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Reply to ‘Early Silurian positive δ 13 C excursions and their relationship to glaciations, sea‐level changes and extinction events: discussion’ by Bradley D. Cramer and Axel Munnecke

2008; Wiley; Volume: 43; Issue: 4 Linguagem: Inglês

10.1002/gj.1110

1099-1034

David K. Loydell,

Geochemistry and Elemental Analysis

Geological JournalVolume 43, Issue 4 p. 511-515 Reply Article Reply to 'Early Silurian positive δ13C excursions and their relationship to glaciations, sea-level changes and extinction events: discussion' by Bradley D. Cramer and Axel Munnecke David K. Loydell, Corresponding Author David K. Loydell [email protected] School of Earth and Environmental Sciences, University of Portsmouth, Portsmouth, UKSchool of Earth and Environmental Sciences, University of Portsmouth, Burnaby Road, Portsmouth PO1 3QL, UK.Search for more papers by this author David K. Loydell, Corresponding Author David K. Loydell [email protected] School of Earth and Environmental Sciences, University of Portsmouth, Portsmouth, UKSchool of Earth and Environmental Sciences, University of Portsmouth, Burnaby Road, Portsmouth PO1 3QL, UK.Search for more papers by this author First published: 10 April 2008 https://doi.org/10.1002/gj.1110Citations: 15AboutPDF 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 onEmailFacebookTwitterLinkedInRedditWechat REFERENCES Bickert T, Pätzold J, Samtleben C, Munnecke A. 1997. 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