Step 1: Fe and Al oxides are variable-charge minerals with a naturally high zero point of charge, around pH 8 to 9.
Step 2: Intense weathering increases their share in the soil, pulling the overall ZPC toward that higher value, supporting A.
Step 3: Organic matter's functional groups interacting with these oxide surfaces are described as reinforcing this same upward shift, supporting R.
Step 4: Both statements hold together, matching the first option.