Evidence for an Ice Shelf Covering the Central Arctic Ocean During the Penultimate Glaciation

TitleEvidence for an Ice Shelf Covering the Central Arctic Ocean During the Penultimate Glaciation
Publication TypeJournal Article
Year2016
AuthorsJakobsson, M, Nilsson, J, Anderson, L, Backman, J, Bjork, G, Cronin, T, Kirchner, N, Koshurnikov, A, Mayer, LA, Noormets, R, O'Regan, MA, Stranne, C, Ananiev, R, Barrientos, N, Chernykh, D, Coxall, H, Eriksson, B, Floden, T, Gemery, L, Gustafson, O, Jerram, K, Johansson, C, Khortov, A, Mohammad, R, Semiltov, I
JournalNature Communications
Volume7
Date PublishedJanuary 18
PublisherMacmillan Publishers Ltd.
KeywordsArctic Ocean, glaciation, ice shelf

The hypothesis of a km-thick ice shelf covering the entire Arctic Ocean during peak glacial conditions was proposed nearly half a century ago. Floating ice shelves preserve few direct traces after their disappearance, making reconstructions difficult. Seafloor imprints of ice shelves should, however, exist where ice grounded along their flow paths. Here we present new evidence of ice-shelf groundings on bathymetric highs in the central Arctic Ocean, resurrecting the concept of an ice shelf extending over the entire central Arctic Ocean during at least one previous ice age. New and previously mapped glacial landforms together reveal flow of a spatially coherent, in some regions >1-km thick, central Arctic Ocean ice shelf dated to marine isotope stage 6 (~140 ka). Bathymetric highs were likely critical in the ice-shelf development by acting as pinning points where stabilizing ice rises formed, thereby providing sufficient back stress to allow ice shelf thickening.

Publication Linkhttp://www.nature.com/ncomms/2016/160118/ncomms10365/full/ncomms10365.html
DOI10.1038/ncomms10365
Refereed DesignationRefereed
Region