Abstract
Research Article| April 01, 2003 Reply Michael M. Joachimski; Michael M. Joachimski 1Institut für Geologie und Mineralogie, Schlossgarten 5, 91054 Erlangen, Germany Search for other works by this author on: GSW Google Scholar Werner Buggisch Werner Buggisch 1Institut für Geologie und Mineralogie, Schlossgarten 5, 91054 Erlangen, Germany Search for other works by this author on: GSW Google Scholar Geology (2003) 31 (4): 384. https://doi.org/10.1130/0091-7613(2003)031<0384:>2.0.CO;2 Article history first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Michael M. Joachimski, Werner Buggisch; Reply. Geology 2003;; 31 (4): 384. doi: https://doi.org/10.1130/0091-7613(2003)031<0384:>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Gong and Xu question whether the positive excursions in conodont apatite δ18O during the Late Frasnian and Frasnian-Famennian transition are the effect of climatic cooling. Instead, they favor changes in surface-water salinity in order to account for the observed shifts in δ18O of +1‰ to +1.5‰. Gong and Xu do not provide any data that may support higher surface-water salinity during the late Frasnian, but speculate on hypersalinity, red tides, and anoxia as potential causes of the Frasnian-Famennian extinction event. To our understanding, a change in surface-water salinity is not plausible. The studied sections were situated... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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