Articles | Volume 42, issue 2
https://doi.org/10.5194/jm-42-95-2023
https://doi.org/10.5194/jm-42-95-2023
Research article
 | 
13 Sep 2023
Research article |  | 13 Sep 2023

Paleoenvironmental changes related to the variations of the sea-ice cover during the Late Holocene in an Antarctic fjord (Edisto Inlet, Ross Sea) inferred by foraminiferal association

Giacomo Galli, Caterina Morigi, Romana Melis, Alessio Di Roberto, Tommaso Tesi, Fiorenza Torricella, Leonardo Langone, Patrizia Giordano, Ester Colizza, Lucilla Capotondi, Andrea Gallerani, and Karen Gariboldi

Viewed

Total article views: 888 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
654 197 37 888 39 22 24
  • HTML: 654
  • PDF: 197
  • XML: 37
  • Total: 888
  • Supplement: 39
  • BibTeX: 22
  • EndNote: 24
Views and downloads (calculated since 13 Sep 2023)
Cumulative views and downloads (calculated since 13 Sep 2023)

Viewed (geographical distribution)

Total article views: 854 (including HTML, PDF, and XML) Thereof 854 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
A sediment core was analysed, focusing over the 2000 years, in Edisto Inlet. Benthic and planktic foraminifera were picked and used to determine changes in the faunal composition. Using other nearby cores, by comparing different proxies, we were able to identify a succession of three different environmental phases over the studied period: a seasonal-cycle phase (from 2000 to around 1500 years BP), a transitional phase (from 1500 to 700 years BP) and a cold phase (from 700 years to present).