3D sedimentary architecture showing the inception of an Ice Age

• Main Authors: Løseth, H., Dowdeswell, J. A., Batchelor, C. L., Ottesen, D.
• Format: Text
• Language: unknown
• Published: Apollo - University of Cambridge Repository 2020
• Subjects: Article; /704/106/413; /704/2151/213; /704/2151/213/4116; /704/2151/215; /134; /123; article; Ice Sheet; Northeast Atlantic
• Online Access: https://dx.doi.org/10.17863/cam.71236; https://www.repository.cam.ac.uk/handle/1810/323778

Abstract: Northeast Atlantic climate shifted into the Quaternary Ice Age around 2.6 M yr ago. Until now, however, the detailed changes associated with this inception of an Ice Age have remained obscure. New high-quality three-dimensional seismic data reveal a detailed geological record of buried surfaces, landforms and sedimentary architecture over vast parts of the Norwegian North Sea. Here, we show the sequence of near-coast geological events spanning the Northeast Atlantic inception of an Ice Age. We identify the location of immediate pre-glacial fluvially derived sandy systems where rivers from the Norwegian mainland built marine deltas. The stratigraphic position of a large submarine channel, formed by enhanced meltwater from initial build-up of local glaciers, is also shown. Finally, we document the transition to full ice-sheet growth over Scandinavia from the ice sheet’s earliest position to the later pattern of debris-flow lobes reaching the present-day shelf edge.