TY - JOUR
T1 - Arctic Ocean glacial history
AU - Jakobsson, Martin
AU - Andreassen, Karin
AU - Bjarnadóttir, Lilja Rún
AU - Dove, Dayton
AU - Dowdeswell, Julian A.
AU - England, John H.
AU - Funder, Svend
AU - Hogan, Kelly
AU - Ingólfsson, Ólafur
AU - Jennings, Anne
AU - Krog-Larsen, Nikolaj
AU - Kirchner, Nina
AU - Landvik, Jon Y.
AU - Mayer, Larry
AU - Mikkelsen, Naja
AU - Möller, Per
AU - Niessen, Frank
AU - Nilsson, Johan
AU - O'Regan, Matt
AU - Polyak, Leonid
AU - Nørgaard-Pedersen, Niels
AU - Stein, Ruediger
N1 - Funding Information:
Financial support to M. Jakobsson and M. O'Regan was received from the Knut and Alice Wallenberg Foundation (KAW) and the Swedish Research Council (VR). Stockholm University scientists are affiliated with the Bolin Centre for Climate Research, supported through a grant from FORMAS . The Research Council of Norway grant 20067 provided funding for K. Andreassen. For four decades J. England's research group in the Canadian Arctic Archipelago has been supported by an NSERC Discovery Grant , an NSERRC Northern Research Chair (2002–2012), and additional grants from the Canadian Circumpolar Institute, University of Alberta . Full logistical support to stage field camps throughout this remote region was provided during this same interval by the Polar Continental Shelf Program, NRCan. Funding for marine research north and east of Svalbard (J.A. Dowdeswell, K. Hogan) was provided by UK Natural Environment Research Council Grant NER/T/S/2003/00318 to Dowdeswell. Dayton Dove publishes with the permission of the Executive Director of the British Geological Survey. We are grateful for the comprehensive and insightful comments provided by two anonymous reviewers.
PY - 2014/5/15
Y1 - 2014/5/15
N2 - While there are numerous hypotheses concerning glacial-interglacial environmental and climatic regime shifts in the Arctic Ocean, a holistic view on the Northern Hemisphere's late Quaternary ice-sheet extent and their impact on ocean and sea-ice dynamics remains to be established. Here we aim to provide a step in this direction by presenting an overview of Arctic Ocean glacial history, based on the present state-of-the-art knowledge gained from field work and chronological studies, and with a specific focus on ice-sheet extent and environmental conditions during the Last Glacial Maximum (LGM). The maximum Quaternary extension of ice sheets is discussed and compared to LGM. We bring together recent results from the circum-Arctic continental margins and the deep central basin; extent of ice sheets and ice streams bordering the Arctic Ocean as well as evidence for ice shelves extending into the central deep basin. Discrepancies between new results and published LGM ice-sheet reconstructions in the high Arctic are highlighted and outstanding questions are identified. Finally, we address the ability to simulate the Arctic Ocean ice sheet complexes and their dynamics, including ice streams and ice shelves, using presently available ice-sheet models. Our review shows that while we are able to firmly reject some of the earlier hypotheses formulated to describe Arctic Ocean glacial conditions, we still lack information from key areas to compile the holistic Arctic Ocean glacial history.
AB - While there are numerous hypotheses concerning glacial-interglacial environmental and climatic regime shifts in the Arctic Ocean, a holistic view on the Northern Hemisphere's late Quaternary ice-sheet extent and their impact on ocean and sea-ice dynamics remains to be established. Here we aim to provide a step in this direction by presenting an overview of Arctic Ocean glacial history, based on the present state-of-the-art knowledge gained from field work and chronological studies, and with a specific focus on ice-sheet extent and environmental conditions during the Last Glacial Maximum (LGM). The maximum Quaternary extension of ice sheets is discussed and compared to LGM. We bring together recent results from the circum-Arctic continental margins and the deep central basin; extent of ice sheets and ice streams bordering the Arctic Ocean as well as evidence for ice shelves extending into the central deep basin. Discrepancies between new results and published LGM ice-sheet reconstructions in the high Arctic are highlighted and outstanding questions are identified. Finally, we address the ability to simulate the Arctic Ocean ice sheet complexes and their dynamics, including ice streams and ice shelves, using presently available ice-sheet models. Our review shows that while we are able to firmly reject some of the earlier hypotheses formulated to describe Arctic Ocean glacial conditions, we still lack information from key areas to compile the holistic Arctic Ocean glacial history.
KW - Arctic Ocean
KW - Glacial history
KW - Ice sheet modelling
KW - Ice sheets
KW - Ice shelves
KW - Ice streams
KW - Landforms
KW - Last Glacial Maximum
KW - Paleoceanography
KW - Quaternary
UR - http://www.scopus.com/inward/record.url?scp=84900401951&partnerID=8YFLogxK
U2 - 10.1016/j.quascirev.2013.07.033
DO - 10.1016/j.quascirev.2013.07.033
M3 - Article
SN - 0277-3791
VL - 92
SP - 40
EP - 67
JO - Quaternary Science Reviews
JF - Quaternary Science Reviews
ER -