TY - JOUR
T1 - New dinosaur species from the Upper Triassic Upper Maleri and Lower Dharmaram formations of Central India
AU - Novas, Fernando E.
AU - Ezcurra, Martin D.
AU - Chatterjee, Sankar
AU - Kutty, T. S.
N1 - Funding Information:
We thank several people who allowed us to study specimens under their care: S. Bandyopadhyay (ISI), M. Langer (USP), C. Malabarba (PUC), J. Ferigolo (FZB), R. Martinez (UNSJ), E. Vaccari (PULR), A. Kramarz (MACN), D. Pol (MEF), J. Powell (PVL), M. Reguero (MLP), K. Padian, P. Holroyd (UCMP) and R. Irmis (UMNH). This research was partially funded by CONICET (to FEN), the Agencia Nacional de Promoción Científica y Técnica (to FEN), the Samuel Welles Fund Grant of the UCMP (to MDE) and The Jurassic Fundation (to MDE). Copies of papers sent by Peter Galton were very useful and appreciated. The comments and suggestions of Randall Irmis (UMNH), Max Langer (USP), Richard Butler (BSPG) and an anonymous reviewer improved the overall quality of the manuscript. M. Ezcurra thanks the Society of Vertebrate Paleontology for the Jackson School of Geosciences Student Member Travel Grant and F. Novas acknowledges the Systematics Association for partial support, respectively, for our participation in the symposium on Late Triassic Terrestrial Biotas and The Rise of Dinosaurs at the 69th SVP meeting.
PY - 2010/9
Y1 - 2010/9
N2 - The beginning of dinosaur evolution is currently known based on a handful of highly informative Gondwanan outcrops of Ischigualastian age (late Carnian-early Norian). The richest Triassic dinosaur records of the southern continents are those of South America and South Africa, with taxonomically diverse faunas, whereas faunas from India and central Africa are more poorly known. Here, the known diversity of Gondwanan Triassic dinosaurs is increased with new specimens from central India, which allow a more comprehensive characterisation of these dinosaur assemblages. Five dinosauriform specimens are reported from the probable late Norian-earliest Rhaetian Upper Maleri Formation, including two new sauropodomorph species, the nonplateosaurian Nambalia roychowdhurii and the plateosaurian Jaklapallisaurus asymmetrica, a guaibasaurid and two basal dinosauriforms. The Lower Dharmaram Formation, probably latest Norian-Rhaetian in age, includes basal sauropodomorph and neotheropod remains, providing the second record of a Triassic Gondwanan neotheropod. The currently available evidence suggests that the oldest known Gondwanan dinosaur assemblages (Ischigualastian) were not homogeneous, but more diverse in South America than in India. In addition, the Upper Maleri and Lower Dharmaram dinosaur assemblages resemble purported coeval South American and European beds in the presence of basal sauropodomorphs. Accordingly, the current available evidence of the Triassic beds of the Pranhita-Godavari Basin suggests that dinosaurs increased in diversity and abundance during the late Norian to Rhaetian in this region of Gondwana.
AB - The beginning of dinosaur evolution is currently known based on a handful of highly informative Gondwanan outcrops of Ischigualastian age (late Carnian-early Norian). The richest Triassic dinosaur records of the southern continents are those of South America and South Africa, with taxonomically diverse faunas, whereas faunas from India and central Africa are more poorly known. Here, the known diversity of Gondwanan Triassic dinosaurs is increased with new specimens from central India, which allow a more comprehensive characterisation of these dinosaur assemblages. Five dinosauriform specimens are reported from the probable late Norian-earliest Rhaetian Upper Maleri Formation, including two new sauropodomorph species, the nonplateosaurian Nambalia roychowdhurii and the plateosaurian Jaklapallisaurus asymmetrica, a guaibasaurid and two basal dinosauriforms. The Lower Dharmaram Formation, probably latest Norian-Rhaetian in age, includes basal sauropodomorph and neotheropod remains, providing the second record of a Triassic Gondwanan neotheropod. The currently available evidence suggests that the oldest known Gondwanan dinosaur assemblages (Ischigualastian) were not homogeneous, but more diverse in South America than in India. In addition, the Upper Maleri and Lower Dharmaram dinosaur assemblages resemble purported coeval South American and European beds in the presence of basal sauropodomorphs. Accordingly, the current available evidence of the Triassic beds of the Pranhita-Godavari Basin suggests that dinosaurs increased in diversity and abundance during the late Norian to Rhaetian in this region of Gondwana.
KW - Archosauria
KW - Gondwana
KW - Sauropodomorpha
KW - macroevolution
KW - phylogeny
UR - http://www.scopus.com/inward/record.url?scp=79959461114&partnerID=8YFLogxK
U2 - 10.1017/S1755691011020093
DO - 10.1017/S1755691011020093
M3 - Article
AN - SCOPUS:79959461114
SN - 1755-6910
VL - 101
SP - 333
EP - 349
JO - Earth and Environmental Science Transactions of the Royal Society of Edinburgh
JF - Earth and Environmental Science Transactions of the Royal Society of Edinburgh
IS - 3-4
ER -