The Devonian-Carboniferous boundary in the Carnic Alps (Austria
and Italy)

J 2021

The Devonian-Carboniferous boundary in the Carnic Alps (Austria and Italy)

SPALLETTA, Claudia; Carlo CORRADINI; Raimund FEIST; Dieter KORN; Tomáš KUMPAN et. al.

Základní údaje

Originální název

The Devonian-Carboniferous boundary in the Carnic Alps (Austria and Italy)

Autoři

SPALLETTA, Claudia; Carlo CORRADINI; Raimund FEIST; Dieter KORN; Tomáš KUMPAN; Maria Cristina PERRI; Monica PONDRELLI a Corrado VENTURINI

Vydání

Palaeobiodiversity and palaeoenvironments, Heidelberg, Springer-Verlag, 2021, 1867-1594

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10506 Paleontology

Stát vydavatele

Německo

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 1.736

Kód RIV

RIV/00216224:14310/21:00120670

Organizační jednotka

Přírodovědecká fakulta

DOI

https://doi.org/10.1007/s12549-019-00413-3

UT WoS

000513046100001

EID Scopus

2-s2.0-85079524331

Klíčová slova anglicky

Devonian-Carboniferous boundary; Conodont biostratigraphy; Hangenberg event; Geochemistry; Carnic Alps; Austria; Italy

Štítky

14315010, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 19. 7. 2021 09:49, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

In the Carnic Alps there are four sections exposing rocks across the Devonian–Carboniferous boundary: the Grüne Schneid and the Kronhofgraben sections in Austria, the Plan di Zermula A and the Sentiero per Cresta Verde sections in Italy. All of them are mainly composed of limestone and span from the late Famennian through the Tournaisian. In the Kronhofgraben and Plan di Zermula A sections, the limestone sedimentation is interrupted by black shales interpreted as equivalent of the Hangenberg Black Shales. The Grüne Schneid and the Sentiero per Cresta Verde sections are two of the few sections worldwide, where the calcareous sedimentation is continuous. The main extinction event registered at the end of the Devonian is testified not only in the sections where the calcareous sedimentation was replaced by black shales sedimentation but also in the Grüne Schneid and in the Sentiero per Cresta Verde sections. Data on conodont biostratigraphy and biofacies, the content in ammonoids, and trilobites and geochemistry patterns from all sections are here summarised and reviewed. These data-set allow to conclude that the four Carnic Alps sections positively test the suitability of the timeline proposed by the DCB working group for the definition of the revised Devonian–Carboniferous boundary.

Citovat

SPALLETTA, Claudia; Carlo CORRADINI; Raimund FEIST; Dieter KORN; Tomáš KUMPAN; Maria Cristina PERRI; Monica PONDRELLI a Corrado VENTURINI. The Devonian-Carboniferous boundary in the Carnic Alps (Austria and Italy). Palaeobiodiversity and palaeoenvironments. Heidelberg: Springer-Verlag, 2021, roč. 101, č. 2, s. 487-505. ISSN 1867-1594. Dostupné z: https://doi.org/10.1007/s12549-019-00413-3.

@article{1674565,
   author = {Spalletta, Claudia and Corradini, Carlo and Feist, Raimund and Korn, Dieter and Kumpan, Tomáš and Perri, Maria Cristina and Pondrelli, Monica and Venturini, Corrado},
   article_location = {Heidelberg},
   article_number = {2},
   doi = {https://doi.org/10.1007/s12549-019-00413-3},
   keywords = {Devonian-Carboniferous boundary; Conodont biostratigraphy; Hangenberg event; Geochemistry; Carnic Alps; Austria; Italy},
   language = {eng},
   issn = {1867-1594},
   journal = {Palaeobiodiversity and palaeoenvironments},
   title = {The Devonian-Carboniferous boundary in the Carnic Alps (Austria and Italy)},
   url = {https://doi.org/10.1007/s12549-019-00413-3},
   volume = {101},
   year = {2021}
}

TY  - JOUR
ID  - 1674565
AU  - Spalletta, Claudia - Corradini, Carlo - Feist, Raimund - Korn, Dieter - Kumpan, Tomáš - Perri, Maria Cristina - Pondrelli, Monica - Venturini, Corrado
PY  - 2021
TI  - The Devonian-Carboniferous boundary in the Carnic Alps (Austria and Italy)
JF  - Palaeobiodiversity and palaeoenvironments
VL  - 101
IS  - 2
SP  - 487-505
EP  - 487-505
PB  - Springer-Verlag
SN  - 18671594
KW  - Devonian-Carboniferous boundary
KW  - Conodont biostratigraphy
KW  - Hangenberg event
KW  - Geochemistry
KW  - Carnic Alps
KW  - Austria
KW  - Italy
UR  - https://doi.org/10.1007/s12549-019-00413-3
L2  - https://doi.org/10.1007/s12549-019-00413-3
N2  - In the Carnic Alps there are four sections exposing rocks across the Devonian–Carboniferous boundary: the Grüne Schneid and the Kronhofgraben sections in Austria, the Plan di Zermula A and the Sentiero per Cresta Verde sections in Italy. All of them are mainly composed of limestone and span from the late Famennian through the Tournaisian. In the Kronhofgraben and Plan di Zermula A sections, the limestone sedimentation is interrupted by black shales interpreted as equivalent of the Hangenberg Black Shales. The Grüne Schneid and the Sentiero per Cresta Verde sections are two of the few sections worldwide, where the calcareous sedimentation is continuous. The main extinction event registered at the end of the Devonian is testified not only in the sections where the calcareous sedimentation was replaced by black shales sedimentation but also in the Grüne Schneid and in the Sentiero per Cresta Verde sections. Data on conodont biostratigraphy and biofacies, the content in ammonoids, and trilobites and geochemistry patterns from all sections are here summarised and reviewed. These data-set allow to conclude that the four Carnic Alps sections positively test the suitability of the timeline proposed by the DCB working group for the definition of the revised Devonian–Carboniferous boundary.
ER  -

SPALLETTA, Claudia; Carlo CORRADINI; Raimund FEIST; Dieter KORN; Tomáš KUMPAN; Maria Cristina PERRI; Monica PONDRELLI a Corrado VENTURINI. The Devonian-Carboniferous boundary in the Carnic Alps (Austria and Italy). \textit{Palaeobiodiversity and palaeoenvironments}. Heidelberg: Springer-Verlag, 2021, roč.~101, č.~2, s.~487-505. ISSN~1867-1594. Dostupné z: https://doi.org/10.1007/s12549-019-00413-3.

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