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Isisaurus

Isisaurus is a genus of titanosaurian sauropod dinosaur that lived during the Maastrichtian stage of the Late Cretaceous Period, approximately 71–66 million years ago, in what is now central India.^[1] The type and only known species is Isisaurus colberti, a medium-sized herbivore known from a partial skeleton including presacral vertebrae, scapulae, humeri, and other postcranial elements, with a referred braincase, discovered in the Lameta Formation.^[2] Based on these remains, particularly a humerus measuring 1.48 meters in length, Isisaurus is estimated to have reached about 18 meters in overall length.^[2] Originally described as Titanosaurus colberti in 1997 by Sohan Lal Jain and Saswati Bandyopadhyay based on material from the Indian Statistical Institute collections, the genus was formally renamed Isisaurus in 2003 by Jeffrey A. Wilson and Paul Upchurch to reflect its distinctiveness from the type species of Titanosaurus.^[2] The holotype specimen (ISI R 335/1–65) consists of an articulated series of 11 middle to posterior dorsal vertebrae, a partial sacrum, caudal vertebrae, chevrons, ribs, a sternal plate, scapulae, a left humerus, partial radius and ulna, and manual elements, providing one of the more complete titanosaur skeletons from the Indian subcontinent.^[2] Additional referred material, including a braincase from Dongargaon and limb bones from other Lameta localities, supports the recognition of Isisaurus as a valid taxon separate from the contemporaneous Indian titanosaur Jainosaurus.^[2] Taxonomically, Isisaurus belongs to the clade Titanosauria within Sauropoda, specifically within the derived subgroup Lithostrotia, based on features such as procoelous caudal vertebrae and robust limb proportions.^[1] It is distinguished from other titanosaurs by autapomorphies including anteroposteriorly elongate cervical parapophyses and a short, vertically oriented neck with cervical centra only about twice as long as tall—unusually compact for a sauropod, potentially indicating a browsing rather than high-reaching feeding strategy.^[3] The scapula is notably robust (1.08 meters long) with a broad acromion process, and the humerus features a proximally placed deltopectoral crest and narrower proximal end compared to related taxa like Jainosaurus.^[2] Fossil evidence associates Isisaurus with the Lameta Formation's floodplain environments, where titanosaur eggshells (Megaloolithus species) and coprolites containing plant fragments and fungal spores suggest a herbivorous diet supplemented by ingested fungi, reflecting adaptation to a seasonal, monsoon-influenced habitat.^[4] Clumped isotope analysis of associated eggshells indicates body temperatures averaging around 37°C, consistent with variable thermoregulation in large titanosaurs.^[4] Isisaurus represents part of the diverse Late Cretaceous sauropod fauna of Gondwana, sharing biogeographic ties with South American titanosaurs like Antarctosaurus while highlighting India's isolation before the end-Cretaceous extinction.^[2]

Discovery and Naming

Etymology

The genus name Isisaurus is derived from "ISI," an abbreviation for the Indian Statistical Institute in Kolkata, where the type specimens are housed and where much of the initial research on the fossils was conducted, combined with the Ancient Greek word sauros (σαῦρος), meaning "lizard" or "reptile." The specific epithet colberti honors Edwin Harris Colbert (1905–2001), an influential American paleontologist renowned for his extensive work on vertebrate fossils, including major contributions to dinosaur systematics and popularization of the field through books and museum exhibits.^[5] The taxon was first named Titanosaurus colberti by Sohan Lal Jain and Saswati Bandyopadhyay in 1997, based on material from the Late Cretaceous Lameta Formation in central India.^[5] However, in a comprehensive revision, Jeffrey A. Wilson and Paul Upchurch transferred it to the new genus Isisaurus colberti in 2003, recognizing that Titanosaurus Lydekker, 1877, was inadequately diagnosed, polyphyletic, and effectively a nomen dubium, rendering its species assignments untenable.^[6]

Type Specimen and Additional Material

The type specimen of Isisaurus, designated ISI R 335/1-65, consists of a partial postcranial skeleton representing a single individual, including 11 dorsal vertebrae, 5 caudal vertebrae, chevrons, ribs, a scapula, coracoid, humerus, radius, ulna, carpals, metacarpals, ilium, pubis, and ischium.^[5] This material was originally described and named as a new species of Titanosaurus, T. colberti, in 1997, and later reclassified into the new genus Isisaurus in 2003 based on its distinct titanosaurian features.^[6] The specimen was excavated during field seasons from 1984 to 1986 by the Geological Studies Unit of the Indian Statistical Institute.^[5] It derives from Dongargaon Hill in Jabalpur District, Madhya Pradesh, India, within the Lameta Formation, a Maastrichtian (~70–66 million years ago) unit characterized by alluvial and lacustrine deposits.^[5]^[7] Additional referred material includes a sauropod braincase (GSP-UM 4301) from the Maastrichtian Pab Formation in Balochistan, Pakistan, which shares endocranial features with Isisaurus and is tentatively assigned to the genus, extending its known geographic range.^[8] No cranial elements, hindlimb bones, or pedal remains are known for Isisaurus.

Description

Size and General Morphology

Isisaurus was a medium-sized titanosaurian sauropod, with body length estimates reaching approximately 18 meters (59 feet) and a mass of around 14 metric tons (15 short tons).^[9] These dimensions position it as intermediate in scale among titanosaurs, smaller than gigantic forms like Argentinosaurus (which exceeded 30 meters) but larger than diminutive taxa such as Saltasaurus (around 12 meters).^[9] The type specimen's postcranial elements, including a humerus measuring 1.48 meters in length, provide the basis for these reconstructions, indicating a quadrupedal herbivore with the characteristic sauropod body plan of a long neck, robust torso, pillar-like limbs, and extended tail.^[10] Distinctive among sauropods, Isisaurus exhibited a relatively short neck oriented vertically, differing from the more elongate, horizontally inclined necks typical of many diplodocids and basal macronarians.^[10] This feature is evident in its cervical vertebrae, which are notably compact anteroposteriorly, with centra lengths only about twice their height—a proportion shorter than in most other sauropods.^[10] In contrast to titanosaurs like Nemegtosaurus, which retained longer cervicals for extended reach, Isisaurus's neck morphology suggests adaptations potentially suited to a more upright posture for accessing mid-level vegetation.^[10] The overall build of Isisaurus emphasized stability and support, with forelimbs contributing to a more level-backed silhouette when in a quadrupedal stance.^[11] Compared to contemporaries like Jainosaurus, which had sturdier proportions, Isisaurus displayed more gracile limb configuration, particularly in the narrower proximal humerus and gracile ulna.^[2]

Osteology

The osteology of Isisaurus colberti is documented primarily from the holotype specimen (ISI R 335/1–65), a partial postcranial skeleton that preserves elements from multiple regions of the axial and appendicular skeleton, providing one of the more complete titanosaurian records from the Late Cretaceous of India. This material reveals a suite of features consistent with derived titanosaurs, including pneumaticity in certain bones and limb elements adapted for quadrupedal support. Many details are inferred from the partial remains or compared to related titanosaurs. The vertebral column includes cervical, dorsal, sacral, and caudal elements preserved in the holotype. The holotype preserves an articulated series of 11 middle to posterior dorsal vertebrae with amphicoelous centra, a condition typical of titanosaurs. Caudal vertebrae are procoelous, with well-developed chevron facets positioned ventrally on the centra to articulate with haemal arches, facilitating tail flexibility. Cervical ribs are short relative to the centra length, indicating a more compact neck structure compared to longer-necked sauropods. The pectoral girdle comprises a scapula featuring a distinct acromion process at the proximal end, which expands dorsally to form an expanded articulation surface for the coracoid; the scapula measures 1.08 meters in length and is notably robust. The forelimb includes a straight left humerus that lacks significant sigmoid curvature and measures 1.48 meters in length. The partial radius and ulna are subequal in length, with the ulna gracile and triradiate in midshaft cross-section, while the manus preserves partial elements consistent with five digits, the first three bearing ungual phalanges that end in sharp claws suitable for substrate interaction. The rib cage includes preserved dorsal ribs, some of which bear pneumatic foramina along their shafts, suggesting the presence of air sacs that extended into the postcranial skeleton for respiratory efficiency. Distinctive osteological traits of Isisaurus include the short cervical ribs, which contrast with the elongated ribs in more gracile sauropods, and the absence of osteoderms, differing from armored titanosaurs such as some saltasaurines. The humerus features a proximally placed deltopectoral crest and narrower proximal end compared to related taxa like Jainosaurus. These features collectively highlight adaptations for a wide-bodied build without dermal armor.

Classification

Phylogenetic Analyses

Initial phylogenetic analyses assigned the type material of Isisaurus to Titanosaurus colberti within Titanosauridae, based on fragmentary vertebrae and limb elements from the Lameta Formation that exhibited typical titanosaurian features such as procoelous caudal centra. This placement was revised in 2003, when the material was erected as the new genus Isisaurus colberti, still regarded as a primitive titanosaur outside more derived clades, supported by autapomorphic traits including a short, vertically oriented neck. Subsequent cladistic studies refined this position using expanded character matrices focused on titanosaurian morphology. Curry Rogers (2005) incorporated Isisaurus into a broad analysis of titanosaurs, recovering it within Opisthocoelicaudiinae, a group defined by opisthocoelous caudal vertebrae and moderate body size, with key supporting characters including the lamination of neural arches in dorsal vertebrae. Zaher et al. (2011) rescored cranial and postcranial data in a matrix of 35 titanosaur taxa and 145 characters, placing Isisaurus as the sister taxon to Saltasauridae within Lithostrotia; this topology was bolstered by shared states such as extensive pneumaticity invading the vertebral centra and neural arches. Carballido et al. (2017) extended this framework with a dataset of 68 sauropods and 304 characters, positioning Isisaurus within Lithostrotia, with pneumatic features in the posterior dorsal vertebrae providing critical synapomorphies. More recent analyses up to 2021 affirm Isisaurus as a lithostrotian titanosaur but highlight ongoing instability in its exact relationships, attributable to the incomplete holotype lacking skull and much of the axial skeleton. Rubilar-Rogers et al. (2021) analyzed 50 taxa with 228 characters, recovering Isisaurus as the sister to Arackar licanantay in a basal lithostrotian position, with neural arch lamination and vertebral pneumaticity again pivotal, though sensitivity analyses showed topological shifts when incomplete taxa were pruned. These evolving hypotheses underscore how character optimization in parsimony-based methods, particularly for pneumatic and appendicular traits, has shifted Isisaurus from basal to more derived titanosaur positions over time.

Systematic Placement

Isisaurus is classified in the kingdom Animalia, phylum Chordata, class Reptilia, clade Dinosauria, order Saurischia, suborder Sauropodomorpha, infraorder Sauropoda, clade Titanosauriformes, clade Titanosauria, and clade Lithostrotia. The genus contains a single valid species, I. colberti, with no recognized synonyms or additional species. Current consensus places Isisaurus colberti as a basal member of Lithostrotia or within Saltasauroidea, its closest relatives including Rapetosaurus krausei, Tapuiasaurus macedoi, and Arackar licanantay. Early proposals suggested potential synonymy of I. colberti with Jainosaurus septentrionalis due to shared Indian provenance, but this has been rejected based on vertebral differences, including centrum shape and the position of the neural arch relative to the centrum in dorsal vertebrae.

Paleobiology

Diet and Feeding Behavior

Isisaurus was a herbivorous sauropod, with its diet primarily consisting of leaves from trees, as inferred from the analysis of coprolites attributed to this dinosaur.^[12] These coprolites, recovered from the Maastrichtian Lameta Formation in India, contain fungal elements comprising approximately 10% of the organic content, including hyphae, spores, and ascostromata of plant pathogens such as Colletotrichum (causing leaf spot and red rot), Erysiphe and Uncinula (powdery mildews), and microthyriaceous forms (black spot fungi).^[12] The presence of these epiphyllous fungi indicates that Isisaurus consumed foliage infected by these pathogens, likely from a mix of conifers and angiosperms, as the fungi affect a broad range of plant types.^[12] Additionally, mycorrhizal fungi like Glomus were identified, though these are interpreted as post-depositional contaminants rather than dietary components.^[12] The high fungal content in the coprolites suggests that Isisaurus fed on tough, fibrous plant matter, with the partially digested remains pointing to a reliance on microbial breakdown in the gut for processing such vegetation.^[12] Although no dentition is preserved for Isisaurus, the peg-like teeth typical of titanosaurs would have been suited for stripping leaves from branches, facilitating its herbivorous lifestyle. Its relatively short, vertically oriented neck, with cervical centra only about twice as long as tall, suggests a low- to mid-level browsing strategy, potentially targeting understory or lower canopy vegetation without high reaching, unlike long-necked sauropods. Robust forelimbs aided in stability during feeding.^[3] In comparison to other sauropods, Isisaurus exhibited a generalized feeding strategy similar to other titanosaurs, with its compact neck providing less reach than high browsers like Brachiosaurus but more versatility than low browsers like the diplodocid Diplodocus, which used elongate necks for precise ground-level stripping.^[12]

Locomotion and Posture

Isisaurus colberti exhibited a quadrupedal gait typical of titanosaur sauropods, with its body weight of approximately 15 tons supported by robust, pillar-like forelimbs and hindlimbs adapted for stability on floodplain terrains.^[13] The forelimbs, including a humerus estimated at 1.48 m in length, indicate a columnar posture similar to that of modern elephants, facilitating weight distribution and minimizing lateral sway during movement; this elongation and stoutness of the humerus, as seen in the type specimen (ISI R 335), underscore an elephantine stance for load-bearing efficiency.^[14] The wide-gauge limb posture, a synapomorphy of titanosaurs including Isisaurus, further enhanced this stability by positioning the feet outward from the midline, promoting a broad base for the massive body.^[14] The neck of Isisaurus was held in a primarily vertical orientation at its base, forming part of an S-shaped curve characteristic of titanosaur sauropods, which allowed for efficient access to vegetation without the horizontal extension seen in diplodocids. Limited flexibility in the neck is inferred from the relatively short cervical ribs and anteroposteriorly compact centra in the preserved middle cervical vertebrae, which would have constrained extensive lateral or dorsoventral bending while providing structural support during locomotion.^[14] As a large-bodied quadruped, Isisaurus was likely slow-moving, with maximum speeds estimated at 5–10 km/h based on limb bone proportions and general sauropod dynamic scaling models that account for stride length relative to body size.^[15] There is no skeletal evidence suggesting bipedal capabilities, consistent with the fully quadrupedal adaptations of its clade. No specific pathologies related to locomotion or posture have been reported in the known material of Isisaurus.^[14]

Physiology

Clumped isotope analysis of titanosaur eggshells from the Lameta Formation, associated with Isisaurus, indicates body temperatures averaging around 37°C, suggesting variable thermoregulation in these large sauropods adapted to a seasonal, monsoon-influenced habitat.^[4]

Paleoecology

Geological Context

The Isisaurus fossils are primarily known from the Lameta Formation, a Maastrichtian (~70–66 Ma) sedimentary unit exposed in central India, particularly in the Narmada Valley region of Madhya Pradesh. This formation consists of intertrappean beds deposited between the massive lava flows of the Deccan Traps, representing a pre-volcanic to syn-eruptive stratigraphic interval. The sediments, including limestones, sandstones, clays, and conglomerates, overlie Precambrian basement and Gondwana rocks, with an unconformable contact marking tectonic stability prior to the Late Cretaceous.^[16]^[17] The depositional environment of the Lameta Formation reflects semi-arid floodplains influenced by meandering rivers, seasonal lakes, and episodic volcanic activity from the emerging Deccan Traps. Facies analysis indicates fluvial-lacustrine settings with calcrete paleosols suggesting alternating wet and dry periods under a warm, subtropical paleoclimate with seasonal precipitation. Palynological studies reveal a diverse flora dominated by gymnosperms (e.g., conifers and Bennettitales) alongside early angiosperms, pointing to a mixed woodland-savanna ecosystem adapted to aridity and volcanic ash inputs. Fossils, including those of Isisaurus, are typically preserved in fine-grained mudstones and clays, indicative of low-energy riverine or overbank deposition that facilitated rapid burial and mineralization. The overlying Deccan volcanism, with eruptions peaking around 66 Ma, likely exacerbated environmental stress through ash fallout and climate perturbation, contributing to the broader Cretaceous-Paleogene mass extinction context.^[17]^[18]^[19] A secondary referral of Isisaurus material, including a braincase, comes from the Pab Formation in Pakistan's Sulaiman Range, which shares a Maastrichtian age and comparable lithology of sandstones interbedded with shales and paleosols. This unit records a fluvio-deltaic depositional environment with river channels, floodplains, and subaerial exposure surfaces, evidenced by trough cross-bedded sands and calcareous nodules indicating freshwater influences and periodic humidity. The similarity in age, sedimentology, and freshwater signatures supports faunal correlations across the Indo-Pakistani region during the Late Cretaceous.^[2]^[20]

Contemporaneous Biota

Isisaurus colberti coexisted with other titanosaurian sauropods in the Maastrichtian Lameta Formation of central India, most notably Jainosaurus septentrionalis, a potentially sympatric taxon distinguished by its larger body size and more robust limb elements.^[21] Fossils of Jainosaurus, including partial skeletons, indicate it occupied similar fluvial and lacustrine habitats, suggesting niche partitioning among sauropods based on body size and possibly foraging height.^[2] The primary predators of Isisaurus were abelisaurid theropods, including Rajasaurus narmadensis, Indosuchus raptorius, and Rahiolisaurus gujaratensis, which preyed on large herbivores through ambush tactics suited to the semi-arid floodplains.^[22]^[23]^[24] Smaller carnivorous theropods, such as noasaurids, may have scavenged remains or targeted juveniles, contributing to a dynamic carnivore guild.^[25] The broader vertebrate assemblage included crocodylomorphs, evidenced by nesting sites in sauropod hatcheries, indicating opportunistic interactions in nesting grounds.^[26] In 2023, a major titanosaur nesting site was discovered in the Dhar district of the Lameta Formation, featuring 92 nests containing 256 eggs, suggesting colonial nesting behavior among these large herbivores.^[27] Turtles, such as the pelomedusoid Jainemys pisdurensis, inhabited aquatic margins, while holostean fish like Pycnodus lametae populated freshwater systems.^[28]^[29] Early birds and mammals were rare, with fragmentary eutherian remains suggesting limited mammalian presence in the ecosystem.^[30] As a mid-to-large herbivore estimated at 15-18 meters in length, Isisaurus likely played a key role in shaping vegetation structure through browsing on high-level foliage, influencing plant community dynamics in a semi-arid to subtropical setting. The overall low faunal diversity reflects end-Cretaceous stressors, including climatic instability and the onset of Deccan Traps volcanism, which reduced habitat suitability.^[31] Recent post-2020 discoveries, such as new noasaurid cranial material, highlight ongoing updates to this incomplete Maastrichtian record.^[25]

References

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Isisaurus | Natural History Museum
Isisaurus ; Diet: herbivorous ; When it lived: Late Cretaceous, 71–66 million years ago ; Found in: India ; Taxonomy: Dinosauria, Saurischia, Sauropodomorpha, ...Missing: credible sources
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Jul 15, 2009 · Currently two genera, Isisaurus and Jainosaurus, are recognized from the Cretaceous of India. ... Sauropod dinosaur humeri from Lameta Group ( ...
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How shortweird was Isisaurus?
Aug 13, 2009 · Isisaurus went the opposite direction–its cervical centra are only about twice as long as tall, right down the column.
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Oct 20, 2020 · The taxonomic revision of Late Cretaceous (Maastrichtian) Indian dinosaurs has clarified that only Titansauriforme sauropods (Isisaurus, ...
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A new taxon, Titanosaurus colberti, is erected for the reception of the new material. The genus Titanosaurus is diagnosed and three species are identified from ...
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The Maastrichtian Lameta Formation is divided into four lithostratigraphic units (from the oldest to the youngest): Green Sandstone, Lower Limestone, Mottled ...
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... to Montague (2006) , Isisaurus might have reached a length of about 18 m and a weight of about 14,000 kg based on that specimen. Isisaurus is known from ...
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Why sauropods had long necks; and why giraffes have short necks
... Isisaurus colberti (Jain & Bandyopadhyay, 1997) are even shorter anteroposteriorly, but have more dorsally located cervical ribs; by contrast, the cervical ...
[10]
(PDF) Reassessment of Sauropod Dinosaur Jainosaurus ...
Currently two genera, Isisaurus and Jainosaurus, are recognized from the Cretaceous of India. Unlike most titanosaurs, both Isisaurus and Jainosaurus are ...
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Mar 3, 2017 · (2003) ... As these fungi attack leaves of herbs, shrubs and trees, it is very likely that Isisaurus also used to browse the leaves of trees.
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Isisaurus colberti life restoration by Cisiopurple. Scientific ... Isisaurus would have grown to about 18 meters length and weighed about 15,000 kg.Missing: estimate | Show results with:estimate
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Isisaurus colberti is diagnosed by the following autapomorphies: anteroposteriorly elongate cervical para- pophyses (Jain & Bandyopadhyay 1997), cervical neural.
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Speeds and gaits of dinosaurs - ScienceDirect.com
Stegosaurs and ankylosaurs may have had maximum speeds as low as 6–8 km/h. Sauropods may have attained 12–17 km/h, and some ceratopsians may have been capable ...
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Overall the Lameta beds are considered to represent a regionally extensive Maastrichtian regolith. Carbon and oxygen isotope analyses of calcareous components ...Missing: paleoclimate | Show results with:paleoclimate
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Aug 10, 2025 · Most scientific ideas on the paleoenvironment of the Lameta Formation were based on paleontology and coarser sedimentary facies studies. Some ...
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[PDF] Palynoflora from Deccan volcano-sedimentary sequence ...
Nov 2, 2009 · Lameta sediments, was dominated by gymnosperms-angiosperm association. The plant canopy consisted mainly of gymnosperms (Conifers and ...
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Dec 5, 2022 · The debate concerning the relative importance of the Chicxulub bolide impact and/or Deccan Traps (DT) volcanism as the cause of the extinction of non-avian ...
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Sedimentary Facies, Architectural Elements, and Depositional ...
Mar 27, 2023 · The Pab Formation (with interbeds of clay and shale) reaches a maximum thickness of 480 m along the eastern limb of the Mughalkot anticline in ...
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Sep 15, 2011 · The Chhota Simla caudal centrum has similar proportions to middle caudal vertebrae of Isisaurus colberti (centrum length/width c. 0.67), and ...
[21]
[PDF] contributions from the museum of paleontology - Cloudfront.net
Aug 17, 2006 · - Rajasaurus narrnadensis is characterized by the following autapomorphies: me- dian nasofrontal prominence, with the frontals forming only the ...Missing: primary | Show results with:primary
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Aug 6, 2025 · Maastrichtian dinosaur fossils are known mainly from the Lameta Formation in three areas, the Jabalpur (Madhya Pradesh), Nand-Dongargaon and ...
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The Lameta Formation (Upper Cretaceous, Maastrichtian) of India has yielded abundant fossils of a-belisaurid theropods, including bones from the cranium, ...
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Feb 7, 2024 · Earlier reports of abelisaurid dinosaurs from India are from the Upper Cretaceous (Maastrichtian) Lameta Group of Jabalpur, Pisdura (Central ...<|control11|><|separator|>
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Dec 7, 2015 · The Late Cretaceous Lameta Formation of India is widespread and contains a great wealth of sauropod dinosaur egg nests. From this predominantly ...
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A revision of the pelomedusoid turtle Jainemys pisdurensis from the ...
Jun 22, 2020 · A Maastrichtian age has been suggested for the Lameta Formation of Pisdura and Dongargaon on the basis of dinosaur skeletal remains, nests, eggs ...
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<I>Pycnodus lametae</I> (Pycnodontidae), a Holostean Fish from ...
May 1, 1996 · A well-preserved, nearly complete skeleton of the holostean fish Pycnodus lametae, is described from the freshwater Upper Cretaceous Lameta Formation of ...
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On the age of the dinosaur fauna from the Lameta Formation (Upper Cretaceous of Central India). Source: Newsletters on Stratigraphy. Fossil Snakes from the ...<|control11|><|separator|>
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Vertebrate fauna from the Deccan volcanic province
For a long time, the Lameta Formation was regarded as. Turonian in age, based on the similarity of dinosaur fauna between the Lameta Formation and the Maevarano ...