The Asian monsoons are triggered by complex interactions between the atmosphere, Asian
and African orography, and the surrounding oceans, resulting in highly seasonal climate …

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

Abstract The Deccan-associated sediments (Lameta Formation and intertrappean) hold
great potential for understanding the role of Deccan Volcanism in the Maastrichtian …

The drivers of the evolution of the South Asian Monsoon remain widely debated. An
intensification of monsoonal rainfall recorded in terrestrial and marine sediment archives …

The rainforests near the early Eocene palaeo-equator were more resilient to greenhouse
warming than mid-latitude vegetation. The mechanism underlying that resilience remains …

Quantitative Miocene climate and vegetation data from the Siwalik succession of western
Nepal indicate that the development of the Indian summer monsoon has had an impact …

Recognition of the existence of an Andean-type continental margin in southern Tibet prior to
its collision with India has provided crucial constraints on the formation of the Tibetan …

Abstract The Cenomanian–Santonian (C–S) carbonate successions include valuable
petroleum reservoirs in the Zagros Basin. They also provide important information on the …

Early Paleogene latitudinal precipitation gradients and patterns along the Pacific coast of
Eurasia are studied in time and space using the Coexistence Approach, for the first time …

Our understanding of the low latitude terrestrial climate of the late Maastrichtian is far from
satisfactory. We have attempted to reconstruct the late Maastrichtian vegetation and climate …