Deccan Vegetation
نویسندگان
چکیده
منابع مشابه
Biodiversity during the Deccan volcanic eruptive episode
This paper gives a detailed overview of biotic assemblages recovered from the Deccan trap intercalated sedimentary sequences (infraand intertrappean beds) of peninsular India as a result of extensive research done during the last 20 years. The infraand intertrappean beds contain remnants of Gondwanan forms such as myobatrachinae frogs, pelomedusid turtles, dinosaurs (i.e. titanosaurids and abel...
متن کاملRheumatic Heart Disease in the Bombay Deccan
By L. B. CARRUTHERS, b.a., m.d., c.m. American Presbyterian Hospital, Miraj, S. M. C. ' he conception that rheumatic fever and its concomitants are rare or entirely unknown within the true tropics has long been in favour. Seemingly it received strong confirmation when Clarke (*1930) published his notable paper on the geographical distribution of rheumatic fever. Rogers and Megaw (1930) in India...
متن کاملWhat Is the "Hill Fever of Mysore and Deccan"?
Sir,?Can any of your readers give any information as to the nature of what has been called the " Hill Fever" of Mysore and the Deccan 1 In reading an account of malaria* recently, I came across the following: " The hill fever of Mysore occurs among bare rocks, stones and brown earth, at the hottest season from March to June, when the rocks in the sun show a surface temperature of 220?F. and rap...
متن کاملPaleoenvironmental signature of the Deccan Phase-2 eruptions
*Correspondence: Eric Font, IDL-FCUL, Instituto Dom Luís, Faculdade de Ciências, Universidade de Lisboa, Edifício C8-8.3.22, Campo Grande, 1749-016 Lisboa, Portugal e-mail: [email protected] The environmental impact of the Deccan trap volcanism is poorly understood as yet. The paucity of geological markers that can unambiguously be attributed to the Deccan volcanism and the temporal coincid...
متن کاملMercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction
The contribution of the Deccan Traps (west-central India) volcanism in the CretaceousPaleogene (KPg) crisis is still a matter of debate. Recent U-Pb dating of zircons interbedded within the Deccan lava flows indicate that the main eruptive phase (>1.1 × 106 km3 of basalts) initiated ~250 k.y. before and ended ~500 k.y. after the KPg boundary. However, the global geochemical effects of Deccan vo...
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ژورنال
عنوان ژورنال: Botanical Gazette
سال: 1922
ISSN: 0006-8071
DOI: 10.1086/332984