Published June 6, 2024 | Version v1
Taxonomic treatment Open

Grallator olonensis Lapparent & Montenat 1967

  • 1. Université Paris-Saclay, CNRS, GEOPS, 91405 Orsay (France) and Biogéosciences, UMR 6282 CNRS, Université Bourgogne, 6 boulevard Gabriel, 21000 Dijon (France)
  • 2. Univ Rennes, CNRS, Géosciences Rennes, UMR 6118, 263 avenue du Général Leclerc, F- 35000 Rennes (France)
  • 3. Biogéosciences, UMR 6282 CNRS, Université Bourgogne, 6 boulevard Gabriel, 21000 Dijon (France)
  • 4. Institut Polytechnique UniLaSalle Beauvais, Département Géosciences, Unité Bassins-Réservoirs-Ressources (B 2 R – U 2 R 7511), UniLaSalle-Université de Picardie Jules VERNE, 19 rue Pierre Waguet – boîte postale 30313, F- 60026 Beauvais cedex (France)
  • 5. Institut Polytechnique UniLaSalle Beauvais, Département Géosciences, Unité Bassins-Réservoirs-Ressources (B 2 R - U 2 R 7511), UniLaSalle-Université de Picardie Jules VERNE, 19 rue Pierre Waguet - boîte postale 30313, F- 60026 Beauvais cedex (France)

Description

Grallator olonensis Lapparent & Montenat, 1967

(Fig. 3)

Grallator olonensis Lapparent & Montenat, 1967: 14-16, pl. III.1- 2, fig. 6.

SYNTYPES. — ULB-04D19_A1 to ULB-04D19_A13. Lapparent & Montenat (1967) defined the “type” of G. olonensis as a surface bearing 25 footprints (surface “B1” in Lapparent & Montenat, 1967). A fragment of this surface is conserved in the Lapparent collection. It consists of the slab ULB-04D19_A (Fig. 3A, B) which bears thirteen tracks preserved as concave epireliefs. The slab ULB-04C12_A (“B1bis” in Lapparent & Montenat, 1967) corresponds to the convexe hyporeliefs of the slab ULB-04D19_A.

EXAMINED MATERIAL. — ULB-04C03_B, ULB-04C03_C, ULB-04C03_D, ULB-04C03_E, ULB-04C03_F, ULB-04C05_C, ULB-04C07_A, ULB-04C08_C, ULB-04C08_E, ULB-04C08_G, ULB-04C09_A, ULB-04C09_C, ULB-04C11_A, ULB-04C17_E, ULB-04C19_A, ULB-04D17_A, ULB-04D17_B, ULB-04D17_C, ULB-04D22_B.

DIAGNOSIS. —Tridactyl, very small-sized tracks (L = 3-5 cm), longer than wide and with a long projection of the trace of digit III (L/D = 2.1 in average). L/W ratio quite variable (1.2-2.5). Well-defined, very thin, elongated and often separated impressions of digits. Impression of digit III longer than traces of digits II and IV. Trace of digit III often curved distally. Traces of digits III and IV quite similar in length. Bases of digits II and IV proximally located at the same height. Variable but low divarication angle II-IV (35° in average). Tiny, oval and well-marked phalangeal pads. Tiny marks of acuminate claws.

DESCRIPTION

The material includes two trackways (T1-Go and T2-Go) preserved on the same slab and each composed of at least three consecutive footprints (ULB-04D19_A; Fig. 3A, B). The longest trackway (T1-Go) is 43.5 cm long. The stride is 34.0-(36.7)- 39.5 cm long and the pace is 15.1-(17.8)- 20.5 cm long. Tracks form a narrow angle with the trackway midline. The material also includes several partial trackways (ULB-04C19_A, ULB-04D17_A, ULB-04D19_A). The tracks are tridactyl, very small-sized, 3.3-(4.3)- 4.9 cm long and 1.5-(2.5)- 3.3 cm wide (Fig. 3 C-H; Table 2). Tracks are longer than wide and show a long projection of the traces of digit III. The L/W and L/D ratios are quite variable, being 1.2-(1.8)-2.5 and 1.8-(2.1)-2.4, respectively. Impressions of digits are well defined, very thin, elongated and often separated. The impression of digit III is longer than those of digits II and IV. The trace of digit III is often curved distally. The traces of digits II and IV are quite similar in length. Typically, the bases of digits II and IV are proximally located at the same height. The position of the digito-metatarsal pad of digit IV is rarely more proximal than that of digit II. The angle between digits II and IV is 24°-(34°)-44°. Phalangeal pads are tiny, oval and commonly well marked. Tracks commonly bear tiny marks of acuminate claws.

REMARKS

Based on material from Le Veillon, Lapparent & Montenat (1967) erected G. olonensis. Although they defined a type and describe the material, they did not erect a formal diagnosis. In France and throughout the world, G. olonensis was only reported from Le Veillon. Other very small-sized tridactyl tracks assigned to distinct ichnospecies of Grallator were described from Early Jurassic strata in Connecticut (Lull 1953): G. cursorius Hitchcock, 1858, G. gracilis Hitchcock, 1865 (synonym of G. tuberosus according to Weems 1992) and G. tenuis Hitchcock, 1858. G. cursorius differs from G. olonensis in showing more slender, longer tracks (type material with L = 7.0- 7.9 cm according to Weems 1992) and a base of IV much more proximal than II (Fig. 4). Although G. gracilis falls in the range size of G. olonensis, it differs from the latter in showing lower projection of III (type material with L/D = 2.6 according to Weems 1992; Fig. 4). G. tenuis differs from G. olonensis in showing longer tracks (type material with L = 6.4-6.6 cm according to Weems 1992) and the base of IV which is more proximal than II (Fig. 4). G. olonensis is strongly smaller than G. cuneatus Hitchcock, 1858, G. variabilis and G. formosus Hitchcock, 1858.

Notes

Published as part of Moreau, Jean-David, Vullo, Romain, Bichr, Elsie, Thomas, Jérôme, Gand, Georges, Gagnaison, Cyril, Barrier, Pascal & Néraudeau, Didier, 2024, Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection), pp. 343-366 in Geodiversitas 46 (8) on pages 347-349, DOI: 10.5252/geodiversitas2024v46a8, http://zenodo.org/record/11501840

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References

  • LAPPARENT A. F. DE & MONTENAT C. 1967. - Les empreintes de pas de reptiles de l'Infralias du Veillon (Vendee). Memoires de la Societe geologique de France 46: 1 - 43.
  • LULL R. S. 1953. - Triassic life of the Connecticut Valley. State Geological and Natural History Survey, Hartford, 331 p.
  • HITCHCOCK E. 1858. - Ichnology of New England: a Report on the Sandstone of the Connecticut Valley Especially its Fossil Footmarks, Made to the Government of the Commonwealth of Massachusetts. William White, Boston, 220 p.
  • WEEMS R. E. 1992. - A re-evaluation of the taxonomy of Newark Supergroup saurischian dinosaur tracks, using extensive statistical data from a recently exposed tracksite near Culpeper, Virginia, in Proceedings 26 th Forum on the Geology of Industrial Minerals. Virginia Division of Mineral Resources Publication 119: 113 - 127.