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...
Published in: | arktos |
---|---|
Main Authors: | , , , , , , |
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 |