Volume susceptibility and anhysteretic susceptibility divided by susceptibility for the 100-248 meters composite depth (1.3-3.2 Ma) interval from Integrated Ocean Drilling Program (IODP) Site 303-U1308

• Main Author: Channell, James E T
• Format: Dataset
• Language: English
• Published: PANGAEA 2021
• Subjects: 303-U1308; ARM Susceptibility/susceptibility ratio; COMPCORE; Composite Core; Depth; composite; Exp303; IODP Site U1308; Joides Resolution; Magnetization directions; North Atlantic; North Atlantic Climate 1; see Channell et al. (2016); Susceptibility; volume
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.931892; https://doi.org/10.1594/PANGAEA.931892

Here we present volume susceptibility and anhysteretic susceptibility divided by susceptibility for the 100-248 meters composite depth (1.3-3.2 Ma) interval from Integrated Ocean Drilling Program (IODP) Site U1308 (49° 53'N, 24° 14'W; water depth 3871 m). Methods are described in Channell et al. (2016) (Quaternary Science Reviews, 131, 1-19, 2016, doi.org/10.1016/j.quascirev.2015.10.011). The magnetic records for 0-1.3 Ma at Site U1308 were published in Channell et al. 2008 (Earth and Planetary Science Letters, 274, 59-71, 2008, doi 10.1016/j.epsl.2008.07.005) and have been archived at: https://doi.org/10.1594/PANGAEA.808942, https://doi.org/10.1594/PANGAEA.808945, https://doi.org/10.1594/PANGAEA.808946. Benthic oxygen isotope stratigraphy for the 0- 3.2 Ma interval are archived at (https://doi.org/10.1594/PANGAEA.871936) and are the basis for the age model. The mean sedimentation rate for the 1.3-3.2 Ma interval is 8.5 cm/kyr.