Abstract
Journal of Quaternary ScienceVolume 17, Issue 1 p. 97-99 Correspondence Comment: the Greenland 8200 cal. yr BP event detected in loss-on-ignition profiles in Norwegian lacustrine sediment sequences A. Nesje S. O. Dahl (2001)(Journal of Quaternary Science, 16, 155-166) K.D. Bennett, Corresponding Author K.D. Bennett Keith.Bennett@geo.uu.se Quaternary Geology, Geocentrum, Villavägen 16, SE-75236 Uppsala, SwedenQuaternary Geology, Geocentrum, Villavägen 16, SE-75236 Uppsala, Sweden.Search for more papers by this author K.D. Bennett, Corresponding Author K.D. Bennett Keith.Bennett@geo.uu.se Quaternary Geology, Geocentrum, Villavägen 16, SE-75236 Uppsala, SwedenQuaternary Geology, Geocentrum, Villavägen 16, SE-75236 Uppsala, Sweden.Search for more papers by this author First published: 24 January 2002 https://doi.org/10.1002/jqs.667Citations: 18AboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onFacebookTwitterLinked InRedditWechat No abstract is available for this article.Citing Literature Volume17, Issue1January 2002Pages 97-99 RelatedInformation
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
