Abstract The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative
to today. Continental configurations and mountain topography transitioned toward modern …

The often-used phrase 'the uplift of the Tibetan Plateau'implies a flat-surfaced Tibet rose as a
coherent entity, and that uplift was driven entirely by the collision and northward movement …

The growth of the Tibetan Plateau throughout the past 66 million years has profoundly
affected the Asian climate, but how this unparalleled orogenesis might have driven …

Abstract The Eocene–Oligocene transition (EOT) was a climate shift from a largely ice-free
greenhouse world to an icehouse climate, involving the first major glaciation of Antarctica …

The origins and development of the arid and highly seasonal steppe-desert biome in Central
Asia, the largest of its kind in the world, remain largely unconstrained by existing records. It …

The uplift history of south-eastern Tibet is crucial to understanding processes driving the
tectonic evolution of the Tibetan Plateau and surrounding areas. Underpinning existing …

Views differ on the uplift history of the SE Tibetan Plateau and causal geodynamic
mechanisms, yet reliable age-constrained paleoaltimetry in this region could test growth …

The uplift of eastern Tibet, Asian monsoon development and the evolution of globally
significant Asian biodiversity are all linked, but in obscure ways. Sedimentology …

As a crucial part of the Asian monsoon stretching from tropical India to temperate East Asia,
the Indian monsoon (IM) contributes predominant precipitation over Asian continent …

The biodiversity of the Himalaya, Hengduan Mountains and Tibet, here collectively termed
the Tibetan Region, is exceptional in a global context. To contextualize and understand the …