Articles | Volume 6, issue 2
https://doi.org/10.5194/esurf-6-329-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-6-329-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
07 May 2018
Research article |
| 07 May 2018
| 07 May 2018
Tracking the 10Be–26Al source-area signal in sediment-routing systems of arid central Australia
School of Earth and Environmental Sciences, University of Wollongong, Wollongong 2522, Australia
John D. Jansen
Department of Geoscience, Aarhus University, 8000 Aarhus C, Denmark
Toshiyuki Fujioka
Australian Nuclear Science and Technology Organisation, Lucas Heights 2234, Australia
Alexandru T. Codilean
School of Earth and Environmental Sciences, University of Wollongong, Wollongong 2522, Australia
David Fink
Australian Nuclear Science and Technology Organisation, Lucas Heights 2234, Australia
Réka-Hajnalka Fülöp
School of Earth and Environmental Sciences, University of Wollongong, Wollongong 2522, Australia
Australian Nuclear Science and Technology Organisation, Lucas Heights 2234, Australia
Klaus M. Wilcken
Australian Nuclear Science and Technology Organisation, Lucas Heights 2234, Australia
David M. Price
School of Earth and Environmental Sciences, University of Wollongong, Wollongong 2522, Australia
Steven Kotevski
Australian Nuclear Science and Technology Organisation, Lucas Heights 2234, Australia
L. Keith Fifield
Research School of Earth Sciences, Australian National University, Canberra 0200, Australia
John Chappell
Research School of Earth Sciences, Australian National University, Canberra 0200, Australia
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Cited
15 citations as recorded by crossref.
- Geomorphic imprints of lithospheric flexure in central Australia J. Jansen et al. 10.1016/j.epsl.2022.117456
- Exploring exogenous controls on short- versus long-term erosion rates globally S. Chen et al. 10.5194/esurf-10-1055-2022
- In situ-produced cosmogenic krypton in zircon and its potential for Earth surface applications T. Dunai et al. 10.5194/gchron-4-65-2022
- Geochemical methods to infer landscape response to Quaternary climate change and land use in depositional archives: A review A. Francke et al. 10.1016/j.earscirev.2020.103218
- Erosional Response to Pleistocene Climate Changes in the Brazilian Highlands V. Godard et al. 10.1029/2024JF007671
- A global rate of denudation from cosmogenic nuclides in the Earth's largest rivers H. Wittmann et al. 10.1016/j.earscirev.2020.103147
- Effects of long soil surface residence times on apparent cosmogenic nuclide denudation rates and burial ages in the Cradle of Humankind, South Africa T. Makhubela et al. 10.1002/esp.4723
- Optimising global landscape evolution models with 10Be G. Ruetenik et al. 10.5194/esurf-11-865-2023
- Constraints on what controls millennial-scale basin-wide denudation across mountain belts, Asia Y. Yang et al. 10.1007/s11430-024-1420-8
- 26Al and 10Be concentrations from alluvial drill cores across the Indo-Gangetic plain reveal multimillion-year sediment-transport lag times S. Bhattacharjee et al. 10.1016/j.epsl.2023.118318
- Fluvial dynamics and 14C‐10Be disequilibrium on the Bolivian Altiplano K. Hippe et al. 10.1002/esp.4529
- Controls on denudation along the East Australian continental margin A. Codilean et al. 10.1016/j.earscirev.2021.103543
- 26Al/10Be ratios reveal the source of river sediments in the Kimberley, NW Australia G. Cazes et al. 10.1002/esp.4744
- The age of dust—A new hydrological indicator in arid environments? S. Turner et al. 10.1130/G48592.1
- Pre-development denudation rates for the Great Barrier Reef catchments derived using 10Be A. Mariotti et al. 10.1016/j.marpolbul.2021.112731
15 citations as recorded by crossref.
- Geomorphic imprints of lithospheric flexure in central Australia J. Jansen et al. 10.1016/j.epsl.2022.117456
- Exploring exogenous controls on short- versus long-term erosion rates globally S. Chen et al. 10.5194/esurf-10-1055-2022
- In situ-produced cosmogenic krypton in zircon and its potential for Earth surface applications T. Dunai et al. 10.5194/gchron-4-65-2022
- Geochemical methods to infer landscape response to Quaternary climate change and land use in depositional archives: A review A. Francke et al. 10.1016/j.earscirev.2020.103218
- Erosional Response to Pleistocene Climate Changes in the Brazilian Highlands V. Godard et al. 10.1029/2024JF007671
- A global rate of denudation from cosmogenic nuclides in the Earth's largest rivers H. Wittmann et al. 10.1016/j.earscirev.2020.103147
- Effects of long soil surface residence times on apparent cosmogenic nuclide denudation rates and burial ages in the Cradle of Humankind, South Africa T. Makhubela et al. 10.1002/esp.4723
- Optimising global landscape evolution models with 10Be G. Ruetenik et al. 10.5194/esurf-11-865-2023
- Constraints on what controls millennial-scale basin-wide denudation across mountain belts, Asia Y. Yang et al. 10.1007/s11430-024-1420-8
- 26Al and 10Be concentrations from alluvial drill cores across the Indo-Gangetic plain reveal multimillion-year sediment-transport lag times S. Bhattacharjee et al. 10.1016/j.epsl.2023.118318
- Fluvial dynamics and 14C‐10Be disequilibrium on the Bolivian Altiplano K. Hippe et al. 10.1002/esp.4529
- Controls on denudation along the East Australian continental margin A. Codilean et al. 10.1016/j.earscirev.2021.103543
- 26Al/10Be ratios reveal the source of river sediments in the Kimberley, NW Australia G. Cazes et al. 10.1002/esp.4744
- The age of dust—A new hydrological indicator in arid environments? S. Turner et al. 10.1130/G48592.1
- Pre-development denudation rates for the Great Barrier Reef catchments derived using 10Be A. Mariotti et al. 10.1016/j.marpolbul.2021.112731
Latest update: 14 Dec 2024
Short summary
Measurements of cosmogenic nuclides 10Be and 26Al in sediment along central Australian streams show that lithologically controlled magnitudes of source-area erosion rates (0.2–11 m Myr-1) are preserved downstream despite sediment mixing. Conversely, downstream-increasing sediment burial signals (> 400 kyr) indicate sediment incorporation from adjacent, long-exposed storages, which, combined with low sediment supply and discontinuous flux, likely favours source-area 10Be–26Al signal masking.
Measurements of cosmogenic nuclides 10Be and 26Al in sediment along central Australian streams...
