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The Holocene Thermal Maximum around Svalbard, Arctic North Atlantic; molluscs show early and exceptional warmth

Holocene (Sevenoaks), 2018-01, Vol.28 (1), p.65-83

2018

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A new global ice sheet reconstruction for the past 80 000 years

Nature communications, 2021-02, Vol.12 (1), p.1199-1199, Article 1199

2021

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The last Eurasian ice sheets - a chronological database and time-slice reconstruction, DATED-1

Boreas, 2016-01, Vol.45 (1), p.1-45

2016

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The discovery of the Younger Dryas, and comments on the current meaning and usage of the term

Boreas, 2021-01, Vol.50 (1), p.1-5

Mangerud, Jan

2021

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Ice-flow patterns and precise timing of ice sheet retreat across a dissected fjord landscape in western Norway

Quaternary science reviews, 2019-06, Vol.214, p.139-163

2019

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Reply to: Towards solving the missing ice problem and the importance of rigorous model data comparisons

Nature communications, 2022-10, Vol.13 (1), p.6264-6264, Article 6264

2022

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Late Quaternary ice sheet history of northern Eurasia

Quaternary science reviews, 2004-06, Vol.23 (11), p.1229-1271

2004

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Collapse of marine-based outlet glaciers from the Scandinavian Ice Sheet

Quaternary science reviews, 2013-05, Vol.67, p.8-16

2013

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Institutt for geovitenskap ved Universitetet i Bergen, 1896–1963

Norwegian journal of geology, 2024-06

Mangerud, Jan

2024

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Yngre dryas: En uventet klimaendring som formet norsk natur

Naturen, 2023-11, Vol.147 (4-5), p.175-188

Mangerud, Jan

2023

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Evidence of early deglaciation (18 000 cal a bp) and a postglacial relative sea‐level curve from southern Karmøy, south‐west Norway

Journal of quaternary science, 2019-08, Vol.34 (6), p.410-423

2019

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Last interglacial sea-level proxies in the glaciated Northern Hemisphere

Earth system science data, 2022-04, Vol.14 (4), p.1447-1492

2022

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Evidence for three North Sea tsunamis at the Shetland Islands between 8000 and 1500 years ago

Quaternary science reviews, 2005-08, Vol.24 (14), p.1757-1775

2005

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A new global ice sheet reconstruction for the past 80000 years

Nature communications, 2021-02, Vol.12 (1)

2021

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Comments to the paper “A 10Be chronology of the Esmark Moraine and Lysefjorden region, southwestern Norway: Evidence for coeval glacier resurgence in both polar hemispheres during the Antarctic Cold Reversal” by Aron E. Putnam, George H. Denton and Joerg M. Schaefer

Quaternary science reviews, 2024-01, Vol.323, p.108348, Article 108348

2024

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Tracing the last remnants of the Scandinavian Ice Sheet: Ice-dammed lakes and a catastrophic outburst flood in northern Sweden

Quaternary science reviews, 2019-10, Vol.221, p.105862, Article 105862

2019

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THE LAST GLACIAL MAXIMUM OF SVALBARD AND THE BARENTS SEA AREA: ICE SHEET EXTENT AND CONFIGURATION

Quaternary science reviews, 1998, Vol.17 (1), p.43-75

1998

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Tsunami sedimentary facies deposited by the Storegga tsunami in shallow marine basins and coastal lakes, western Norway

Sedimentology, 1997-12, Vol.44 (6), p.1115-1131

1997

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Did the Eurasian ice sheets melt completely in early Marine Isotope Stage 3? New evidence from Norway and a synthesis for Eurasia

Quaternary science reviews, 2023-07, Vol.311, p.108136, Article 108136

2023

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The extent of the Barents–Kara ice sheet during the Last Glacial Maximum

Quaternary science reviews, 2002, Vol.21 (1), p.111-119

2002

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Younger Dryas glaciation of Scandinavia – the type area for the Younger Dryas

Quaternary international, 2012-11, Vol.279-280, p.303-304

Mangerud, Jan

2012

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Persistence of arctic-alpine flora during 24,000 years of environmental change in the Polar Urals

Scientific reports, 2019-12, Vol.9 (1), p.19613-11, Article 19613

2019

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The chronology of a large ice-dammed lake and the Barents–Kara Ice Sheet advances, Northern Russia

Global and planetary change, 2001-11, Vol.31 (1), p.321-336

2001

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Maximum extent of the Eurasian ice sheets in the Barents and Kara Sea region during the Weichselian

Boreas, 1999-03, Vol.28 (1), p.234-242

1999

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Quaternary of Norden

33rd International Geological Congress,Oslo, Norway,2008-08-06 - 2008-08-14, 2008-03, Vol.31 (1), p.73-81

2008

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The Holocene Thermal Maximum around Svalbard, Arctic North Atlantic; molluscs show early and exceptional warmth

A new global ice sheet reconstruction for the past 80 000 years

The last Eurasian ice sheets - a chronological database and time-slice reconstruction, DATED-1

The discovery of the Younger Dryas, and comments on the current meaning and usage of the term

Ice-flow patterns and precise timing of ice sheet retreat across a dissected fjord landscape in western Norway

Reply to: Towards solving the missing ice problem and the importance of rigorous model data comparisons

Late Quaternary ice sheet history of northern Eurasia

Collapse of marine-based outlet glaciers from the Scandinavian Ice Sheet

Institutt for geovitenskap ved Universitetet i Bergen, 1896–1963

Yngre dryas: En uventet klimaendring som formet norsk natur

Evidence of early deglaciation (18 000 cal a bp) and a postglacial relative sea‐level curve from southern Karmøy, south‐west Norway

Last interglacial sea-level proxies in the glaciated Northern Hemisphere

Evidence for three North Sea tsunamis at the Shetland Islands between 8000 and 1500 years ago

A new global ice sheet reconstruction for the past 80000 years

Comments to the paper “A 10Be chronology of the Esmark Moraine and Lysefjorden region, southwestern Norway: Evidence for coeval glacier resurgence in both polar hemispheres during the Antarctic Cold Reversal” by Aron E. Putnam, George H. Denton and Joerg M. Schaefer

Tracing the last remnants of the Scandinavian Ice Sheet: Ice-dammed lakes and a catastrophic outburst flood in northern Sweden

THE LAST GLACIAL MAXIMUM OF SVALBARD AND THE BARENTS SEA AREA: ICE SHEET EXTENT AND CONFIGURATION

Tsunami sedimentary facies deposited by the Storegga tsunami in shallow marine basins and coastal lakes, western Norway

Did the Eurasian ice sheets melt completely in early Marine Isotope Stage 3? New evidence from Norway and a synthesis for Eurasia

The extent of the Barents–Kara ice sheet during the Last Glacial Maximum

Younger Dryas glaciation of Scandinavia – the type area for the Younger Dryas

Persistence of arctic-alpine flora during 24,000 years of environmental change in the Polar Urals

The chronology of a large ice-dammed lake and the Barents–Kara Ice Sheet advances, Northern Russia

Maximum extent of the Eurasian ice sheets in the Barents and Kara Sea region during the Weichselian

Quaternary of Norden

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