Isisaurus

From Wikipedia, the free encyclopedia

Isisaurus
Temporal range: Late Cretaceous, 70 Ma
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Isisaurus DB.jpg
Scientific classification edit
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Saurischia
Clade: Sauropodomorpha
Clade: Sauropoda
Clade: Macronaria
Clade: Titanosauria
Clade: Lithostrotia
Family: Saltasauridae
Genus: Isisaurus
Wilson & Upchurch, 2003
Species:
I. colberti
Binomial name
Isisaurus colberti
(Jain & Bandyopadhyay, 1997)
Synonyms
  • Titanosaurus colberti
    Jain & Bandyopadhyay, 1997

Isisaurus (named after the Indian Statistical Institute[1]) is a genus of titanosaurian dinosaur from the Late Cretaceous period from what is now India.

Discovery and Naming[]

The type specimen of Isisaurus colberti, ISI R 335/1-65, was originally described and named as Titanosaurus colberti by Sohan Lal Jain and Saswati Bandyopadhyay in 1997, the specific name honouring Edwin Harris Colbert,[2][3] but was placed in its own genus, by Wilson and Upchurch, in 2003.[4] It had a short, vertically directed neck and long forelimbs,[citation needed] making it considerably different from other sauropods. The humerus is 148 centimetres long.[2] Based on this specimen, Isisaurus would have grown to about 18 metres (59 ft) in length and weighed about 14,000 kilograms (14 long tons; 15 short tons).[citation needed]

Isisaurus is known from much better remains than most titanosaurs. Most of its postcranial skeleton is known. The skeletal material Jain and Bandyopadhyay found between 1984 and 1986 was "in associated and mostly articulated condition;" it included cervical, dorsal, sacral and caudal vertebrae, ribs, pelvis, scapula, coracoid, left forelimb and other bones, though skull, hindlimb and foot bones were missing.[2] The site locality is Dongargaon Hill, which is in a Maastrichtian crevasse splay claystone in the Lameta Formation of India.[3] Dongargaon Hill (20.212318N,79.090709E) is located near Warora, in Chandrapur District, Maharashtra.

Description[]

There are two types of sauropod skulls from the Maastrichtian of India, the first type is from Jainosaurus and the other is from Isisaurus. While Jainosaurus had a broad and flat cranium, the skull of Isisaurus was robust and compact. Additionally, the angle between the occipital bone and occipital condyle is different in the two taxa. In the specimen from Dongargaon it is equal to 120°. The cranium of Isisaurus resembles in that matter the skulls of Diplodocus and Apatosaurus (genera belonging to the Diplodocidae), but the bone modifications are different.[5]

Palaeobiology[]

Fungus in coprolites believed to have been voided by Isisaurus indicate that it ate leaves from several species of tree, since these fungi are known to be pathogens which infect tree leaves.[6]

Paleoecology[]

Isisaurus lived in the area belonging nowadays to India[7] during the Maastrichtian (which is the uppermost stage of Late Cretaceous epoch).[8] Its remains are the most complete among the Cretaceous dinosaurs known from that region.[9] Khosla et al. (2003) listed the following Indian sauropods:[10]

Wilson et al. (2009) listed only two Indian titanosaurs, Isisaurus and its distant relative, Jainosaurus. Isisaurus and Jainosaurus lived sympatrically in the area of nowadays middle and western India, Isisaurus being also present in the area of western Pakistan.[5]

References[]

  1. ^ "The 10 Ugliest Dinosaurs". about.com. Retrieved November 15, 2013.
  2. ^ Jump up to: a b c Jain, Sohan L.; Bandyopadhyay, Saswati (1997). "New Titanosaurid (Dinosauria: Sauropoda) from the Late Cretaceous of Central India". Journal of Vertebrate Paleontology. Norman, Okla.: University of Oklahoma. 17 (1): 114. doi:10.1080/02724634.1997.10010958.
  3. ^ Jump up to: a b "Isisaurus colberti". Paleobiology Database. Retrieved December 31, 2012.
  4. ^ Wilson, Jeffrey A.; Upchurch, P. (2003). "A revision of Titanosaurus Lydekker (Dinosauria – Sauropoda), the first dinosaur genus with a 'Gondwanan' distribution" (PDF). Journal of Systematic Palaeontology. Cambridge, U.K.: Cambridge University Press. 1 (3): 125–160. doi:10.1017/s1477201903001044. Retrieved December 31, 2012.
  5. ^ Jump up to: a b Jeffrey A. Wilson, Michael D. D'emic, Kristina A. Curry Rogers, Dhananjay M. Mohabey & Subashis Sen (2009). "A reassessment of the sauropod dinosaur Jainosaurus (="Antarctosaurus") septentrionalis from the Upper Cretaceous of India". Contributions from the Museum of Paleontology, University of Michigan. 32 (2): 17–40. Retrieved 2 September 2018.CS1 maint: multiple names: authors list (link)
  6. ^ Sharma, N., Kar, R.K., Agarwal, A. and Kar, R. (2005). "Fungi in dinosaurian (Isisaurus) coprolites from the Lameta Formation (Maastrichtian) and its reflection on food habit and environment." Micropaleontology, 51(1): 73-82.
  7. ^ Wilson, J. A. (2006). "An Overview of Titanosaur Evolution and Phylogeny" (PDF). Actas de las III Jornadas Internacionales Sobre Paleontología de Dinosaurios y Su Entorno, Salas de los Infantes, Burgos. Retrieved 2 September 2018.
  8. ^ González Riga, Bernardo J. (2005). "Nuevos restos fósiles de Mendozasaurus neguyelap (Sauropoda, Titanosauria) del Cretácico Tardío de Mendoza, Argentina". Ameghiniana. 42.
  9. ^ Jeffrey A. Wilson, Paul C. Sereno, Suresh Srivastava, Devendra K. Bhatt (2003-08-15). "A New Abelisaurid (Dinosauria, Theropoda) Grom The Lameta" (PDF). Contributions from the Museum of Paleontology. The University of Michigan. 31 (1): 1–42. Retrieved 2 September 2018.CS1 maint: multiple names: authors list (link)
  10. ^ Khosla, A., V. V. Kapur, P. C. Sereno, J. A. Wilson, G. P. Wilson, D. Dutheil, A. Sahni, M. P. Singh, S. Kumar (2003). "First dinosaur remains from the Cenomanian-Turonian Nimar Sandstone (Bagh Beds), district Dhar, Madhya Pradesh, India" (PDF). Journal of the Palaeontogical Society of India. 48: 115–127. Retrieved 2 September 2018.CS1 maint: multiple names: authors list (link)
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