Bottom current control on sediment deposition between the Iselin Bank and the Hillary Canyon (Antarctica) since the late Miocene: An integrated seismic-oceanographic approach

• Published in: Deep Sea Research Part I: Oceanographic Research Papers
• Main Authors: Conte, R., Rebesco, M., De Santis, L., Colleoni, F., Bensi, M., Bergamasco, A., Kovacevic, V., Gales, J., Zgur, F., Accettella, D., De Steur, L., Ursella, L., McKay, R., Kim, S., Lucchi, R.G., Ash, Jeanine, Beny, F., Browne, Imogen, Cortese, Giuseppe, Dodd, Justin P., Esper, Oliver, Harwood, D. M., Ishino, Saki, Keisling, B., Kulhanek, D. K., Laberg, Jan Sverre, Leckie, R. Mark, Müller, Juliane, Patterson, Molly O., Romans, Brian W., Romero, Oscar E., Sangiorgi, Francesca, Seki, Osamu, Shevenell, Amelia E., Singh, Shiv M., Cordeiro de Sousa, Isabela M., Sugisaki, Saiko T., Van De Flierdt, T., van Peer, T. E., Xiao, Whenshen, Xiong, Zhifang
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2021
• Subjects: Antarctic; The Antarctic; Ross Sea; Iselin Bank; Hillary Canyon; Antarc*; Antarctica; Ice Sheet; Ice Shelves; Sea ice
• Online Access: https://epic.awi.de/id/eprint/55948/; https://doi.org/10.1016/j.dsr.2021.103606; https://hdl.handle.net/10013/epic.a961eec2-b2e2-4c14-9622-57877961a76b

In this paper we analyze how oceanic circulation affects sediment deposition along a sector of the Ross Sea continental margin, between the Iselin Bank and the Hillary Canyon, and how these processes evolved since the Late Miocene. The Hillary Canyon is one of the few places around the Antarctic con...