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The progressive co-evolutionary development of the Pan-Tibetan . . . We argue that an east–west-oriented Paleogene Central Tibetan Valley was a cradle and conduit for thermophilic biota, seeding the modern regional biodiversity The rise of eastern Tibet intensified regional rainfall and erosion, which increased topographic relief and biodiversification
Open Research Online Understanding the interplay between monsoon dynamics, landscape and biodiversity are critical for future resource management We explore the strengths and weaknesses of different palaeoaltimetric methodologies as applied across the Tibetan region
Contents | Geological Society, London, Special Publications 549, 1 This book addresses the interplay between geodynamics, climate and biodiversity, focusing on the India–Asia collision, the key abiotic parameter shaping the region's topography, climate and ecosystems
The progressive co-evolutionary development of the Pan-Tibetan . . . The rise of eastern Tibet intensified regional rain-fall and erosion, which increased topographic relief and biodiversification Gradual monsoon development reflected the evolving topography, but modern-like Asian monsoons developed only after a plateau formed in the Miocene
The progressive co-evolutionary development of the Pan-Tibetan . . . We argue that an east–west-oriented Paleogene Central Tibetan Valley was a cradle and conduit for thermophilic biota, seeding the modern regional biodiversity The rise of eastern Tibet intensified regional rainfall and erosion, which increased topographic relief and biodiversification