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: Iceland-Scotland Overflow; Oscillation; sediment transport; sediment provenances; grain size end-members; Greenland; Reykjanes; Fennoscandian; Iceland
• Online Access: https://doi.org/10.1029/2019GC008298; http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9053

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...