The Carboniferous goniatites of the neighbourhood of Tenby

Bisat, W. S.

doi:10.1016/s0016-7878(33)80042-3

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Cited by 7 publications

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“…They were first systematically described as part of the classic work of Dixon (1921) on the Carboniferous rocks in Pembrokeshire. Although important additions to the zonal interpretation of the succession were made by Dixon (1933 a and b) and Bisat (1933), no further detailed account has appeared since. The Namurian succession in South Wales has been described in detail for the North Crop by Ware (1939), Jones andOwen (1957 and1967) and Archer (1965), and for the South Crop by Dix (1931) and Woodland and Evans (1964).…”

Section: Introductionmentioning

confidence: 99%

The namurian succession between Tenby and Waterwynch, Pembrokeshire

Jones

Eagar²

1969

Geological Journal

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With a report on some bivalve faunas by R. M. c. EAGAR Namurian cliff sections are described in detail. A minimum thickness of about 76 m is ascribed to Namurian A and 198 m and 104 m respectively to Namurian B and C. Faunal marker bands enable the Chokierian. Marsdenian and Yeadonian Stages to be recognised and the detailed structure to be worked out and this confirms the structural interpretation of Dixon.

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