Environmental and oceanographic conditions at the continental margin of the central basin, northwestern ross sea (antarctica) since the last glacial maximum

• Published in: Geosciences
• Main Authors: Torricella F., Melis R., Malinverno E., Fontolan G., Bussi M., Capotondi L., Del Carlo P., Di Roberto A., Geniram A., Kuhn G., Khim B. -K., Morigi C., Scateni B., Colizza E.
• Other Authors: Torricella, F, Melis, R, Malinverno, E, Fontolan, G, Bussi, M, Capotondi, L, Del Carlo, P, Di Roberto, A, Geniram, A, Kuhn, G, Khim, B, Morigi, C, Scateni, B, Colizza, E
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2021
• Subjects: Antarctica; Central basin; Cryptotephra; Diatom; LGM to Holocene; Micropaleontology; Sedimentology; Western ross sea; Settore GEOS-02/A - Paleontologia e paleoecologia; Settore GEOS-02/B - Geologia stratigrafica e sedimentologia; Central Basin; Mount Rittmann; Rittmann; Ross Ice Shelf; Ross Sea; Antarc*; Ice Shelf; Sea ice
• Online Access: http://hdl.handle.net/10281/313772; https://doi.org/10.3390/geosciences11040155

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...