Direct effect of ice sheets on terrestrial bicarbonate, sulphate and base cation fluxes during the last glacial cycle: minimal impact on atmospheric CO2 concentrations

Chemical erosion in glacial environments is normally a consequence of chemical weathering reactions dominated by sulphide oxidation linked to carbonate dissolution and the carbonation of carbonates and silicates. Solute fluxes from small valley glaciers are usually a linear function of discharge. Re...

Full description

Bibliographic Details

Main Authors:	Martyn Tranter, P. Huybrechts, G. Munhoven, M.J. Sharp, G.H. Brown, I.W. Jones, A.J. Hodson, Richard Hodgkins
Format:	Default Article
Published:	2002
Subjects:	Geochemistry not elsewhere classified Geology not elsewhere classified Other earth sciences not elsewhere classified Glaciers Chemical denudation rates Global geochemical cycles Atmospheric CO2 concentrations Geochemistry Earth Sciences not elsewhere classified Geology
Online Access:	https://hdl.handle.net/2134/3325
Tags:	Add Tag No Tags, Be the first to tag this record!