Environmental and Oceanographic Conditions at the Continental Margin of the Central Basin, Northwestern Ross Sea (Antarctica) Since the Last Glacial Maximum

The continental margin is a key area for studying the sedimentary processes related to the advance and retreat of the Ross Ice Shelf (Antarctica); nevertheless, much remains to be investigated. The aim of this study is to increase the knowledge of the last glacial/deglacial dynamics in the Central B...

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Bibliographic Details
Published in:Geosciences
Main Authors: Fiorenza Torricella, Romana Melis, Elisa Malinverno, Giorgio Fontolan, Mauro Bussi, Lucilla Capotondi, Paola Del Carlo, Alessio Di Roberto, Andrea Geniram, Gerhard Kuhn, Boo-Keun Khim, Caterina Morigi, Bianca Scateni, Ester Colizza
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
diatoms
micropaleontology
sedimentology
cryptotephra
LGM to Holocene
Central Basin
Geology
QE1-996.5
Mount Rittmann
Rittmann
Ross Ice Shelf
Ross Sea
Antarc*
Antarctica
Ice Shelf
Sea ice
Online Access:https://doi.org/10.3390/geosciences11040155
https://doaj.org/article/1daaceba55fa46198a8306019ba9451d
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Summary:The continental margin is a key area for studying the sedimentary processes related to the advance and retreat of the Ross Ice Shelf (Antarctica); nevertheless, much remains to be investigated. The aim of this study is to increase the knowledge of the last glacial/deglacial dynamics in the Central Basin slope–basin system using a multidisciplinary approach, including integrated sedimentological, micropaleontological and tephrochronological information. The analyses carried out on three box cores highlighted sedimentary sequences characterised by tree stratigraphic units. Collected sediments represent a time interval from 24 ka Before Present (BP) to the present time. Grain size clustering and data on the sortable silt component, together with diatom, silicoflagellate and foraminifera assemblages indicate the influence of the ice shelf calving zone (Unit 1, 24–17 ka BP), progressive receding due to Circumpolar Deep Water inflow (Unit 2, 17–10.2 ka BP) and (Unit 3, 10.2 ka BP–present) the establishment of seasonal sea ice with a strengthening of bottom currents. The dominant and persistent process is a sedimentation controlled by contour currents, which tend to modulate intensity in time and space. A primary volcanic ash layer dated back at around 22 ka BP is correlated with the explosive activity of Mount Rittmann.

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