Synchronous Changes in Sediment Transport and Provenance at the Iceland-Faroe Ridge Linked to Millennial Climate Variability From 55 to 6 ka BP

• Published in: Geochemistry, Geophysics, Geosystems
• Main Authors: Mirzaloo, M., Nürnberg, D., Kienast, M., van der Lubbe, H. J.L.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2019
• Subjects: grain size end-members; Iceland-Scotland Overflow; Oscillation; sediment provenances; sediment transport; /dk/atira/pure/sustainabledevelopmentgoals/life_below_water; name=SDG 14 - Life Below Water; Greenland; Reykjanes; Fennoscandian; Iceland
• Online Access: https://research.vu.nl/en/publications/9ad2b521-1973-4357-98e9-edb2ac3d5fc7; https://doi.org/10.1029/2019GC008298; https://hdl.handle.net/1871.1/9ad2b521-1973-4357-98e9-edb2ac3d5fc7; http://www.scopus.com/inward/record.url?scp=85070897237&partnerID=8YFLogxK; http://www.scopus.com/inward/citedby.url?scp=85070897237&partnerID=8YFLogxK

Unique marine sediment cores retrieved from the southwestern slope of the Iceland-Faroe Ridge (IFR), close to the main axis of the Iceland-Scotland Overflow Water (ISOW), revealed prominent sedimentary cycles reflecting near-bottom current dynamics, sediment transport, and deposition, coincident wit...