Articles | Volume 20, issue 7
https://doi.org/10.5194/tc-20-3739-2026
https://doi.org/10.5194/tc-20-3739-2026
Research article
 | 
02 Jul 2026
Research article |  | 02 Jul 2026

Last Glacial Maximum extent and subsequent retreat of the East Antarctic Ice Sheet from the Mac. Robertson Shelf

Janina Güntzel, Juliane Müller, Ralf Tiedemann, Gesine Mollenhauer, Lester Lembke-Jene, Estella Weigelt, Lasse Schopen, Niklas Wesch, Laura Kattein, Andrew N. Mackintosh, and Johann P. Klages

Viewed

Total article views: 13,184 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
11,349 1,593 242 13,184 354 317 345
  • HTML: 11,349
  • PDF: 1,593
  • XML: 242
  • Total: 13,184
  • Supplement: 354
  • BibTeX: 317
  • EndNote: 345
Views and downloads (calculated since 10 Jul 2025)
Cumulative views and downloads (calculated since 10 Jul 2025)

Viewed (geographical distribution)

Total article views: 13,184 (including HTML, PDF, and XML) Thereof 13,163 with geography defined and 21 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 22 Jul 2026
Download
Short summary
Combined multi-proxy sediment core analyses and bathymetry data reveal the deglaciation along the Mac. Robertson Shelf, a yet insufficiently studied sector of the East Antarctic margin. Grounding line extent towards the continental shelf break prior to ~12.7 cal. ka BP and subsequent episodic mid-shelf retreat until the early Holocene prevented Dense Shelf Water formation in its current form, hence suggesting a different formation mechanism under such full glacial conditions.
Share