Expedition 382 Preliminary Report: Iceberg Alley and Subantarctic Ice and Ocean Dynamics

• Main Authors: Weber, ME, Raymo, ME, Peck, VL, Williams, T, Armbrecht, L, Bailey, I, Brachfeld, S, Du, Z, Fauth, G, Garcia, M, Gluder, A, Guitard, M, Gutjahr, M, Hemming, S, Hernandez-Almeida, I, Hoem, FS, Hwang, J-H, Lizuka, M, Kato, Y, Lee, BK, Martos, YM, O'Connell, S, Perez, LF, Reilly, B, Ronge, TA, Seki, O, Tauxe, L, Tripathi, S, Warnock, J, Zheng, X
• Format: Article in Journal/Newspaper
• Language: English
• Published: International Ocean Discovery Program 2019
• Subjects: Antarc*; Antarctic; Antarctica; Drake Passage; Ice Sheet; Iceberg*; Scotia Sea
• Online Access: http://hdl.handle.net/10871/123188; https://doi.org/10.14379/iodp.pr.382.2019

This is the final version. Available from International Ocean Discovery Program via the DOI in this record. International Ocean Discovery Program (IODP) Expedition 382, Iceberg Alley and Subantarctic Ice and Ocean Dynamics, investigated the long-term climate history of Antarctica, seeking to understand how polar ice sheets responded to changes in insolation and atmospheric CO2 in the past and how ice sheet evolution influenced global sea level and vice versa. Five sites (U1534–U1538) were drilled east of the Drake Passage: two sites at 53.2°S at the northern edge of the Scotia Sea and three sites at 57.4°–59.4°S in the southern Scotia Sea. We recovered continuously deposited late Neogene sediment to reconstruct the past history and variability in Antarctic Ice Sheet (AIS) mass loss and associated changes in oceanic and atmospheric circulation. The sites from the southern Scotia Sea (Sites U1536–U1538) will be used to study the Neogene flux of icebergs through “Iceberg Alley,” the main pathway along which icebergs calved from the mar- gin of the AIS travel as they move equatorward into the warmer wa- ters of the Antarctic Circumpolar Current (ACC). In particular, sediments from this area will allow us to assess the magnitude of iceberg flux during key times of AIS evolution, including the following: • The middle Miocene glacial intensification of the East Antarctic Ice Sheet, • The mid-Pliocene warm period, • The late Pliocene glacial expansion of the West Antarctic Ice Sheet, • The mid-Pleistocene transition (MPT), and • The “warm interglacials” and glacial terminations of the last 800 ky. We will use the geochemical provenance of iceberg-rafted detritus and other glacially eroded material to determine regional sources of AIS mass loss. We will also address interhemispheric phasing of ice sheet growth and decay, study the distribution and history of land-based versus marine-based ice sheets around the continent over time, and explore the links between AIS variability and global sea level. By comparing ...