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Euronecturus grogu

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GrafMauz/sandbox
Temporal range: Miocene
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Amphibia
Order: Urodela
Suborder: Salamandroidea
Family: Proteidae
Genus:
Euronecturus
Species:
Euronecturus grogu
Binomial name
Euronecturus grogu
Macaluso, 2022


Euronecturus grogu is an extinct type species of the genus Euronecturus (Proteidae) from in Hambach, Germany. It appeared in the early middle Miocene (late Orleanian, MN 5) in Europe.

E. grogu is additionally an important finding, because of its high phylogenetic similarity to the oldest known prodeid fossil Paranecturus garbanii (Maastrichian, late Cretaceous), whereas it has low phylogenetic similarity to other European proteids (Mioproteus and Proteus). This allows the assumption, two different lineages of Proteidae would have inhabited Europe during the Cenozoic.

Discovery and Naming

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Euronecturus grogu was discovered in the Hambach 6C main seam, of a lignite mine in Hambach, Germany (50° 540 44″ N, 6° 290 51″ E; Fig. 1), that exposes the miocenic Ville Formation. The genus is part of the Hambach 6C fauna (middle Miocene (late Orleanian, MN 5).

Its genus name (Euronecturus) is assembled of Euro (reference to its appearance in Europe) and necturus (reference to its similarity and suggested phylogenetic affinity to Paranecturus and Necturus).

The specific epithet of its Type species “Euronecturus grogu” referes to a character of the popular Star Wars series “The Mandalorian” called Grogu.

One of its distinctive morphological features (secondary dorsal crest, further described below), is usually rarely preserved.

Description

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E. grogu was described, based on five atlases from several individuals. These are the only fossil remainings in Hambach 6C, that can undoubtedly attributed to Euronecturus. Some distinctive morphological features justify to define a new genus and species:

  • Its secondary dorsal crest differs from all known proteids, however this feature is very rarely preserved.
  • small posteriorly-directed postzygapophyses
  • wide and deep ventral fossa between the anterior cotyles

It allows furthermore exceptional resemblance with an North American relative, Paranecturus garbanii, based on the similar morphology of the atlas.

The phylogenetic relationship of E. grogu is based on the work of Macaluso et al., 2022.[1]

Cryptobranchus alleganiensis

Hambach 6C of the Ville Formation contains sediments typical for an estuarine environment: a large river system, surrounded by extended coal swamps [2]. This is also covered by paleontological evidence:

The climatological setting of Hambach 6C was subtropical:

Cultural Significance

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Significance of E. grogu for paleontology

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E. grogu shows high phylogenetic similarity to the oldest known proteid fossil Paranecturus garbanii from Northern America (Maastrichian, late Cretaceous) [1]. This is outstanding, regarding the time difference between the occurrence of both species, and the low phylogenetic similarity of E. grogu to other European proteids (Mioproteus and Proteus). This allows the assumption, two different lineages of Proteidae would have inhabited Europe during the Cenozoic.

The authors who described E. grogu hypotise, its ancestors could have colonised Europe via the De Geer or Thulean route (via Greenland to west Eurasia, Fennoscandia or Great Britain) in stead of Beringia. The other hypothesis is, E. grogu could be a relic from times, when Northern America and Europe shared similar faunal elements.

References

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  1. ^ a b Macaluso, Loredana; Villa, Andrea; Mörs, Thomas (2022-01). Mannion, Philip (ed.). "A new proteid salamander (Urodela, Proteidae) from the middle Miocene of Hambach (Germany) and implications for the evolution of the family". Palaeontology. 65 (1). doi:10.1111/pala.12585. ISSN 0031-0239. {{cite journal}}: Check date values in: |date= (help)
  2. ^ Mörs, Th. (2002-08). "Biostratigraphy and paleoecology of continental Tertiary vertebrate faunas in the Lower Rhine Embayment (NW-Germany)". Netherlands Journal of Geosciences - Geologie en Mijnbouw. 81 (2): 177–183. doi:10.1017/S0016774600022411. ISSN 0016-7746. {{cite journal}}: Check date values in: |date= (help)
  3. ^ Hierholzer, E. "Cypriniden-Schlundzähne (Osteichthyes: Teleostei) aus dem Tertiär von Hambach (Niederrheinische Bucht, NW-Deutschland)". Palaeontographica. 269: 1–38.
  4. ^ a b Klein, Nicole; Mörs, Thomas (2003-03-19). "Turtles (Reptilia: Testudines) from the middle Miocene of Hambach (Lower Rhine Embayment, NW Germany)". Palaeontographica Abteilung A. 268 (1–3): 1–48. doi:10.1127/pala/268/2003/1. ISSN 0375-0442.
  5. ^ Stefen, Clara; Mörs, Thomas (2008-09). "The beaver Anchitheriomys from the Miocene of central Europe". Journal of Paleontology. 82 (5): 1009–1020. doi:10.1666/06-049.1. ISSN 0022-3360. {{cite journal}}: Check date values in: |date= (help)
  6. ^ Steinthorsdottir, M.; Coxall, H. K.; de Boer, A. M.; Huber, M.; Barbolini, N.; Bradshaw, C. D.; Burls, N. J.; Feakins, S. J.; Gasson, E.; Henderiks, J.; Holbourn, A. E.; Kiel, S.; Kohn, M. J.; Knorr, G.; Kürschner, W. M. (2021-04). "The Miocene: The Future of the Past". Paleoceanography and Paleoclimatology. 36 (4). doi:10.1029/2020PA004037. ISSN 2572-4517. {{cite journal}}: Check date values in: |date= (help)
  7. ^ a b Utescher, T. "Terrestrial climate evolution in northwest Germany over the last 25 million years". Palaios.