Description: We present lithogenic grain-size composition, high-resolution XRF bulk chemistry records, weighted coarse bulk fraction (〉150 μm) and the isotopic record of benthic foraminifera (C.wuellestorfi) of gravity sediment cores P457-905 and P57-909 from the southwestern flank of the Iceland-Faroe Ridge.

Description: We present lithogenic grain-size composition, high-resolution XRF bulk chemistry records, weighted coarse bulk fraction (〉150 μm) and the isotopic record of benthic foraminifera (C.wuellestorfi) of gravity sediment cores P457-909 from the southwestern flank of the Iceland-Faroe Ridge.

Description: We present lithogenic grain-size composition, high-resolution XRF bulk chemistry records, weighted coarse bulk fraction (〉150 μm) and the isotopic record of benthic foraminifera (C.wuellestorfi) of gravity sediment cores P457-905 from the southwestern flank of the Iceland-Faroe Ridge.

Description: Explosive volcanic eruptions on Iceland, even of intermediate magnitude have far-reaching impacts. Their far-distal deposits have been found up to Northern Continental Europe and Greenland. On Iceland, the harsh environment and strongly erosive conditions limit the preservation of volcanic deposits and their accessibility on land. The area offshore southern Iceland preserves information about the depositional fans at medial distance from the volcanic source. Here we use this sedimentary archive to reconstruct the Icelandic eruption record in greater detail. This high resolution geological record allows us to infer eruption frequencies and explosiveness in great detail and contributes to the assessment of Icelandic volcanic hazards, volcano-climate interaction, stratigraphy and palaeoceanographic reconstructions. Eight gravity cores were obtained during RV Poseidon Cruise 457, at 260 to 1,600 m water depths and distances of 130 to 400 km west to southeast of Iceland. The ~4 to 10 m long sediment cores reach back to the Late Pleistocene (~68 ka BP; dated by 14C and sedimentation rates), mostly excluding the Holocene. Potential tephra layers were identified by visual inspection and color scans. Volcanic glass shards were analyzed for their major element composition by electron microprobe and assigned to their eruptive source by geochemical fingerprinting. More than 50 primary tephra layers and nearly as many reworked layers were identified, several of which were correlated across the cores. The mostly basaltic tephra shards are derived from the Katla, Grímsvötn-Lakagígar, Bárðarbunga-Veiðivötn, and Hekla volcanic systems. Primary and mixed layers with particles of unique bimodal composition identical to the ~12 ka BP Vedde-Tephra from the Katla Volcanic System, including rhyolitic particles, were identified in nearly all cores and used as time marker and for inter-core correlation. Tephra layers of unique unknown composition were also identified and stratigraphically assigned across some of the cores. Intercalated dropstones from Heinrich events provide additional age constraints. The core and tephra correlations are supported by color scans, of which the *b-values tie in with the delta18O Greenland Ice-core record. The marine tephrostratigraphy offshore southern Iceland extends the eruption record further back in time than currently inferred from terrestrial Iceland and in more detail than far-distant deposits. It provides depositional evidence for previously unrecognized eruptions and demonstrates that Icelandic volcanoes erupted more often than previously thought. The depositional time frame of the tephra layers in the cores facilitates to integrate climatically-induced variations in sedimentation rates and conditions at the different sites around Iceland with changes in eruption frequency.

Description: 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 with Dansgaard‐Oeschger cycles and deglacial perturbations of the Atlantic Meridional Overturning Circulation (AMOC). The transition between Greenland Stadials (GSs) and Greenland Interstadials (GIs) follows a distinct, recurring sedimentation pattern. Basaltic (Ti‐rich) silts were transported from local volcanic sources by strong bottom currents and deposited during GIs comparable to modern ocean circulation. Finer‐grained felsic (K‐rich) sediments were deposited during GSs, when ISOW was weak. Possible felsic source areas include British‐Ireland and/or Fennoscandian shelf areas. A cyclic saw‐tooth pattern of bottom current strength is characterized by gradual intensification during GIs followed by a sharp decline towards GSs as is documented at core sites along the flank of Reykjanes Ridge. The cores north of Faroe Channel instead document the opposite pattern. This suggests that the near‐bottom currents along the Reykjanes Ridge are strongly controlled by the flow cascading over the IFR. Heinrich (like) Stadials (HSs) especially HS‐1 and HS‐2 are characterized by the deposition of very fine felsic sediments pointing to weakened bottom currents. Distinct coarse‐grained intervals of ice rafted debris (IRD) are absent from the sediment records, although pebble and gravel sized IRD is irregularly distributed throughout the fine sediment matrix. Near bottom currents are considered to have a major control on the lithogenic sediment deposition southwest of the Iceland‐Faroe Ridge and further down‐stream.