Evolution of soil erosion rates in alpine soils of the Central Rocky Mountains using fallout Pu and δ¹³C

Data from soil chronosequences have been widely used to quantify soil formation and weathering rates, but are less used to determine erosion rates and the stabilisation of moraines over time. We hypothesise that soil erosion rates on moraine hillslopes decrease over time as soils evolve and slopes stabilise. We selected a sequence of moraines in the Wind River Range (Central Rocky Mountains) to study these processes over time. Moraine ages were based on ¹⁰Be surface exposure dating of moraine boulders. Quantitative soil erosion and accumulation rates along slopes with similar exposures, lengths and gradients were determined from profile patterns of ^239+240Pu radionuclides. We used stable carbon isotopes (δ¹³C) in relation with the total soil organic carbon (SOC) content for qualitative information about soil erosion. The ¹⁰Be boulder exposure ages revealed that the moraines were deposited during the Younger Dryas and the pre Bølling–Allerød episodes of the late Pleistocene. The morphology of the soils suggests a complex history of development and shows that both erosion and aeolian deposition have affected the soils. The ^239+240Pu measurements revealed that erosion rates strongly decrease with time as soils develop. A weakly developed soil (Cambisol) is found on the youngest moraine (11.8 ka) that exhibits an erosion rate, depending on the calculation procedure, in the range of 260 to 520 t km⁻² a⁻¹. With time the erosion rate rapidly decreases to almost zero, presumably as a full vegetation cover develops. Bioturbation and/or dust influx is increasingly obvious with increasing age of the soils, as evidenced by the comparison of δ¹³C and SOC. The mass balance of the oldest soil (15.8 ka) indicates that the slopes have reached a geomorphological stability with little or no net erosion. Aeolian influx appears to be the primary factor to account for mass changes in the oldest soil.