Geochemical evidence for major environmental change at the Devonian¿Carboniferous boundary in the Carnic Alps and the Rhenish Massif

Volume: 240, Issue: 1, Pages: 146 - 160
Published: Oct 6, 2006
Abstract
null null A positive carbon isotope excursion is reported for the global Hangenberg Event near the Devonian–Carboniferous boundary, one of the most significant Phanerozoic mass extinction events. The null δ null 13 C excursion occurs both in micritic limestones and in sedimentary organic matter of black shales and limestones from different palaeogeographical regions, which were precisely correlated by conodont biostratigraphy. The excursion...
Paper Details
Title
Geochemical evidence for major environmental change at the Devonian¿Carboniferous boundary in the Carnic Alps and the Rhenish Massif
Published Date
Oct 6, 2006
Volume
240
Issue
1
Pages
146 - 160
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