John J. Cawley: Unterschied zwischen den Versionen

Aus WORLDFISH WIKI
Wechseln zu: Navigation, Suche
(Publikationen)
 
(Eine dazwischenliegende Version desselben Benutzers wird nicht angezeigt)
Zeile 10: Zeile 10:
 
{{Cawley & Kriwet, 2017}}<!--A new pycnodont fish, Scalacurvichthys naishi gen. et sp. nov., from the Late Cretaceous of Israel.-->
 
{{Cawley & Kriwet, 2017}}<!--A new pycnodont fish, Scalacurvichthys naishi gen. et sp. nov., from the Late Cretaceous of Israel.-->
 
{{Cawley et al., 2018}}<!--A quantitative approach to determine the taxonomic identity and ontogeny of the pycnodontiform fish Pycnodus (Neopterygii, Actinopterygii) from the Eocene of Bolca Lagerstätte, Italy-->
 
{{Cawley et al., 2018}}<!--A quantitative approach to determine the taxonomic identity and ontogeny of the pycnodontiform fish Pycnodus (Neopterygii, Actinopterygii) from the Eocene of Bolca Lagerstätte, Italy-->
 +
{{Cawley et al., 2020}}<!--Njoerdichthys dyckerhoffi gen. et sp. nov. (Pycnodontiformes, lower Turonian) northward migration caused by the Cretaceous Thermal Maximum-->
 +
{{Cawley & Kriwet, 2024}}<!--The Fossil Record and Diversity of Pycnodontiform Fishes in Non-Marine Environments-->

Aktuelle Version vom 10. April 2024, 13:01 Uhr

John Joseph Cawley

  • Department of Palaeontology, University of Vienna, Geozentrum, Althanstarße 14, 1090 Vienna, Austria.
  • E-mail: john.cawley@univie.ac.at

Beschriebene Taxa

Publikationen

  • Cawley, J.J. & Kriwet, J. 2017. A new pycnodont fish, Scalacurvichthys naishi gen. et sp. nov., from the Late Cretaceous of Israel. Journal of Systematic Palaeontology. 16 (8): 659–673. (doi) Zitatseite 
  • Cawley, J.J., Marramà, G., Carnevale, G. & Kriwet, J. 2018. A quantitative approach to determine the taxonomic identity and ontogeny of the pycnodontiform fish Pycnodus (Neopterygii, Actinopterygii) from the Eocene of Bolca Lagerstätte, Italy. PeerJ, '6: e4809. (doi) Zitatseite 
  • Cawley, J., Lehmann, J., Wiese, F. & Kriwet, J. 2020. Njoerdichthys dyckerhoffi gen. et sp. nov. (Pycnodontiformes, lower Turonian) northward migration caused by the Cretaceous Thermal Maximum. Cretaceous Research, 116: Article 104590. (doi) Zitatseite 
  • Cawley, J.J. & Kriwet, J. 2024. The Fossil Record and Diversity of Pycnodontiform Fishes in Non-Marine Environments. Diversity, 16 (4): 225. (doi) Zitatseite