The uplift of the Tibetan Plateau is an important geological event, but there is considerable
controversy about its growth history. Different geological observations contribute to this …

A broad compilation of modern carbon isotope compositions in all C3 plant types shows a
monotonic increase in δ 13C with decreasing mean annual precipitation (MAP) that differs …

The remarkable uplift of the Tibetan Plateau in the Neogene had great impacts on the
climate and environment of East Asia and even the world. Therefore, establishment of the …

Over the last two decades, many quantitative paleoaltimetry reconstructions of the Tibetan
Plateau have been published, but they are still preliminary and controversial, although …

This study presents new δ18O and δD data from 191 streams across the Himalaya and
Tibetan Plateau to better constrain the spatial variability of stable isotopes in modern …

Estimates of the permafrost-climate feedback vary in magnitude and sign, partly because
permafrost carbon stability in warmer-than-present conditions is not well constrained. Here …

The relationship between central Asian aridification and the evolution of the Himalayan–
Tibetan orogen remains elusive. New isotopic data from pedogenic and lacustrine …

East–west extension has been a prominent feature of Cenozoic tectonics in central-southern
Tibet, and the onset of this extension has been interpreted as indicating the surface uplift of …

It has been demonstrated in climate models that both the Indian and East Asian summer
monsoons (ISM and EASM) are strengthened by the uplift of the entire Asian orography or …

Bos grunniens Linnaeus, 1766, and Bos mutus (Przewalski, 1883) are the domestic and wild
forms, respectively, of the bovid commonly called the yak. B. mutus inhabits remote high …