Journal
PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS
Volume 101, Issue 2, Pages 507-514Publisher
SPRINGER HEIDELBERG
DOI: 10.1007/s12549-019-00411-5
Keywords
Devonian; Carboniferous boundary; Hangenberg event; Sardinia; Conodonts; Magnetic susceptibility
Categories
Funding
- Cagliari University grant (PRID)
- Cagliari University grant (FIR)
- Cagliari University grant (FdS-RAS) [F72F16003080002]
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In Sardinia, Italy, two sections at the southeastern part of the island display the Devonian/Carboniferous Boundary, showing a limestone sequence from the middle Famennian to the lower Tournaisian Siphonodella jii Zone, with a thin level of shales representing the Hangenberg Event. Data on conodont biostratigraphy and magnetic susceptibility across this boundary are summarized and reviewed.
In Sardinia (Italy) two sections, located in the southeastern part of the island, expose the Devonian/Carboniferous Boundary: the Monte Taccu Section and the Bruncu Bullai section. Both expose limestones from the middle Famennian to the lower Tournaisian Siphonodella jii Zone. The limestone sequence is interrupted by a thin level of shales representing the Hangenberg Event. Data on conodont biostratigraphy and magnetic susceptibility across the Devonian/Carboniferous Boundary are here summarised and reviewed.
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