Reorganization of the Asian climate from one dominated by global planetary wind systems
to a regional monsoon climate is closely related to the surface uplift of the Tibetan Plateau …

Rapid atmospheric warming since the mid-twentieth century has increased temperature-
dependent erosion and sediment-transport processes in cold environments, affecting food …

Mountain uplift and erosion have regulated the balance of carbon between Earth's interior
and atmosphere, where prior focus has been placed on the role of silicate mineral …

Uplift and erosion modulate the carbon cycle over geologic timescales by exposing minerals
to chemical weathering. However, the erosion sensitivity of mineral weathering remains …

Fine-grained muds produced largely from rock weathering at the Earth's surface have great
influence on global carbon cycling. Mud binds and protects organic carbon (OC) from …

Seafloor sediment flows, called turbidity currents, form the largest sediment accumulations,
deepest canyons and longest channels on Earth. It was once thought that turbidity currents …

This paper aims to update our understanding of the carbon cycle in the Himalayas, the most
intense collisional orogeny globally, by providing new insight into its impact on Cenozoic …

The Palaeozoic evolution of land plants revolutionized river geomorphology. However, the
relationships between biotic forcing and channel dynamics are still debated and, as such …

In this Perspective, we put forward an integrative framework to improve estimates of land-
atmosphere carbon exchange based on the accumulation of carbon in the landscape as …

Submarine turbidity currents form the largest sediment accumulations on Earth, raising the
question of their role in global carbon cycles. It was previously inferred that terrestrial …