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Scarce ctenacanthiform sharks from the Mississippian of Austria with an analysis of Carboniferous elasmobranch diversity in response to climatic and environmental changes. / Feichtinger, Iris; Ivanov, Alexander O.; Winkler, Viola; Dojen, Claudia; Kindlimann, René; Kriwet, Jürgen; Pfaff, Cathrin; Schraut, Gunnar; Stumpf, Sebastian.

In: Journal of Vertebrate Paleontology, Vol. 41, No. 2, e1925902, 24.06.2021.

Research output: Contribution to journalArticlepeer-review

Harvard

Feichtinger, I, Ivanov, AO, Winkler, V, Dojen, C, Kindlimann, R, Kriwet, J, Pfaff, C, Schraut, G & Stumpf, S 2021, 'Scarce ctenacanthiform sharks from the Mississippian of Austria with an analysis of Carboniferous elasmobranch diversity in response to climatic and environmental changes', Journal of Vertebrate Paleontology, vol. 41, no. 2, e1925902. https://doi.org/10.1080/02724634.2021.1925902

APA

Feichtinger, I., Ivanov, A. O., Winkler, V., Dojen, C., Kindlimann, R., Kriwet, J., Pfaff, C., Schraut, G., & Stumpf, S. (2021). Scarce ctenacanthiform sharks from the Mississippian of Austria with an analysis of Carboniferous elasmobranch diversity in response to climatic and environmental changes. Journal of Vertebrate Paleontology, 41(2), [e1925902]. https://doi.org/10.1080/02724634.2021.1925902

Vancouver

Author

Feichtinger, Iris ; Ivanov, Alexander O. ; Winkler, Viola ; Dojen, Claudia ; Kindlimann, René ; Kriwet, Jürgen ; Pfaff, Cathrin ; Schraut, Gunnar ; Stumpf, Sebastian. / Scarce ctenacanthiform sharks from the Mississippian of Austria with an analysis of Carboniferous elasmobranch diversity in response to climatic and environmental changes. In: Journal of Vertebrate Paleontology. 2021 ; Vol. 41, No. 2.

BibTeX

@article{8b49f92f0304410197030e611e73fb72,
title = "Scarce ctenacanthiform sharks from the Mississippian of Austria with an analysis of Carboniferous elasmobranch diversity in response to climatic and environmental changes",
abstract = "The Carboniferous is characterized by drastic climatic and environmental fluctuations, which include multiple phases of glaciation resulting in an icehouse climate. Additionally, dynamic continental reconfigurations forced the contraction of the Rheic Ocean resulting in the closure of the Rheic–Tethyan Gateway, which precluded further faunal exchanges between the North American and Eurasian marine realms. Interestingly, cartilaginous fishes seem to be relatively immune to these drastic climatic and environmental changes. The Eurasian fossil record of Paleozoic sharks is strongly biased towards intensively sampled localities from England, Ireland, Scotland, and the Russian Platform. Here we present rare dental material from the Serpukhovian (early Carboniferous) of Austria, adding new information to the paleogeographic distribution of ctenacanthiform sharks. The new material revealed the first record of the genus Saivodus in Central Europe and allowed us to recognize a new species, Cladodus gailensis sp. nov., and a remnant of fossilized cartilage. In an attempt to identify possible linkages between climatic or environmental fluctuations on shark diversity throughout the Carboniferous, we provide a synopsis of the distribution and diversity of elasmobranchs based on primary literature. This preliminary assessment at genus level indicates two pronounced events of extinction, with the first one occurring during the latest Mississippian and the second one towards the end of the Pennsylvanian. The first extinction event distinctly correlates with the known diversity decline of other marine inhabitants and the second occurred during an unstable period of multiple phases of glaciation.",
keywords = "PALEOZOIC ICE-AGE, CHONDRICHTHYAN, EXTINCTION, BRAINCASE, CLADODUS, HISTORY, ORIGINATION, GLACIATION, ORDOVICIAN, EVOLUTION",
author = "Iris Feichtinger and Ivanov, {Alexander O.} and Viola Winkler and Claudia Dojen and Ren{\'e} Kindlimann and J{\"u}rgen Kriwet and Cathrin Pfaff and Gunnar Schraut and Sebastian Stumpf",
note = "Publisher Copyright: {\textcopyright} 2021, by the Society of Vertebrate Paleontology.",
year = "2021",
month = jun,
day = "24",
doi = "10.1080/02724634.2021.1925902",
language = "English",
volume = "41",
journal = "Journal of Vertebrate Paleontology",
issn = "0272-4634",
publisher = "Taylor & Francis",
number = "2",

}

RIS

TY - JOUR

T1 - Scarce ctenacanthiform sharks from the Mississippian of Austria with an analysis of Carboniferous elasmobranch diversity in response to climatic and environmental changes

AU - Feichtinger, Iris

AU - Ivanov, Alexander O.

AU - Winkler, Viola

AU - Dojen, Claudia

AU - Kindlimann, René

AU - Kriwet, Jürgen

AU - Pfaff, Cathrin

AU - Schraut, Gunnar

AU - Stumpf, Sebastian

N1 - Publisher Copyright: © 2021, by the Society of Vertebrate Paleontology.

PY - 2021/6/24

Y1 - 2021/6/24

N2 - The Carboniferous is characterized by drastic climatic and environmental fluctuations, which include multiple phases of glaciation resulting in an icehouse climate. Additionally, dynamic continental reconfigurations forced the contraction of the Rheic Ocean resulting in the closure of the Rheic–Tethyan Gateway, which precluded further faunal exchanges between the North American and Eurasian marine realms. Interestingly, cartilaginous fishes seem to be relatively immune to these drastic climatic and environmental changes. The Eurasian fossil record of Paleozoic sharks is strongly biased towards intensively sampled localities from England, Ireland, Scotland, and the Russian Platform. Here we present rare dental material from the Serpukhovian (early Carboniferous) of Austria, adding new information to the paleogeographic distribution of ctenacanthiform sharks. The new material revealed the first record of the genus Saivodus in Central Europe and allowed us to recognize a new species, Cladodus gailensis sp. nov., and a remnant of fossilized cartilage. In an attempt to identify possible linkages between climatic or environmental fluctuations on shark diversity throughout the Carboniferous, we provide a synopsis of the distribution and diversity of elasmobranchs based on primary literature. This preliminary assessment at genus level indicates two pronounced events of extinction, with the first one occurring during the latest Mississippian and the second one towards the end of the Pennsylvanian. The first extinction event distinctly correlates with the known diversity decline of other marine inhabitants and the second occurred during an unstable period of multiple phases of glaciation.

AB - The Carboniferous is characterized by drastic climatic and environmental fluctuations, which include multiple phases of glaciation resulting in an icehouse climate. Additionally, dynamic continental reconfigurations forced the contraction of the Rheic Ocean resulting in the closure of the Rheic–Tethyan Gateway, which precluded further faunal exchanges between the North American and Eurasian marine realms. Interestingly, cartilaginous fishes seem to be relatively immune to these drastic climatic and environmental changes. The Eurasian fossil record of Paleozoic sharks is strongly biased towards intensively sampled localities from England, Ireland, Scotland, and the Russian Platform. Here we present rare dental material from the Serpukhovian (early Carboniferous) of Austria, adding new information to the paleogeographic distribution of ctenacanthiform sharks. The new material revealed the first record of the genus Saivodus in Central Europe and allowed us to recognize a new species, Cladodus gailensis sp. nov., and a remnant of fossilized cartilage. In an attempt to identify possible linkages between climatic or environmental fluctuations on shark diversity throughout the Carboniferous, we provide a synopsis of the distribution and diversity of elasmobranchs based on primary literature. This preliminary assessment at genus level indicates two pronounced events of extinction, with the first one occurring during the latest Mississippian and the second one towards the end of the Pennsylvanian. The first extinction event distinctly correlates with the known diversity decline of other marine inhabitants and the second occurred during an unstable period of multiple phases of glaciation.

KW - PALEOZOIC ICE-AGE

KW - CHONDRICHTHYAN

KW - EXTINCTION

KW - BRAINCASE

KW - CLADODUS

KW - HISTORY

KW - ORIGINATION

KW - GLACIATION

KW - ORDOVICIAN

KW - EVOLUTION

UR - http://www.scopus.com/inward/record.url?scp=85108424597&partnerID=8YFLogxK

UR - https://www.mendeley.com/catalogue/bafd4051-bdcc-3159-9ab8-1825d7a80577/

U2 - 10.1080/02724634.2021.1925902

DO - 10.1080/02724634.2021.1925902

M3 - Article

AN - SCOPUS:85108424597

VL - 41

JO - Journal of Vertebrate Paleontology

JF - Journal of Vertebrate Paleontology

SN - 0272-4634

IS - 2

M1 - e1925902

ER -

ID: 84332094