S
Stein Bondevik
Researcher at Bergen University College
Publications - 40
Citations - 2711
Stein Bondevik is an academic researcher from Bergen University College. The author has contributed to research in topics: Holocene & Sea level. The author has an hindex of 24, co-authored 39 publications receiving 2546 citations. Previous affiliations of Stein Bondevik include University of Washington & University of Bergen.
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The last glacial maximum of svalbard and the barents sea area: ice sheet extent and configuration
Jon Y. Landvik,Stein Bondevik,Anders Elverhøi,Willy Fjeldskaar,Jan Mangerud,Otto Salvigsen,Martin J. Siegert,John Inge Svendsen,Tore O. Vorren +8 more
TL;DR: This paper reviewed the geological observations and interpretations regarding the size and timing of the Late Weichselian Barents ice sheet, combined with numerical modelling of its formation in order to produce a reconstruction of ice sheet extent and behaviour.
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The Storegga Slide tsunami—comparing field observations with numerical simulations
Stein Bondevik,Finn Løvholt,Carl B. Harbitz,Jan Mangerud,Alastair G. Dawson,John Inge Svendsen +5 more
TL;DR: A good agreement was obtained for a retrogressive slide that descends at 25-30m/s, and that has short time lags of 15-20 s between each individual slide-block as mentioned in this paper.
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Tsunami sedimentary facies deposited by the Storegga tsunami in shallow marine basins and coastal lakes, western Norway
TL;DR: In this paper, an erosional unconformity underlies the tsunami facies and is traced throughout the basins, with most erosion found at the seaward portion of the lakes.
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Marine 14C reservoir ages for 19th century whales and molluscs from the North Atlantic
TL;DR: In this paper, the authors present reservoir ages from dating 21 whales collected 1860-1901 and recalculating dates of 23 molluscs collected 1857-1926.
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Changes in North Atlantic radiocarbon reservoir ages during the Allerod and Younger Dryas
TL;DR: Radiocarbon age difference between the shells and the plants showed that sea surface reservoir ages increased from 400 to 600 years in the early YD, stabilized for 900 years, and dropped by 300 years within a century across the YD-Holocene transition.