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3D sedimentary architecture showing the inception of an Ice Age

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  • H. Løseth

    (Equinor ASA)

  • J. A. Dowdeswell

    (University of Cambridge)

  • C. L. Batchelor

    (University of Cambridge
    Norwegian University of Science and Technology)

  • D. Ottesen

    (Geological Survey of Norway)

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.

Suggested Citation

  • H. Løseth & J. A. Dowdeswell & C. L. Batchelor & D. Ottesen, 2020. "3D sedimentary architecture showing the inception of an Ice Age," Nature Communications, Nature, vol. 11(1), pages 1-7, December.
  • Handle: RePEc:nat:natcom:v:11:y:2020:i:1:d:10.1038_s41467-020-16776-7
    DOI: 10.1038/s41467-020-16776-7
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