Dinosaur origins: Evidence from the footprint record

Triassic tracks and trackways assigned to dinosaur trackmakers or closest relatives have been mentioned from several Middle to the latest Triassic successions from both northern and southern Pangea. At present, the earliest gondwanan records are those from the Middle Triassic Los Rastros Formation i...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Marsicano, C.A., Domnanovich, N.S., Mancuso, A.C.
Formato: JOUR
Materias:
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_08912963_v19_n1_p83_Marsicano
Aporte de:
id todo:paper_08912963_v19_n1_p83_Marsicano
record_format dspace
spelling todo:paper_08912963_v19_n1_p83_Marsicano2023-10-03T15:41:18Z Dinosaur origins: Evidence from the footprint record Marsicano, C.A. Domnanovich, N.S. Mancuso, A.C. Argentina Dinosauria Footprints Los Rastros Formation Triassic dinosaur footprint fossil record ichnology trackway Triassic Argentina South America Dinosauria Ornithischia Saurischia Theropoda Triassic tracks and trackways assigned to dinosaur trackmakers or closest relatives have been mentioned from several Middle to the latest Triassic successions from both northern and southern Pangea. At present, the earliest gondwanan records are those from the Middle Triassic Los Rastros Formation in west-central Argentina. A reanalysis of Los Rastros ichnites at the Ischichuca area, including new material, has revealed the presence of a more diverse ichnofauna than previously suspected. The ichnocoenosis includes several tracks and trackways of bipeds with functionally tridactyl digitigrade pes, well developed claws, and a parasagittal posture of the hindlimbs. Previously, some large tridactyl footprints from the Ischichuca area were allied to theropod dinosaurs, although no synapomophies are preserved in the three-toed footprints that might discriminate among theropods, basal saurischians and basal ornithischian groups as their possible trackmakers. If the Ischichuca trackmakers are referred to a dinosaur taxon and/or to a close dinosaur sister-taxon, their presence in the Los Rastros levels suggests that derived dinosauriforms (including dinosaurs) had diverged and acquired their characteristic functionally tridactyl pes by at least the Middle Triassic, something that the body-fossil record has failed to document to date. Fil:Marsicano, C.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Domnanovich, N.S. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Mancuso, A.C. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_08912963_v19_n1_p83_Marsicano
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Argentina
Dinosauria
Footprints
Los Rastros Formation
Triassic
dinosaur
footprint
fossil record
ichnology
trackway
Triassic
Argentina
South America
Dinosauria
Ornithischia
Saurischia
Theropoda
spellingShingle Argentina
Dinosauria
Footprints
Los Rastros Formation
Triassic
dinosaur
footprint
fossil record
ichnology
trackway
Triassic
Argentina
South America
Dinosauria
Ornithischia
Saurischia
Theropoda
Marsicano, C.A.
Domnanovich, N.S.
Mancuso, A.C.
Dinosaur origins: Evidence from the footprint record
topic_facet Argentina
Dinosauria
Footprints
Los Rastros Formation
Triassic
dinosaur
footprint
fossil record
ichnology
trackway
Triassic
Argentina
South America
Dinosauria
Ornithischia
Saurischia
Theropoda
description Triassic tracks and trackways assigned to dinosaur trackmakers or closest relatives have been mentioned from several Middle to the latest Triassic successions from both northern and southern Pangea. At present, the earliest gondwanan records are those from the Middle Triassic Los Rastros Formation in west-central Argentina. A reanalysis of Los Rastros ichnites at the Ischichuca area, including new material, has revealed the presence of a more diverse ichnofauna than previously suspected. The ichnocoenosis includes several tracks and trackways of bipeds with functionally tridactyl digitigrade pes, well developed claws, and a parasagittal posture of the hindlimbs. Previously, some large tridactyl footprints from the Ischichuca area were allied to theropod dinosaurs, although no synapomophies are preserved in the three-toed footprints that might discriminate among theropods, basal saurischians and basal ornithischian groups as their possible trackmakers. If the Ischichuca trackmakers are referred to a dinosaur taxon and/or to a close dinosaur sister-taxon, their presence in the Los Rastros levels suggests that derived dinosauriforms (including dinosaurs) had diverged and acquired their characteristic functionally tridactyl pes by at least the Middle Triassic, something that the body-fossil record has failed to document to date.
format JOUR
author Marsicano, C.A.
Domnanovich, N.S.
Mancuso, A.C.
author_facet Marsicano, C.A.
Domnanovich, N.S.
Mancuso, A.C.
author_sort Marsicano, C.A.
title Dinosaur origins: Evidence from the footprint record
title_short Dinosaur origins: Evidence from the footprint record
title_full Dinosaur origins: Evidence from the footprint record
title_fullStr Dinosaur origins: Evidence from the footprint record
title_full_unstemmed Dinosaur origins: Evidence from the footprint record
title_sort dinosaur origins: evidence from the footprint record
url http://hdl.handle.net/20.500.12110/paper_08912963_v19_n1_p83_Marsicano
work_keys_str_mv AT marsicanoca dinosauroriginsevidencefromthefootprintrecord
AT domnanovichns dinosauroriginsevidencefromthefootprintrecord
AT mancusoac dinosauroriginsevidencefromthefootprintrecord
_version_ 1807323182298824704