University of Wollongong Research Online Faculty of Science, Medicine and Health - Papers Faculty of Science, Medicine and Health 2014 Age and weathering rate of sediments in small catchments: the role of hillslope erosion Anthony Dosseto University of Wollongong,
[email protected] Heather L. Buss University of Bristol Francois Chabaux University of Strasbourg Publication Details Dosseto, A., Buss, H. L. & Chabaux, F. (2014). Age and weathering rate of sediments in small catchments: the role of hillslope erosion. Geochimica et Cosmochimica Acta, 132 238-258. Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library:
[email protected] Age and weathering rate of sediments in small catchments: the role of hillslope erosion Abstract Uranium-series (U-series) isotopes in river material can be used to determine quantitative time constraints on the transfer of erosion products from source to sink. In this study, we investigate the U-series isotope composition of river-borne material in small catchments of Puerto Rico and southeastern Australia in order to improve our understanding of (i) the controls on the U-series isotope composition of river-borne material and (ii) how erosion products acquire their geochemical characteristics. In both regions, thorium isotopes track the origin of sediment and dissolved loads. Stream solutes are mainly derived from the deepest part of the weathering profile, whereas stream sediments originate from much shallower horizons, even in landslide- dominated Puerto Rican catchments. This suggests that in environments where thick weathering profiles have developed, solutes and sediments have distinct origins.