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GeoRef Categories
Era and Period
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Book Series
Date
Availability
Dongargaon Hill Beds
Vertebrate biodiversity of the Deccan volcanic province of India: A review Available to Purchase
Vertebrate Fauna From the Infra- and Inter-trappean Beds of Andhra Pradesh: Age Implications Available to Purchase
Pycnodus lametae (Pycnodontidae), a Holostean Fish from Freshwater Upper Cretaceous Lameta Formation of Maharashtra Available to Purchase
Deccan Continental Flood Basalt Eruption Terminated Indian Dinosaurs before the Cretaceous-Paleogene Boundary Available to Purchase
Abstract: Late Cretaceous-Early Paleogene sediments associated with Deccan Continental Flood Basalt (DCFB) sequences of central and western India record the timing of the introduction and extinction of Late Cretaceous dinosaurs in India based on magnetostratigraphy and magnetic susceptibility stratigraphy. Current taxonomy indicates that only two genera of titanosaurs (e.g., Isisaurus and Jainosaurus), at least four species of large-bodied abelisauridae theropods (e.g., Rajasaurus narmadensis, Rahiolisaurus gujaratensis, Indosuchus matleyi and Indosaurus raptorius) and a small-bodied theropod Laevisuchus inhabited India during the Maastrichtian. Their stratigraphic and geographic distribution suggests that these dinosaurs were dominated by titanosauriforme and abelisauridae that first appeared before the advent of Deccan volcanism in the magnetochron C30n and were well established with the acme of breeding and nesting during C30n to maastrichtian C29r. Their decline in diversity and abundance coincides with initiation of DCFB eruptions when most of the early taxa were terminated and only a few titanosauriforme sauropods survived becoming extinct at about 350 kyr before the Cretaceous-Paleogene boundary (KPB). Dinosaur extinction in India is thus directly tied to Deccan volcanism with no evidence of an asteroid impact.
Implications of the infra- and inter-trappean biota from the Deccan, India, for the role of volcanism in Cretaceous-Tertiary boundary extinctions Available to Purchase
Cretaceous-Tertiary Boundary Events: The Fossil Vertebrate, Palaeomagnetic and Radiometric Evidence from Peninsular India Available to Purchase
Fungi in dinosaurian (Isisaurus) coprolites from the Lameta Formation (Maastrichtian) and its reflection on food habit and environment Available to Purchase
Aquilapollenites and other triprojectate pollen from the Late Cretaceous to Early Paleocene Deccan intertrappean deposits of India Available to Purchase
Palaeoecology and Affinity of Ostracod Fauna from the Classic Localities of Lameta Formation of Jabalpur, Madhya Pradesh, India Available to Purchase
Abstract : Contrasting opinions have been expressed by different workers about the palaeo-environments of the Lameta Formation of Jabalpur. Some workers have ascribed a shallow marine/estuarine environment of depositions for its sediments, while others have favoured a non-marine interpretation. The present authors have recently recorded 26 ostracod species from the basal beds of Lameta Formation from three classic localities (i.e., Chui Hill, Bara Simla Hill and Chhota Simla Hill). These are univocally freshwater fauna. Khosla and Sahni (2000) earlier proposed Late Cretaceous Mongolian and Chinese affinities for the ostracod fauna of the Lameta Formation of Jabalpur. Whatley and Bajpai (2006) considered them strongly endemic to India. Our study revealed an African and/or South American zoogeographic affinity. The genera common to these continents are Altanicypris , Neuquenocypris, Paracypretta, Stenocypris and Wolburgiopsis .
Pyroxenes from Alkaline Rocks of the Chhota Udaipur Carbonatite-Alkaiic Province, Gujarat, India Available to Purchase
Stratigraphy, structure and volcanology of the SE Deccan continental flood basalt province: implications for eruptive extent and volumes Available to Purchase
Lithostratigraphy of the Paleogene Deccan Intra-, Intertrappeans of the Saurashtra, Western India and their Prevalence in Large Igneous Provinces Available to Purchase
Splenial and Vomerine Dentitions of Pycnodont Fishes from the Upper Part of the Subathu Formation (Middle Eocene), Malyuriyan, Rajauri District, Jammu and Kashmir Available to Purchase
Morphological and Stratigraphical Significance of Lower Gondwana Plant Fossils of Mohpani Coalfield, Satpura Gondwana Basin, Madhya Pradesh Available to Purchase
Late Cretaceous continental vertebrate fossil record from India: Palaeobiogeographical insights Available to Purchase
Understanding the Interrelationship of Aquifer Parameters and Sedimentary Characteristics of an Aquifer: A Case Study of WRD Watershed, Chandrapur District, Maharashtra Available to Purchase
EARLY DANIAN PLANKTIC FORAMINIFERA FROM CRETACEOUS-TERTIARY INTERTRAPPEAN BEDS AT JHILMILI, CHHINDWARA DISTRICT, MADHYA PRADESH, INDIA Available to Purchase
The history of dinosaur collecting in central India, 1828–1947 Available to Purchase
Abstract The history of dinosaur collecting in central India (former Central Provinces and Central India Agency) began in 1828 when W. H. Sleeman discovered isolated sauropod caudal vertebrae in the Lameta Formation near Jabalpur. Subsequently, the area became a focal point for fossil collection, leading to a series of further discoveries that continues today. The earliest discoveries were made by numerous collectors for whom palaeontology was a secondary pursuit, and who were employed in the armed forces (W. H. Sleeman and W. T. Nicolls), medicine (G. G. Spilsbury) or as geologists (T. Oldham, H. B. Medlicott, T. W. H. Hughes and C. A. Matley). Most of their finds were concentrated around Jabalpur or farther south near Pisdura and often consisted of isolated, surface-collected bones. Charles Matley undertook the two most extensive collecting efforts, in 1917–1919 and 1932–1933 (Percy Sladen Trust Expedition). As a result he discovered significant deposits of dinosaurs on Bara Simla and Chhota Simla, revisited Pisdura, and mapped the Lameta Formation. Many new dinosaur taxa resulted from Matley's studies, which still represent most of the known Lameta Formation dinosaur fauna. Current scientific understanding places these fossils among the Sauropoda (as titanosaurians) and Theropoda (as abelisaurids and noasaurids). Early reports of armoured ornithischians were erroneous; these materials also pertain to sauropods and theropods. Supplementary material: A list of the archival documents in the Natural History Museum, London that were used for this study is available at http://www.geolsoc.org.uk/SUP18418 .