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The runoff and riverine fluxes of HCO 3- , Si and Ge that arise from chemical erosion in non-glaciated terrain, are modelled at six time steps from the Last Glacial Maximum (LGM) to the present day. The fluxes that arise from the Great Ice Sheets are also modelled. Terrestrial HCO 3- fluxes decrease during deglaciation, largely because of the reduction in the area of the...
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