| Reference Type | Journal (article/letter/editorial) |
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| Title | Cambrian stratigraphy of St Tudwal's Peninsula, Gwynedd, northwest Wales |
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| Journal | Geological Magazine |
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| Authors | Young, T. | Author |
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| Martin, F. | Author |
| Dean, W. T. | Author |
| Rushton, A. W. A. | Author |
| Year | 1994 (May) | Volume | 131 |
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| Issue | 3 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800011109Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 256190 | Long-form Identifier | mindat:1:5:256190:9 |
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| GUID | 0 |
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| Full Reference | Young, T., Martin, F., Dean, W. T., Rushton, A. W. A. (1994) Cambrian stratigraphy of St Tudwal's Peninsula, Gwynedd, northwest Wales. Geological Magazine, 131 (3) 335-360 doi:10.1017/s0016756800011109 |
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| Plain Text | Young, T., Martin, F., Dean, W. T., Rushton, A. W. A. (1994) Cambrian stratigraphy of St Tudwal's Peninsula, Gwynedd, northwest Wales. Geological Magazine, 131 (3) 335-360 doi:10.1017/s0016756800011109 |
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| In | (1994, May) Geological Magazine Vol. 131 (3) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractLithostratigraphic units of early to late Cambrian age established by T. C. Nicholas in 1915 in the St Tudwal's Peninsula are revised. They comprise, in ascending order: Hell's Mouth Formation (> 190 m); Trwyn y Fulfran Formation (37 m);Cilan Formation (400 m); Ceiriad Formation (40 m seen); Nant-y-big Formation (> 110 m seen); Maentwrog Formation (in part, 50 m seen, an estimated 250 m concealed); Ffestiniog Flags Formation (in part, c. 120m seen). The ‘calcareous grit’ at the top of Nicholas's Nant-pig Mudstones spans the unconformable boundary between the Nant-y-big and Maentwrog formations. Previously described limestone clasts in the ‘grit’ are probably erosional remnants of an in situ bioclastic limestone bed; their contained trilobites include genera and species found in the Andrarum Limestone (late Middle Cambrian) of Scania, Sweden. Acritarchs are documented and compared particularly with those from eastern Newfound-land. Those from the highest part of the ‘calcareous grit’ include Cymatiogalea sp. and are of late Cambrian age. One new species, Heliosphaeridium? llynense Martin, comes from the lower part of the Nant-y-big Formation (middle Middle Cambrian), where it appears a little earlier than the Adara alea Biozone. |
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