Late Pliocene and early Pleistocene rock-magnetic record of IODP Site 306-U1314 ...

• Main Authors: Sato, Masahiko, Makio, Masato, Hayashi, T, Ohno, Masao
• Format: Dataset
• Language: English
• Published: PANGAEA 2015
• Subjects: DEPTH, sediment/rock; AGE; High-coerecivity component; Low-coerecivity component; Residual; Isothermal Remanent Magnetization, intensity; Isothermal Remanent Magnetization, mode of gradient; Isothermal Remanent Magnetization, median of gradient; Isothermal Remanent Magnetization, mean of gradient; Composite Core; Exp306; Joides Resolution; Integrated Ocean Drilling Program / International Ocean Discovery Program IODP; New Rock; Iceland; NADW; Nordic Seas; North Atlantic Deep Water; North Atlantic
• Online Access: https://dx.doi.org/10.1594/pangaea.848329; https://doi.pangaea.de/10.1594/PANGAEA.848329

Knowledge of the evolution of North Atlantic Deep Water (NADW) is key to understanding the past evolution of the climatic system. We developed a new rock-magnetic method to determine the constituent magnetic minerals of sediments and report on the evolution of NADW during 2.2-2.9 Ma. We measured isothermal remanence acquisition curves of North Atlantic deep-sea sediments drilled at the Gardar Drift and decomposed the first derivatives of these curves into high-coercivity and low-coercivity components. Residuals of the decomposition were sufficiently small throughout the study interval, confirming that the Gardar Drift sediments represent a mixing of the two end-members. Fractional changes of the high-coercivity component represent variation of the Iceland-Scotland Overflow Water, a branch of NADW formed at the Nordic Seas. The high-coercivity component increased significantly during an interglacial period just after ~2.68 Ma, which suggests that NADW formation in the Nordic Seas abruptly intensified at this ... : Supplement to: Sato, Masahiko; Makio, Masato; Hayashi, T; Ohno, Masao (2015): Abrupt intensification of North Atlantic Deep Water formation at the Nordic Seas during the late Pliocene climate transition. Geophysical Research Letters, 42(12), 4949-4955 ...