『Abstract
　Water samples from the Fraser, Skeena and Nass River basins of the Canadian Cordillera were analyzed for dissolved major element concentrations (HCO3^-, SO4^2-, Cl^-, Ca²⁺, Mg²⁺, K⁺, Na⁺), δ¹³C of dissolved inorganic cation (δ¹³CDIC), and δ³⁴S of dissolved sulfate (δ³⁴SSO4) to quantify chemical weathering rates and exchanges of CO2 between the atmosphere, hydrosphere, and lithosphere. Weathering rates of silicates and carbonates were determined from major element mass balance. Combining the major element mass balance with δ³⁴SSO4(-8.9 to 14.1‰CDT) indicates sulfide oxidation (sulfuric acid production) and subsequent weathering of carbonate and to a lesser degree silicate minerals are important processes in the study area. We determine that on average, 81％ of the riverine sulfate can be attributed to sulfide oxidation in the Cordilleran rivers, and that 25％ of the total weathering cation flux can be attributed to carbonate and silicate dissolution by sulfuric acid. This result is validated by δ¹³CDIC values (-9.8 to -3.7‰VPDB) which represents a mixture of DIC produced by the following weathering pathways: (i) carbonate dissolution by carbonic acid (-8.25‰)＞(ii) silicate dissolution by carbonic acid (-17‰)≒(iii) carbonate dissolution by sulfuric acid derived from the oxidation of sulfides (coupled sulfide-carbonate weathering)(+0.5‰).
　δ³⁴SSO4 is negatively correlated with δ¹³CDIC in the Cordilleran rivers, which further supports the hypothesis that sulfuric acid produced by sulfide oxidation is primarily neutralized by carbonates, and that sulfide-carbonate weathering impacts the δ¹³CDIC of rivers. The negative correlation between δ³⁴SSO4 and δ¹³CDIC is not observed in the Ottawa and St. Lawrence River basins. This suggests other factors such as landscape age (governed by tectonic uplift) and bedrock geology are important controls on regional sulfide oxidation rates, and therefore also on the magnitude of sulfide-carbonate weathering - i.e., it is more significant in tectonically active areas.
　Calculated DIC fluxes due to Ca and Mg silicate weathering by carbonic acid (38.3×10³ mol C・km^-2・yr^-1) are similar in magnitude to DIC fluxes due to sulfide-carbonate weathering (18.5×10³ mol C・km^-2・yr^-1). While Ca and Mg silicate weathering facilitates a transfer of atmospheric CO2 to carbonate rocks, sulfide-carbonate weathering can liberate CO2 from carbonate rocks to the atmosphere when sulfide oxidation exceeds sulfide deposition. This implies that in the Canadian Cordillera, sulfide-carbonate weathering can offset up to 48％ of the current CO2 drawdown by silicate weathering in the region.』

1. Introduction
2. Chemical weathering pathways
　2.1. Carbonic acid-based weathering
　2.2. Sulfuric acid-based weathering
3. Study area
　3.1. Watershed characteristics
　3.2. Basin geology
4. Methods
　4.1. Field methods
　4.2. Water samples
　4.3. Laboratory analyses
　　4.3.1. Cations and anions
　　4.3.2. Carbon isotopes
　　4.3.3. Sulfur isotopes
5. Results
　5.1. Major elements
　5.2. Dissolved inorganic carbon and δ¹³CDIC
　5.3. Dissolved sulfate and δ³⁴SSO4
6. Chemical weathering rates
　6.1. Rock types contributing to weathering products
　　6.1.1. Mass balance
　　　6.1.1.1. Step 1: Atmospheric input
　　　6.1.1.2. Step 2: Apportion SO4^* to sulfide and evaporite dissolution
　　　6.1.1.3. Step 3: Apportion cations and DIC to weathering of carbonates and silicates by sulfuric acid
　　　6.1.1.4. Step 4: Apportion cations and DIC to weathering of silicates by carbonic acid
　　　6.1.1.5. Step 5: Apportion cations and DIC to weathering of carbonates by carbonic acid
　6.2. Pollution inputs
　6.3. Mass balance results
　6.4. Validation of results
　　6.4.1. Carbon isotopes
　　6.4.2. End-member definition
　　6.4.3. Measured δ¹³CDIC　　
　　6.4.4. Expected δ¹³CDIC
7. CO2 fluxes due to chemical weathering
8. Conclusions
Acknowledgments
References