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Temporal range: Late Triassic
~236–234 Ma
Lagerpeton NT small.jpg
Scientific classification e
Kingdom: Animalia
Phylum: Chordata
Family: Lagerpetidae
Genus: Lagerpeton
Romer 1971
Type species
Lagerpeton chanarensis

Lagerpeton is a genus of basal dinosauromorph. First described by A. S. Romer in 1971,[1] it includes only the species L. chanarensis.[2] This species is incompletely known, with fossil specimens accounting for the pelvic girdle, hindlimbs and posterior presacral, sacral and anterior caudal vertebrae.


Lagerpeton fossils have only been collected from the Chañares Formation in La Rioja Province, Argentina. The first of these fossils were discovered in a 1964-1965 expedition by the Museum of Comparative Zoology (MCZ) and Museo de la Plata (MLP), although some were also discovered in 1966 by paleontologists from the Miguel Lillo Institute (PVL) of the University of Tucuman.[1][3][4]

Alfred Romer named Lagerpeton chanarensis in 1971, based on a complete right hindlimb discovered during the MCZ-MLP expedition. The specimen was initially stored at the Museo de la Plata with catalogue number MLP 64-XI-14-10, but by 1986 it had been transferred to the Paleontology Museum at the National University of La Rioja (PULR) and given the designation PULR 06,[4][5] though some studies alternatively call it UPLR 06[2] or UNLR 06.[6] Some of the foot bones from this specimen have gone missing.[2] Romer also mentioned PVL material collected by Jose Bonaparte.[1]

In 1972, Romer described MCZ 4121, which was a specimen smaller than the holotype. It was preserved in a nodule alongside the holotype of Lewisuchus admixtus and a few Lagosuchus bones. MCZ 4121 represents a few vertebrae, a pair of scapulocoracoids (mislabeled as belonging to Lagosuchus) and portions of the hip and hindlimbs, including two complete femurs. He also suggested that Lagerpeton was the probable identity of several incomplete tibiae and fibulae preserved along with several gomphodont skeletons in slab MCZ 3691.[3] However, later authors have doubted the referral of most MCZ material to Lagerpeton, with only the MCZ 4121 femurs being confidently referred to the genus.[2][6]

Andrea Arcucci described two PVL specimens, PVL 4619 and 4625, in 1986. PVL 4619, the PVL specimen mentioned by Romer, was a partial skeleton including a complete pelvis and left hindlimb, as well as a partial right hindlimb. PVL 4625 was another skeleton discovered later, which included portions of the left hip, left hindlimb, and vertebral column.[4] Paul Sereno and Arcucci redescribed the known material in 1994 and mentioned that an isolated partial femur of this species was also present at the PVL,[2] although Martin Ezcurra (2016) noted that the provided catalogue number, PVL 5000, actually referred to a notoungulate mammal.[5]


Lagerpeton is estimated to have been 70 cm (28 in) in length based on the length of the hindlimb;[7] the most complete hindlimb specimen, from PVL 4619, measures 257.9mm from proximal femur to distal ungual.[2] Body mass has been estimated as no more than 4 kilograms (8.8 lb), based on the slender cross section of limb bones and estimates between more derived dinosauromorphs, such as Silesaurus, and basal saurischians like Eoraptor.[8] Twenty one autapomorphic characters have been identified in L. chanarensis, these include: the anterior inclination of the posterior dorsal neural spines, the hook-shaped femoral head and the length of digit IV and metatarsal IV being greater than digit III and metatarsal III.[2] L. chanarensis lacks many dinosaurian characters, such as the anterior trochanter, placing it basal within Dinosauromorpha.[7]


Early to late Olenekian trackways from Poland have yielded footprints of a Lagerpeton-like quadrupedal dinosauromorph.[9] This ichnogenus, named Prorotodactylus shares multiple synapomorphic characters with Lagerpeton including approximately parallel digits II, III and IV, fused metatarsus, digitigrade posture and reduced digits I and V. Prorotodactylus also shares the, previously autapomorphic, pes morphology of Lagerpeton. If this ichnogenus represents a close relative of Lagerpeton, it would push back the origin of this taxon to the Early Triassic; as a quadrupedal basal dinosauromorph, it also raises questions debating the theory that bipedalism is ancestral to dinosaurs.[9]

The genus Lagerpeton is currently accepted as the most basal clade within Dinosauromorpha and the sister taxon to Dinosauriformes.[7] Presently, Lagerpeton sits within the family “Lagerpetidae”, also occupied by the more derived genus Dromomeron, known from Late Triassic rocks of the southwestern USA.[7][6][10]

Cladogram simplified after Kammerer, Nesbitt & Shubin (2012):[11]




Lagerpeton chanarensis

Dromomeron gregorii

Dromomeron romeri




The oldest fossils of L. chanarensis were found in the Chañares Formation and originate from the Upper Middle Triassic (Ladinian) of Gondwana, southern Pangaea. All Lagerpeton specimens share this geographic location, including other fossils from the Lower Late Triassic (Carnian).[12] Radiometric dating of volcanic material in the formation has narrowed the formation and entire fossil assemblage found there to between 236 and 234 million years old.[13]


It has been suggested that the extant analogues most similar to L. chanarensis are small bipedal mammals, which are often saltators. Three morphological characteristics in L. chanarensis fossils have been putatively cited as evidence of saltation in this taxon.[2]

Neural spines[edit]

The neural spines of the posterior dorsal vertebrae are inclined anteriorly, a character not observed in any other archosaur, but common in saltatory mammals. This feature is suggested to allow for greater vertebral flexibility, correlated with leaping and bounding locomotor styles.

Pelvic girdle[edit]

Relative to the hindlimb length, the pelvic girdle is remarkably small. The distance from the pelvic girdle to the femur is therefore also small, more so than most other archosaurs apart from closely related taxa. This reduction in distance may increase the force production during hip extension in extant small mammals.

Didactyl foot[edit]

The narrow and functionally didactyl pes are a further similarity to modern saltators. By condensing into a single unit, the metatarsus gains strength without the drawback of increased weight. It also appears likely that, consequently to the reduction of digit II, digit IV may have elongated to balance the pes.

The hypothesis of saltatorial locomotion is debated, however.[8] Vertebral adaptations of extant organisms exceed those seen in Lagerpeton; the sacral vertebrae of modern saltators are fused and the neural spines reduced. Furthermore, the size of the pelvic girdle and lateral digital reduction may be equally used as evidence for cursorial locomotion.


  1. ^ a b c Romer, A. S. (1971). "The Chanares (Argentina) Triassic reptile fauna. X. Two new but incompletely known long-limbed pseudosuchians". Breviora. 378: 1–10.
  2. ^ a b c d e f g h Sereno, P. C.; Arcucci, A. B. (1994). "Dinosaurian precursors from the Middle Triassic of Argentina: Lagerpeton chanarensis". Journal of Vertebrate Paleontology. 13 (4): 385–399. doi:10.1080/02724634.1994.10011522. JSTOR 4523529.
  3. ^ a b Romer, Alfred Sherwood (11 August 1972). "The Chañares (Argentina) Triassic reptile fauna. XV. Further remains of the thecodonts Lagerpeton and Lagosuchus". Breviora. 394: 1–7.
  4. ^ a b c Arcucci, Andrea (1986). "New materials and reinterpretation of Lagerpeton chanarensis Romer (Thecodontia, Lagerpetonidae nov.) from the Middle Triassic of La Rioja, Argentina" (PDF). Ameghiniana. 23 (3–4): 233–242.
  5. ^ a b Ezcurra, Martín D. (2016-04-28). "The phylogenetic relationships of basal archosauromorphs, with an emphasis on the systematics of proterosuchian archosauriforms". PeerJ. 4: e1778. doi:10.7717/peerj.1778. ISSN 2167-8359. PMC 4860341. PMID 27162705.
  6. ^ a b c Nesbitt, S.J. (2011). "The Early Evolution of Archosaurs: Relationships and the Origin of Major Clades" (PDF). Bulletin of the American Museum of Natural History. 352: 189. doi:10.1206/352.1. hdl:2246/6112. ISSN 0003-0090.
  7. ^ a b c d Nesbitt, S. J.; Irmis, R. B.; Parker, W. G.; Smith, N. D.; Turner, A. H.; Rowe, T. (2009). "Hindlimb osteology and distribution of basal dinosauromorphs from the Late Triassic of North America" (PDF). Journal of Vertebrate Paleontology. 29 (2): 498–516. doi:10.1671/039.029.0218.
  8. ^ a b Fechner, R. (2009). Morphofunctional evolution of the pelvic girdle and hindlimb of Dinosauromorpha on the lineage to Sauropoda (Thesis). Ludwigs Maximilians Universitä.
  9. ^ a b Brusatte, S. L.; Niedźwiedzki, G.; Butler, R. J. (2011). "Footprints pull origin and diversification of dinosaur stem lineage deep into Early Triassic". Proceedings of the Royal Society B: Biological Sciences. 278 (1708): 1107–1113. doi:10.1098/rspb.2010.1746. PMC 3049033. PMID 20926435.
  10. ^ Baron, M.G., Norman, D.B., and Barrett, P.M. (2017). A new hypothesis of dinosaur relationships and early dinosaur evolution. Nature, 543: 501–506. doi:10.1038/nature21700
  11. ^ Kammerer, C. F.; Nesbitt, S. J.; Shubin, N. H. (2012). "The First Silesaurid Dinosauriform from the Late Triassic of Morocco" (PDF). Acta Palaeontologica Polonica. 57 (2): 277. doi:10.4202/app.2011.0015.
  12. ^ Langer, M. C.; Nesbitt, S. J.; Bittencourt, J. S.; Irmis, R. B. (2013). "Non-dinosaurian Dinosauromorpha". Geological Society, London, Special Publications. 379 (1): 157–186. Bibcode:2013GSLSP.379..157L. doi:10.1144/sp379.9.
  13. ^ Claudia A. Marsicano; Randall B. Irmis; Adriana C. Mancuso; Roland Mundil; Farid Chemale (2016). "The precise temporal calibration of dinosaur origins". Proceedings of the National Academy of Sciences of the United States of America. 113 (3): 509–513. Bibcode:2016PNAS..113..509M. doi:10.1073/pnas.1512541112. PMC 4725541. PMID 26644579.