Conodonts across the Silurian/Devonian boundary in the Carnic Alps (Austria and Italy)

2020 ◽  
Vol 549 ◽  
pp. 109097 ◽  
Author(s):  
Carlo Corradini ◽  
Maria G. Corriga ◽  
Monica Pondrelli ◽  
Thomas J. Suttner
Keyword(s):  
Carnic Alps

Polyphase metamorphism in the eastern Carnic Alps (N Italy–S Austria): clay minerals and conodont Colour Alteration Index evidence

2007 ◽  
Vol 97 (6) ◽  
pp. 1213-1229 ◽  
Author(s):  
Covadonga Brime ◽  
Maria Cristina Perri ◽  
Monica Pondrelli ◽  
Claudia Spalletta ◽  
Corrado Venturini
Keyword(s):  
Clay Minerals ◽  
Carnic Alps ◽  
Conodont Colour Alteration Index ◽  
Polyphase Metamorphism ◽  
Colour Alteration

Geological map and stratigraphic evolution of the central sector of the Carnic Alps (Austria-Italy)

2020 ◽  
Vol 139 (3) ◽  
pp. 469-484
Author(s):  
Monica Pondrelli ◽  
Carlo Corradini ◽  
Claudia Spalletta ◽  
Luca Simonetto ◽  
Maria Cristina Perri ◽  
...  
Keyword(s):  
Carnic Alps ◽  
Geological Map ◽  
Stratigraphic Evolution

scholarly journals Chrono-, litho- and conodont bio-stratigraphy of the Rauchkofel Boden Section (Upper Ordovician – Lower Devonian), Carnic Alps, Austria

2017 ◽  
Vol 50 (4) ◽  
pp. 445-469 ◽  
Author(s):  
Hans Peter Schönlaub ◽  
Carlo Corradini ◽  
Maria G. Corriga ◽  
Annalisa Ferretti
Keyword(s):  
Lower Devonian ◽  
Upper Ordovician ◽  
Carnic Alps

The schulterkofel section in the Carnic Alps, Austria: Implications for the carboniferous-permian boundary

Facies ◽  
1993 ◽  
Vol 28 (1) ◽  
pp. 257-276 ◽  
Author(s):  
Franz Kahler ◽  
Karl Krainer
Keyword(s):  
Carnic Alps

Exceptional preservation in calcareous nodules

1985 ◽  
Vol 311 (1148) ◽  
pp. 67-73 ◽  
Keyword(s):  
Lower Triassic ◽  
Environmental Indicators ◽  
Carnic Alps ◽  
Upper Cambrian ◽  
Exceptional Preservation ◽  
Alum Shale ◽  
Shale Formation ◽  
The Common ◽  
Santana Formation ◽  
Barstow Formation

Preservation of soft integument in calcareous nodules seems to be more widespread geographically and stratigraphically than hitherto realized. It cannot be recognized in the field, and to recover such material requires special etching techniques. Such preservation can be of exceptional quality, with fossils preserved three dimensionally either by secondary phosphatization or by silicification. Coating as well as the replacement of integument has been observed even within the same sample. Methodical search for such preservation may be based on the common denominators of depositional, geochemical, and environmental indicators in previously described occurrences. As such exceptionally preserved material may be rare within the samples, large quantities of rock have to be prepared. The examples described here are from anthraconitic limestones (Orsten) of the Upper Cambrian Alum Shale Formation in Sweden. They are now known from many localities and from different trilobite zones. In addition nodules from the Lower Cretaceous Santana Formation in Brazil, the Upper Devonian cephalopod limestone in the Carnic Alps, the Lower Triassic of Spitzbergen and the Miocene Barstow Formation in California have all yielded extremely fine material.

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