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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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Indian Peninsula
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India (2)
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Siwalik Range (1)
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fossils
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Chordata
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Vertebrata (1)
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fossil man (1)
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geologic age
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Cenozoic
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Quaternary
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Pleistocene
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lower Pleistocene (1)
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upper Pleistocene (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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granites (1)
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pegmatite (1)
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Primary terms
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Asia
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Indian Peninsula
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India (2)
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Siwalik Range (1)
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Cenozoic
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Quaternary
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Pleistocene
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lower Pleistocene (1)
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upper Pleistocene (1)
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Chordata
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Vertebrata (1)
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fossil man (1)
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igneous rocks
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plutonic rocks
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granites (1)
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pegmatite (1)
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petrology (1)
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Odara area
The Odara pegmatite
A New Technique for the Determination of Homogenization Temperatures of Fluid Inclusions
Genesis of Two Zoned Pegmatites of the Bihar Mica Belt: A Fluid Inclusion Study
Petrochemistry of the Chengannoor Granite, Alleppey District, Kerala
Studies on Zircon - Host Rock/Sediment Association along Manimala River Meanders in Kerala
Gemstone Mineralization in Southern Kerala, India
Granite-Molybdenite System of Ambalavayal, Kerala: Part II. Nature of Mineralization, Sulphur Isotopes, Fluid Characteristics and Genetic Model
Chrono-contextual issues at open-air Pleistocene vertebrate fossil sites of central and peninsular India and implications for Indian palaeoanthropology
Abstract Pleistocene vertebrate fossils are prominently known from several regions across the Indian Subcontinent including the Siwalik Hills, the numerous river valleys across India and some cave sites. Unfortunately, most of this evidence is lacking a robust chronological framework and very few fossil specimens have been subjected to absolute dating methods. All of the known fossil evidence is found in diverse sedimentary contexts and these faunal assemblages have mostly been assigned broad or relative age brackets such as Early Pleistocene (i.e. the Pinjore Formation of the Upper Siwalik Subgroup) and Late Pleistocene (almost all the remaining fossil vertebrate fauna in the rest of the Subcontinent). This paper discusses contextual and chronological perspectives and associated interpretative issues of open-air Pleistocene faunal sites south of the Siwalik Hills, such as north-central and peninsular India. For instance, the virtual lack of Early and Middle Pleistocene fauna across most of India requires consideration and explanations beyond just the lack of absolute dates. A general review of the known data demonstrates a critical need for absolute dates for the various fauna as well as more rigorous field and lab methods for Indian palaeontology in general, and to avoid erroneous implications for Indian palaeoanthropology.