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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Anjar India
Cretaceous age for Ir‐rich Deccan intertrappean deposits: palaeontological evidence from Anjar, western India Available to Purchase
Revisiting the 1956 Anjar Earthquake in Western India: Empirical Green’s Function Approach Available to Purchase
The Possibility of Site Effects: The Anjar Case, following Past Earthquakes in Gujarat, India Available to Purchase
False Site Effects: The Anjar Case, following the 2001 Bhuj (India) Earthquake Available to Purchase
Natural fullerenes from the Cretaceous-Tertiary boundary layer at Anjar, Kutch, India Available to Purchase
Full article available in PDF version.
Moment Tensor Solutions of some Selected Local Events: Implications towards the Present-day Tectonics of the Kachchh Rift zone Available to Purchase
Vertebrate fauna from the Deccan volcanic province: Response to volcanic activity Available to Purchase
During the last two decades, extensive paleontological research in the main Deccan volcanic province has led to a better understanding of biodiversity close to the Cretaceous-Paleogene boundary. Several infratrappean localities exposed in Jabalpur, Kheda, Balasinor, Rahioli, Dohad, and Bagh in the Narmada Valley (India) preserve one of the most geographically widespread dinosaur nesting sites known in the world. The well-studied intertrappean beds, such as those of Naskal on the southern margin, Asifabad and Nagpur on the eastern margin, Kisalpuri and Mohgaon Kalan on the northeastern margin, and Anjar on the northwestern margin of the main Deccan volcanic province, have yielded Maastrichtian fish (Igdabatis) and dinosaur remains and palynofossils (Aquilapollenites - Gabonisporites - Ariadnaesporites), either separately or in association, that suggest a Maastrichtian age for these beds. Only two intertrappean sections, Papro on the northern margin and Jhilmili on the northeastern margin of the main Deccan volcanic province, have produced Paleocene fossils. The fossil record from the infratrappean and intertrappean beds demonstrates that the dinosaurs survived the early phase of volcanism, though there was an apparent decline in their diversity, and that freshwater vertebrate fauna was least affected by the initial volcanic activity. The episodic nature of Deccan volcanism may possibly explain the survival of many freshwater and terrestrial communities during the periods of quiescence. In addition, as in the case of the late Maastrichtian sections in eastern Montana, North America, detritus-feeding freshwater vertebrate communities possibly had greater potential for survival than the terrestrial communities dependent on primary productivity. A close examination of the vertebrate faunal distribution across the two stratigraphic intervals (infratrappean and intertrappean) suggests that sampling bias in the infratrappean beds may have also masked the actual diversity of these beds.