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Abstract We report a comprehensive inventory of Be-based basin-wide denudation rates (n = 160) and Al/ Be ratios (n = 67) from 48 drainage basins along a 3000 km stretch of the East Australian passive continental margin. We provide data from both basins draining east of the continental divide (n = 37) and discharging into the Tasman and Coral Seas, and from basins draining to the west as part of the larger Murray-Darling and Lake Eyre river systems (n = 11). Be-derived denudation rates in mainstem samples from east-draining basins range between 7.7 ± 1.9 (± 1σ; Mary) and 54.6 ± 13.7 mm kyr (North Johnstone). Denudation rates in tributary samples range between 3.0 ± 0.7 (Burdekin) and 70.2 ± 18.9 mm kyr (Liverpool). For west-draining basins, denudation rates are overall lower and with a more restricted range of 4.8 ± 1.2 (Barcoo) to 15.4 ± 3.6 mm kyr (Maranoa) in mainstem samples, and between 4.4 ± 1.0 (Murrumbidgee) and 38.5 ± 7.8 mm kyr (Murray) in tributary sample

Lake eyreSouth australiaWestern australiaBeast australianCoral seasNorth johnstoneOsmogenic be 10Osmogenic al be 26 10Great dividing rangeAssive continental marginஏரி கண்தெற்கு ஆஸ்திரேலியாமேற்கு ஆஸ்திரேலியாகிழக்கு ஆஸ்திரேலியபவளம் கடல்கள்வடக்கு ஜான்ஸ்டோன்