Evidence from the age of the dinosaurs to today shows that chemical weathering of rocks is less sensitive to global temperature, and may depend on the steepness of the surface. The results call into ...

Rock organic carbon oxidation CO 2 release offsets silicate weathering sink It has been hypothesized that the interval of glaciations at the end of the Late Ordovician (peaking in the Hirnantian Stage ...

A new University of Washington study shows that the textbook understanding of global chemical weathering -- in which rocks are dissolved, washed down rivers and eventually end up on the ocean floor to ...