Quick
Search: 		  
advanced search
 GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help 
  Journal of the Geological Society   Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Journal of the Geological Society; August 1990; v. 147; no. 4; p. 693-701; DOI: 10.1144/gsjgs.147.4.0693
© 1990 Geological Society of London
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by DIMBERLINE, A. J.
Right arrow Articles by WOODCOCK, N. H.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Article

A laminated hemipelagic facies from the Wenlock and Ludlow of the Welsh Basin

A. J. DIMBERLINE, A. BELL and N. H. WOODCOCK

Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK

A hemipelagic fades from the Silurian succession in Wales consists of finely laminated, dominantly silt-grade sediment. It can be interbedded with sand- or mud-grade turbidites, or can occur as an independent facies. Its occurrence and character was controlled mainly by low bottom water oxicity. The pelagic fauna of the laminated hemipelagite supports this view. Many of the silt-grade particles have an aggregate structure and probably represent the faecal pellets of oceanic zooplankton. The fine lamination is thought to have formed by alternations of planktonic blooms and increased discharges of silt into the basin. By comparison with modern examples this alternation was likely to have been annual or seasonal.




This article has been cited by other articles:


Home page
 Proceedings of the Yorkshire Geological SocietyHome page
R. B. Rickards and N. H. Woodcock
Stratigraphical revision of the Windermere Supergroup (Late Ordovician-Silurian in the southern Howgill Fells, NW England
Proceedings of the Yorkshire Geological Society, November 1, 2005; 55(4): 263 - 285.
[Abstract] [PDF]

Home page
 Geological Society, London, Special PublicationsHome page
J. H. Morris, N. H. Woodcock, and M. P. A. Howe
The Silurian succession of the Isle of Man: the late Wenlock Niarbyl Formation, Dalby Group
Geological Society, London, Special Publications, January 1, 1999; 160(1): 189 - 211.
[Abstract] [PDF]

Home page
 Geological Society, London, Special PublicationsHome page
A. E. S. Kemp
Laminated sediments as palaeo-indicators
Geological Society, London, Special Publications, January 1, 1996; 116(1): vii - xii.
[Abstract] [PDF]

Home page
 Proceedings of the Yorkshire Geological SocietyHome page
R. J. Merriman, D. C. Rex, N. J. Soper, and D. R. Peacor
The age of Acadian cleavage in northern England, UK: K-Ar and TEM analysis of a Silurian metabentonite
Proceedings of the Yorkshire Geological Society, June 1, 1995; 50(3): 255 - 265.
[Abstract] [PDF]

Home page
 Geological Society, London, Special PublicationsHome page
D. J. Bottjer, K. A. Campbell, J. K. Schubert, and M. L. Droser
Palaeoecological models, non-uniformitarianism, and tracking the changing ecology of the past
Geological Society, London, Special Publications, January 1, 1995; 83(1): 7 - 26.
[Abstract] [PDF]

Home page
 Journal of the Geological SocietyHome page
Discussion on a laminated hemipelagic facies from the Wenlock and Ludlow of the Welsh Basin
Journal of the Geological Society, December 1, 1991; 148(6): 1145 - 1148.
[Abstract] [PDF]


JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Geological Society of London