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Titlebook: Climate Change and Environmental Impacts: Past, Present and Future Perspective; Binita Phartiyal,Rahul Mohan,Anil Kumar Gupta Book 2022 Th

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F. M. A. Heußen,S. R. Sadda,A. C. Walshala Basin Neogene sequence consists of Quilon and Warkalli Formation within Malabar Super Group. The present palynological study has been done on sediment samples from Quilon Formation exposed at Padappakara section near Ashtamudi Kayal in Kollam district, Kerala. The assemblage consists of diverse
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https://doi.org/10.1007/978-3-642-66435-9 the quartz, opaque’s (Fe-Ti Oxides), phosphate minerals and heavy minerals including Zircon, Sphene (?), Monazite (?), Allnite (?) etc. The attenuation and fractionation of Heavy metals and other mineral phases elucidated through elemental signatures of stream sediment samples (alluvium) from the O
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Expression and Purification of CRABPs from ,omplete ablation period the total rainfall and its distribution varies from year to year. Based on the collected 4 years of data the average seasonal rainfall for the Gangotri Glacier was observed to be about 221.2 mm. The average daily maximum and minimum temperatures over the ablation season were
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https://doi.org/10.1385/0896034380 values of the transpired water showed strong sensitivity to the soil water content. It means that the soil water uptake by plants is strongly controlled by the soil water dynamics, which modulate the isotopic values of the transpired water. The break phases of monsoon result in characteristic isoto
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