Hodell, DavidGersonde, RainerBlum, PeterAndersson, E. C.Austin, W.Billups, K.Channell, J.Diekmann, B.Filippelli, G.Flores, J. A.Hewitt, T.Howard, W.Ikehara, M.Janecek, T.Kanfoush, S.Kemp, A.Kleiven, H.Kuhn, G.Marino, M.Ninnemann, U.O'Connell, S.Ortiz, J.Stoner, J.Sugiyama, K.Warnke, D.Zielinski, U.2025-05-302025-05-301816-8957RIS:urn:704E67C41C4425F9D5B49629814EE5E8RIS:4299ORCID:/0000-0003-0714-9994/work/184757381http://www.scopus.com/inward/record.url?eid=2-s2.0-0032427733&partnerID=40https://hdl.handle.net/1885/733754624Leg 177 marked the return of the JOIDES Resolution to the Southern Ocean after more than a decade, and the successful recovery of a superb suite of cores has significantly improved the latitudinal and bathymetric coverage of drilled-ocean sites in the high-latitude Southern Hemisphere. These cores will be used as the raw material for investigating the role of the Southern Ocean in millennial-scale climate variability, glacial/interglacial cycles of the Plio-Pleistocene, and the longterm evolution of the Antarctic ocean-cryosphere system during the Cenozoic.en©1998 The authors19980032427733