Jump directly to the page contents

Recent Highlights

Feedbacks in the land-ocean transition

Influence of erosion on the oceanic CO2 storage capacity

Alkalinity generation from rock weathering modulates Earth’s climate at geological time scales. Particularly challenging remains the discrimination of climatic and erosional influences. Based on global observations, here we uncover the role of erosion rate in governing riverine alkalinity, accompanied by areal proportion of carbonate, mean annual temperature, catchment area, and soil regolith thickness. We show that the weathering flux to the ocean will be significantly altered by climate warming as early as 2100, by up to 68% depending on the environmental conditions, constituting a sudden feedback of ocean CO2 sequestration to climate.