Research output: Contribution to journal › Article › peer-review
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 journal › Article › peer-review
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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