marine conditions were not immediately established across the Mendips in the early Carboniferous. The main fauna of the Avon Group is brachiopod-dominated, and species of Chonetes, Productus, Eumetria, Camarotechia and Unispirifer are common.

Crinoid stem fragments locally occur in rock-building proportions, forming the iron-stained crinoidal limestones that occur in the succession, and bryozoans form the well-known 'Bryozoa Bed' in the lower part of the group.
  Chonetes (Avon Group)
Black Rock Limestone Subgroup
The Black Rock Limestone is the most fossiliferous part of the Carboniferous Limestone in the Mendips. The remains of crinoids, brachiopods and corals are especially abundant, and three broad faunal subdivisions can be recognised. In the lowest subdivision brachiopods are dominant, such as Cleiothyridina, Dictyoclostus, Pugilis, Rhipidomella, Rugosochonetes and Syringothyris. This interval is similar to the fauna of the Avon Group, but can be distinguished by the presence of the coral Zaphrentites delanouei and the brachiopod Rugosochonetes vaughani. The middle part of the Black Rock Limestone is characterised by a rich coral fauna, particularly Caninophyllum, Caninia, Cyathaxonia, Cyathoclisia, Fasciculophyllum and Sychnoelasma. In the upper part of the Black Rock Limestone the coral Siphonophyllia cylindrica is diagnostic and brachiopods, such as Pustula cf. pustuliformis, become an increasingly important part of the fauna.

Syringothyris Productus (Dictyodostus) Vaughani
Burrington Oolite Subgroup and Vallis Limestone Formation
Crinoid remains are an important constituent of much of the lower part of the Burrington Oolite, and especially of the coarse bioclastic limestones that form the laterally equivalent Vallis Vale Limestone Formation. In the Burrington Oolite, the coral Palaeosmilia murchisoni occurs in the lower part of the formation and Siphonodendron ['Lithostrotion'] martini in the upper part. The brachiopod fauna includes Gigantoproductus, Delepinea, and Megachonetes, the latter two mainly occurring in the lower part of the formation; Davidsonina occurs near the top. The coral and brachiopod fauna of the Vallis Vale Limestone in the Mendips is similar to that occurring in the Burrington Oolite, including Palaeosmilia murchisoni and Delepinea.

Siphonodendron martini Palaeosmilia murchisoni
Megachonetes   Clifton Down Limestone Formation
The Clifton Down Limestone has a rich but low diversity fauna. The most notable feature is the abundant, partly silicified remains of the coral Siphonodendron ['Lithostrotion'] martini in the middle part of the formation. This coral-rich interval, named the 'Lithostrotion Beds', forms a conspicuous marker-interval that can be traced across the Mendip region. Axophyllum 'Carcinophyllum' vaughani is another widely occurring coral in this unit, and the brachiopod fauna includes Composita, which are concentrated at horizons throughout the formation. Megachonetes and Linoprotonia also occur, and Davidsonina is common in the lower part of the Clifton Down Limestone.
Oxwich Head Limestone Formation
A rich fauna of crinoids, corals and thick-shelled brachiopods is characteristic of the Oxwich Head Limestone, the top of which also contains goniatites and a diverse gastropod fauna, indicating full open-marine conditions. There is a distinct change in the coral and brachiopod fauna compared to the underlying Clifton Down Limestone; although species of Lithostrotion continue to occur, several species of Dibunophyllum are also present, and the brachiopods include the large Gigantoproductus maximus, as well as spiriferoids, athyroids and chonetoids.

Dibunophyllum Gigantoproductus

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