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AVONIAN , in See also:geology, the name proposed by Dr A . See also:Vaughan in 1905 (Q.J.G.S. vol. lxi. p . 264) for the rocks of See also:Lower Carboniferous See also:age in the See also:Avon See also:gorge at See also:Bristol . The Avonian See also:stage appears to embrace precisely the same rocks and fossil-zones as the earlier designation " Dinantien " (see CARBONIFEROUS See also:SYSTEM) ; but its substages, being founded upon different See also:local conditions and a different See also:interpretation of the zonal fossils, do not correspond exactly with those of the See also:French and Belgian geologists . Substages . ZONES . Substages . Kidwellian .Dibunophyllum- Seminula Syringothyris Clevedonian Zaphrentis Tournaisien ,Cleistopora The upper Avonian (Kidwellian) is well See also:developed about See also:Kidwelly in See also:Carmarthenshire . The lower substage (Clevedonian) is well displayed near See also:Clevedon in See also:Somerset . See A . Vaughan, " The Carboniferous See also:Limestone See also:Series (Avonian) of the Avon Gorge," Proc . Bristol Naturalists' See also:Soc., 4th series, vol. i. pt . 2, 1906, pp . 74-168 (many plates) ; and T . F . Sibley, " On the Carboniferous Limestone (Avonian) of the Mendip See also:area (Somerset)," Q.J.G.S. vol . ]Iii., 1906, pp . 324-380 (plates) . (J . A . |
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