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.
Corradini, C., Mossoni, A., Corriga, M.G., Spalletta, C. (2021). The Devonian/Carboniferous boundary in Sardinia (Italy). PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS, 101(2), 507-514 [10.1007/s12549-019-00411-5].
The Devonian/Carboniferous boundary in Sardinia (Italy)
Corradini, Carlo
;Spalletta, ClaudiaMembro del Collaboration Group
2021
Abstract
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.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
