Published January 9, 2024 | Version v1
Taxonomic treatment Open

Geosaurini Bonaparte 1845

  • 1. School of GeoSciences, Grant Institute, The King's Buildings, University of Edinburgh, James Hutton Road, Edinburgh, EH 9 3 FE, United Kingdom & LWL-Museum für Naturkunde, Sentruper Strasse 285, 48161 Münster, Germany
  • 2. Department of Anatomical Sciences, Stony Brook University, Stony Brook, NY 11794, USA
  • 3. Staatliches Museum für Naturkunde, Rosenstein 1, 70191 Stuttgart, Germany
  • 4. Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), División Paleontología Vertebrados, Museo de La Plata, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, B 1900 La Plata, Buenos Aires, Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) & Departamento de Diversidade e Ecologia, Faculdade de Biociências, Pontifícia Universidade Católica do Rio Grande do Sul, Av. Ipiranga 6681, Prédio 12, Porto Alegre, 90619 - 900, Brazil & Setor de Paleontologia, Museu de Ciências e Tecnologia, Pontifícia Universidade Católica do Rio Grande do Sul, Av. Ipiranga 6681, Prédio 40, Porto Alegre, 90619 - 900, Brazil
  • 5. Departamento de Diversidade e Ecologia, Faculdade de Biociências, Pontifícia Universidade Católica do Rio Grande do Sul, Av. Ipiranga 6681, Prédio 12, Porto Alegre, 90619 - 900, Brazil & Setor de Paleontologia, Museu de Ciências e Tecnologia, Pontifícia Universidade Católica do Rio Grande do Sul, Av. Ipiranga 6681, Prédio 40, Porto Alegre, 90619 - 900, Brazil
  • 6. 5, Villa Jeanne-d'Arc, 92340 Bourg-la-Reine, France
  • 7. Naturkunde-Museum Bielefeld, Abteilung Geowissenschaften, Adenauerplatz 2, 33602 Bielefeld, Germany
  • 8. Eberhard-Karls-University Tübingen, Fachbereich Geowissenschaften, Sigwartstrasse 10, 72074 Tübingen, Germany
  • 9. Department of Geosciences, Virginia Tech, 4044 Derring Hall 926 West Campus Drive, Blacksburg 24061, Virginia, USA & School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham B 15 2 TT, United Kingdom
  • 10. Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), División Paleontología Vertebrados, Museo de La Plata, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, B 1900 La Plata, Buenos Aires, Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET)
  • 11. Laboratoire de Paléontologie, Evolution, Paléoécosystèmes et Paléoprimatologie, CNRS UMR 7262, Department of Geosciences, University of Poitiers, 86073 Poitiers Cedex 9, France
  • 12. School of GeoSciences, Grant Institute, The King's Buildings, University of Edinburgh, James Hutton Road, Edinburgh, EH 9 3 FE, United Kingdom

Description

Geosaurini Bonaparte, 1845 (Zoological Code)

Geosaurini Cau and Fanti 2011: 551, converted clade name (PhyloCode)

RegNum registration number 1021.

Type genus: Geosaurus Cuvier 1824.

Etymology

‘Pertaining to Geosaurus ’. The stem Geosaur - is based on the genus Geosaurus. - ini is a Latin masculine plural suffix for ‘pertaining to’. Under Article 29.2 of the Zoological Code, the suffix - ini denotes a tribe rank within the family-group.

Geological range

Middle Jurassic (early Callovian) to Early Cretaceous (earliest Aptian) (Young et al. 2013, 2023 a, Chiarenza et al. 2015, Foffa et al. 2018, Sachs et al. 2020).

PhyloCode phylogenetic definition

The smallest clade within Metriorhynchidae containing Tyrannoneustes lythrodectikos Young et al., 2013, Geosaurus giganteus (von Sömmerring 1816), Torvoneustes carpenteri (Wilkinson et al. 2008), and Dakosaurus maximus (Plieninger 1846).

Reference phylogeny

Fig. 3.

Zoological Code diagnosis and PhyloCode diagnostic apomorphies

Metriorhynchid crocodylomorphs with the following unique combination of characters (4): prefrontal lateral border is a continuous convex curve, with an inflexion point of approximately 60–70° from the anteroposterior axis of the skull (209.1); coronoid process ventral to both the retroarticular process and glenoid process (488.1); deeply excavated surangulodentary groove (529.2); enlargement of the anterior maxillary tooth crowns (626.1–2).

Composition

Tyrannoneustes, Purranisaurus, Torvoneustes, the subclade Geosaurina, the subclade Plesiosuchina, the subclade Dakosaurina, and multiple taxa that do not have a valid generic assignment.

Comments

Authorship: The nomen Geosaurini was first used by Cau and Fanti (2011), however, under the Zoological Code Bonaparte 1845 is the nominal authority. The nominal author of a family-group is the author who first erected a family-group taxon that is valid (in fulfilment of Article 11), and in accordance with the Zoological Code Principle of Coordination applied to family-group names (Article 36.1). Under the PhyloCode, Cau and Fanti (2011) is the nominal authority.

Prior phylogenetic definition: Cau and Fanti (2011) defined Geosaurini as the least inclusive clade, including Geosaurus giganteus (von Sömmerring 1816), Torvoneustes carpenteri (Wilkinson et al. 2008), and Dakosaurus maximus (Plieninger 1846). Here we have added Tyrannoneustes lythrodectikos to the list of internal specifiers.

Characteristics: Many of the tooth crown characters (including those relating to the reduction in number, increase in crown size, and those scoring for contiguous denticles) independently evolved in lineages within Geosaurini rather than at the base of the clade (e.g. see: Foffa et al. 2018). The discovery that the geosaurin lineages originated in the Middle Jurassic (e.g. Foffa et al. 2018) and the discovery of Tyrannoneustes (Young et al. 2013, Foffa and Young 2014) have altered character polarity at the base of the clade.

Cau and Fanti (2011: 551) listed the following characters as being diagnostic for Geosaurini: the presence of prefrontal with the inflexion point directed caudally at an angle of less than 70° from the rostrocaudal axis of the skull; the presence of a very narrow (close to 45°) angle between the medial and the caudolateral processes of the frontal; by the caudal expansion of the supratemporal fossa beyond the parietal; the reduction of the basal tubera; the elongation of the maxillary tooth crowns; and the reduction of the humerus. Two out of five of those characters still define the clade Dakosaurus + Plesiosuchus + Torvoneustes.

Notes

Published as part of Young, Mark T., Wilberg, Eric W., Johnson, Michela M., Herrera, Yanina, Brandalise, Marco de Andrade, Brignon, Arnaud, Sachs, Sven, Abel, Pascal, Foffa, Davide, Fernández, Marta S., Vignaud, Patrick, Cowgill, Thomas & Brusatte, Stephen L., 2024, The history, systematics, and nomenclature of Thalattosuchia (Archosauria: Crocodylomorpha), pp. 547-617 in Zoological Journal of the Linnean Society 200 (2) on pages 606-607, DOI: 10.1093/zoolinnean/zlad165, http://zenodo.org/record/11241243

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Linked records

Additional details

References

  • Bonaparte CL. Specchio Generale dei Sistemi Erpetologico, Anfibiologico ed Ittiologico. Milan: Giacomo Pirola, 1845, 11.
  • Cau A, Fanti F. The oldest known metriorhynchid crocodylian from the Middle Jurassic of North-eastern Italy: Neptunidraco ammoniticus gen et sp nov. Gondwana Research 2011; 19: 550 - 65. https: // doi. org / 10.1016 / j. gr. 2010.07.007
  • Cuvier G. Recherches sur les Ossemens Fossiles, ou l'on retablit les Caracteres de Plusieurs Animaux dont les Revolutions du Globe ont Detruit les Especes, Nouvelle edition, Vol. 5, 2 e partie. Paris: G. Dufour et E. d'Ocagne, 1824.
  • Young MT, Andrade MB, Brusatte SL et al. The oldest known metriorhynchid super-predator: a new genus and species from the Middle Jurassic of England, with implications for serration and mandibular evolution in predacious clades. Journal of Systematic Palaeontology 2013; 11: 475 - 513.
  • Young MT, Zverkov NG, Arkhangelsky MS et al. Thalattosuchian crocodylomorphs from European Russia, and new insights into metriorhynchid tooth serration evolution and their palaeolatitudinal distribution. PeerJ 2023 a; 11: e 15781. https: // doi. org / 10.7717 / peerj. 15781
  • Chiarenza A, Foffa D, Young MT et al. The youngest record of metriorhynchid crocodylomorphs, with implications for the extinction of Thalattosuchia. Cretaceous Research 2015; 56: 608 - 16.
  • Foffa D, Young MT, Brusatte SL et al. A new metriorhynchid crocodylomorph from the Oxford Clay Formation (Middle Jurassic) of England, with implications for the origin and diversification of Geosaurini. Journal of Systematic Palaeontology 2018; 16: 1123 - 43. https: // doi. org / 10.1080 / 14772019.2017.1367730
  • Sachs S, Young MT, Hornung J. The enigma of Enaliosuchus, and a reassessment of the Early Cretaceous fossil record of Metriorhynchidae. Cretaceous Research 2020; 114: 104479.
  • von Sommerring ST. Ueber die Lacerta gigantea der Vorwelt. Denkschriften der Koniglichen Akademie der Wissenschaften zu Munchen Classe der Mathematik und Naturwissenschaften 1816; 6: 37 - 58.
  • Wilkinson LE, Young MT, Benton MJ. A new metriorhynchid crocodilian (Mesoeucrocodylia: Thalattosuchia) from the Kimmeridgian (Upper Jurassic) of Wiltshire, UK. Palaeontology 2008; 51: 1307 - 33. https: // doi. org / 10.1111 / j. 1475 - 4983.2008.00818. x
  • Plieninger T. Uber ein neues Sauriergenus und die Einreihung der Saurier mit flachen, schneidenden Zahnen in eine Familie. Pp. 148 - 154 in Zweite Generalversammlung am 1. Mai 1846 zu Tubingen. Wurttembergische naturwissenschaftliche Jahreshefte 1846; 2: 129 - 83.
  • Foffa D, Young MT. The cranial osteology of Tyrannoneustes lythrodectikos (Crocodylomorpha: Metriorhynchidae) from the Middle Jurassic of Europe. PeerJ 2014; 2: e 608. https: // doi. org / 10.7717 / peerj. 608