Articles | Volume 21, issue 9
https://doi.org/10.5194/cp-21-1661-2025
https://doi.org/10.5194/cp-21-1661-2025
Research article
 | 
23 Sep 2025
Research article |  | 23 Sep 2025

Edisto Inlet as a sentinel for Late Holocene environmental changes over the Ross Sea: insights from foraminifera turnover events

Giacomo Galli, Katrine Elnegaard Hansen, Caterina Morigi, Alessio Di Roberto, Federico Giglio, Patrizia Giordano, and Karen Gariboldi

Viewed

Total article views: 1,330 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,179 110 41 1,330 43 39 50
  • HTML: 1,179
  • PDF: 110
  • XML: 41
  • Total: 1,330
  • Supplement: 43
  • BibTeX: 39
  • EndNote: 50
Views and downloads (calculated since 07 Feb 2025)
Cumulative views and downloads (calculated since 07 Feb 2025)

Viewed (geographical distribution)

Total article views: 1,330 (including HTML, PDF, and XML) Thereof 1,313 with geography defined and 17 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 15 Oct 2025
Download
Short summary
In the Edisto Inlet, Ross Sea, over the last 3.6 kyr, a marked transition at 2.7–2.5 kyr BP occurred. Geochemical proxies and changes in the foraminiferal community suggest a change from multi-year to seasonal sea ice, likely linked to mCDW (modified Circumpolar Deep Water) intrusion. The study integrates ecological information and geochemical data to unveil connections between mCDW, sea-ice conditions and the SAM (Southern Annular Mode) in Edisto, highlighting it as a key site for regional paleoclimate reconstruction over the Ross Sea.
Share