Relationship between magnetic susceptibility and sediment grain size since the last glacial period in the Southern Ocean off the northern Antarctic Peninsula – Linkages between the cryosphere and atmospheric circulation

• Published in: Palaeogeography, palaeoclimatology, palaeoecology Vol. 505; pp. 359 - 370
• Main Authors: Kim, Sunghan, Yoo, Kyu-Cheul, Lee, Jae Il, Lee, Min Kyung, Kim, Kitae, Yoon, Ho Il, Moon, Heung Soo
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 15.09.2018
• Subjects: Grain size; Ice-rafted debris; Magnetic susceptibility; Southern ocean; The last glacial period; Grain size; Ice-rafted debris; Southern ocean; The last glacial period; Magnetic susceptibility
• DOI: 10.1016/j.palaeo.2018.06.016
• ISSN: 0031-0182

Magnetic susceptibility (MS) values in Scotia Sea sediments showed strong correlations to ice core non-sea salt Ca2+ concentration (dust input), which emphasizes the role of atmospheric circulation in the Southern Ocean. As a result, the correlation between these values was suggested as a powerful tool for age reconstruction of marine sediments in the Southern Ocean. However, controls on MS variation in Scotia Sea sediments are not clear. In this study, we documented records of grain size, MS values (10−6 CGS/g) of bulk sediments, and MS values of sand-sized (>63 μm), coarse silt-sized (16–63 μm), and fine sediment fractions (<16 μm) at sediment cores from the Southern Ocean off the northern Antarctic Peninsula (the south Scotia Sea and the northern Powell Basin) to reveal which size fraction is responsible for increased MS values during the glacial period and how this size fraction is transported to the Southern Ocean deep-sea. The MS values of all cores GC02-SS02, GC03-C2, GC03-C4, and GC04-G03 increased along with increased sand- and coarse silt-sized fractions and decreased fine sediment fraction. Although The MS values of all size fractions increased during the glacial period, the increased glacial MS values are more related to fine sand- to coarse silt-sized fractions than they are to the fine sediment fraction. The fine sand- to coarse silt-sized sediments with the highest MS values during the glacial period show (semi-)normal distribution patterns, indicating that they are transported by the same mechanism. The sediments are considered to be transported as ice rafted debris (IRD) during the glacial period. Based on our record, the strong correlation between marine core MS values and ice core dust record thus suggests a strong linkage between the cryosphere (iceberg calving activity) and atmospheric circulation (dust) in the Southern Ocean off the northern Antarctic Peninsula. •Magnetic susceptibility (MS) variation is related to fine sand to coarse silt grain input.•Fine sand-coarse silt fractions have higher MS values than that of fine sediments.•Fine sand-coarse silt fractions during the glacial period are transported as ice rafted debris.•Iceberg calving activity was active at the margin of ice shelf during the glacial period.•Cryosphere and atmospheric circulation is coupled in the Southern Ocean.