Sedimentary proxies for Pacific water inflow through the Herald Canyon, western Arctic Ocean

Pacific water inflow to the Arctic Ocean occurs through the shallow Bering Strait. With a present sill depth of only 53 m, this gateway has been frequently closed during glacial sea-level low stands of the Pleistocene. Here, we investigate the sedimentological and mineralogical response to sea-level...

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Bibliographic Details
Published in:arktos
Main Authors: Swärd, Henrik, O’Regan, Matt, Pearce, Christof, Semiletov, Igor, Stranne, Christian, Tarras, Henrik, Jakobsson, Martin
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://pure.au.dk/portal/da/publications/sedimentary-proxies-for-pacific-water-inflow-through-the-herald-canyon-western-arctic-ocean(df8ce454-b075-4e74-b9e5-2675f17f25a0).html
https://doi.org/10.1007/s41063-018-0055-x
https://pure.au.dk/ws/files/140336284/Sw_rd2018_Article_SedimentaryProxiesForPacificWa.pdf