skip to navigation
ADS Main Website
Help
|
Login
/
Browse by Series
/
Series
/ Journal Issue
The Holocene 19 (7)
Title
The title of the publication or report
Title:
The Holocene 19 (7)
Series
The series the publication or report is included in
Series:
The Holocene
Volume
Volume number and part
Volume:
19 (7)
Number of Pages
The number of pages in the publication or report
Number of Pages:
115
Publication Type
The type of publication - report, monograph, journal article or chapter from a book
Publication Type:
Journal
Year of Publication
The year the book, article or report was published
Year of Publication:
2009
Source
Where the record has come from or which dataset it was orginally included in.
Source:
BIAB (biab_online)
Relations
Other resources which are relevant to this publication or report
Relations:
URI:
http://hol.sagepub.com/content/19/7.toc
Created Date
The date the record of the pubication was first entered
Created Date:
14 Feb 2011
Please click on an Article link to go to the Article Details.
Article Title
Access Type
Author / Editor
Page
Start/End
Abstract
Holocene comment and reply; The disappearance of S. imbricatum from European r...
Bjorn J M Robroek
Jean G M Waucomont
M G C Schouten
1093 - 1094
Comment on McClymont et al. (The Holocene 18 (2008) 991'“1002, suggesting that decreased water-table depth and increased airborne pollution may not be the best explanations for the decline, given its persistence in modern Irish peatlands. Proposes a localised fire-event as an alternative explanation for the decline. PP-B
The disappearance of Sphagnum imbricatum from Butterburn Flow, UK; a reply to comments by Bjorn Robroek et al.
Erin L McClymont
Dimitri Mauquoy
Dan Yeloff
Peter Broekens
Bas Geel, van
Dan J Charman
Richard D Pancost
Frank M Chambers
Richard P Evershed
1094 - 1097
Clarifies the site of study; data was presented only from Butterburn Flow, northern England, not from Wales or Ireland as suggested in the opening paragraph of Robroek's comment. Notes that the original papers notes that replacement of S. imbricatum by S. magellanicum occurred over c. 44 years, but that it is proposed that it may have been longer owing to evidence for reduced peat accumulation across the transition.