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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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https://doi.org/10.1007/978-3-031-13119-6Climate Change; Disaster Management; Middle Miocene Climatic Optimum; Palaeoclimate; Polar Climate
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Early Paleogene Megaflora of the Palaeoequatorial Climate: A Case Study from the Gurha Lignite Minethe equator (∼10°N), and was moving northwards towards Eurasia. In this chapter we mainly focus on the Gurha lignite mine as it is very rich in plant remains. It is situated ~47 km WSW of Bikaner in western Rajasthan. The plant fossils of this mine are late Paleocene-early Eocene in age and show sim
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Development of Cenogram Technique Over the Past Six Decades with Some Insights into the Varied Habible baseline to analyze the effects of these transcendent climatic changes on the mammalian community structures. The present investigation is an attempt to examine the palaeohabitat of a Neogene (Middle Miocene: ~15–11.5 Ma) geographically distant (i.e., from Spain, China, and India) extinct mammal
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Palynofloral Diversity During Mid-Miocene Warming in Kerala Basin, South-Western India: Palaeoclimate events of the Neogene, MMCO (Mid-Miocene Climate Optimum) that occurred around ~17–15 Ma is considered to be the most recent extreme global warming episode. The global warming during MMCO, created annual surface temperature ~3–4 °C higher than the present, is equivalent to the warming predicted f
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Non-Pollen Palynomorphs from the Late-Holocene Sediments of Majuli Island, Assam (Indo-Burma Regionn order to provide an overview of palaeoenvironment in Majuli Island (world largest river island), Assam for the late Holocene. About 25 varieties of non-pollen palynomorphs were reported, out of which fungal spores were at high abundance along with scanty occurrence of zoological remains reflecting
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