CHANGES IN CATCHMENT DYNAMICS IN A RETREATING WORLD: HIGH RESOLUTION PROVENANCE ANALYSIS FROM DETRITAL APATITE

Glacial retreat quickly and dramatically changes erosion dynamics across catchments. As ice retreats, newly exposed valley walls and sediment can become the target of hillslope and fluvial erosion that in turn can significantly increase fluxes downstream. These increases have important implications for hydropower generation and water quality, presenting risks to biodiversity, ecosystem stability, and human inhabitants. Determining the source of sediment, and what parts of catchments are experiencing the greatest erosion, requires the ability to trace exactly where sediment is derived in the catchment.

Recent analytical advances in the dating of apatite have improved its utility as a provenance tool. The advent of LA-ICP-MS techniques now allow thermochronometric, geochronometric, and chemical data to be collected from each individual grain of a detrital sample. This allows us to trace sediment sources across a glaciated catchment based on lithology and source-rock elevation. In this work, samples were collected across the Bugaboo Glacier catchment, Western Canada, where ice has retreated >2 km in the last century. Detrital samples were collected from the outwash river and two moraine locations, coupled with bedrock from varying elevations. Bedrock samples encompass the catchment’s two principal lithologies, a Cretaceous granitic intrusion, and Neoproterozoic metasediments. Thermochronometric dates range from 41.4 Ma at the highest elevation to 23.9 Ma at the lowest, while geochronometric dates range 68.7–151.3 Ma in granites to 90.5–1952 Ma in metasediments. Chemical data help to highlight key differences between the lithologies.

Detrital mixture models and multi-dimensional scaling suggest moraine samples are composed of sediment derived from a wide range of elevations within the catchment, while the sediments of the modern outwash river appear to be derived entirely from erosion of these moraines, left exposed by retreating ice. This suggests the widely documented increase in sediment flux during glacial retreat is primarily driven by the erosion of newly exposed unconsolidated moraines in catchments. Moreover, we show that multi-method analysis of detrital apatite can be a highly accurate provenance tool in glacial catchment studies.