Earth Surface Dynamics
Earth Surface Dynamics
ESurf
Articles | Volume 6, issue 2
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.
https://doi.org/10.5194/esurf-6-329-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 6, issue 2
Research article
 | 
07 May 2018
Research article |  | 07 May 2018

Tracking the 10Be–26Al source-area signal in sediment-routing systems of arid central Australia

Martin Struck, John D. Jansen, Toshiyuki Fujioka, Alexandru T. Codilean, David Fink, Réka-Hajnalka Fülöp, Klaus M. Wilcken, David M. Price, Steven Kotevski, L. Keith Fifield, and John Chappell

Viewed

Total article views: 4,646 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,280 1,222 144 4,646 735 117 157
  • HTML: 3,280
  • PDF: 1,222
  • XML: 144
  • Total: 4,646
  • Supplement: 735
  • BibTeX: 117
  • EndNote: 157
Views and downloads (calculated since 16 Jan 2018)
Cumulative views and downloads (calculated since 16 Jan 2018)

Viewed (geographical distribution)

Total article views: 4,646 (including HTML, PDF, and XML) Thereof 4,399 with geography defined and 247 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 08 Nov 2025
Download
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.
Read more
Share