IMIS - Marine Onderzoeksgroepen | Compendium Kust en Zee

IMIS - Marine Onderzoeksgroepen

[ meld een fout in dit record ]mandje (1): toevoegen | toon Print deze pagina

one publication added to basket [231615]
Cambrian stratigraphy of St Tudwal's Peninsula, Gwynedd, northwest Wales
Young, T.; Martin, F.; Dean, W.T.; Rushton, A.W.A. (1994). Cambrian stratigraphy of St Tudwal's Peninsula, Gwynedd, northwest Wales. Geol. Mag. 131(3): 335-360. http://dx.doi.org/10.1017/S0016756800011109
In: Geological Magazine. Cambridge University Press: London. ISSN 0016-7568; e-ISSN 1469-5081, meer
Peer reviewed article  

Beschikbaar in  Auteurs 

Trefwoorden
    Geological time > Phanerozoic > Paleozoic > Palaeozoic > Cambrian
    Acritarcha [WoRMS]
    British Isles, Wales [Marine Regions]
    Marien/Kust

Auteurs  Top 
  • Young, T.
  • Martin, F.
  • Dean, W.T.
  • Rushton, A.W.A.

Abstract
    Lithostratigraphic 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. 120 m 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 Newfoundland. 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.

Alle informatie in het Integrated Marine Information System (IMIS) valt onder het VLIZ Privacy beleid Top | Auteurs