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

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1. Verfasser: Channell, James E T
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Veröffentlicht: PANGAEA 2021
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author Channell, James E T
author_facet Channell, James E T
collection Datos científicos de ciencias marinas y ambientales
contents 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Channell et al. 2008 (Earth and Planetary Science Letters, 274, 59-71, 2008, doi 10.1016/j.epsl.2008.07.005) and have been archived at: https://doi.org/10.1594/PANGAEA.808942, https://doi.org/10.1594/PANGAEA.808945, https://doi.org/10.1594/PANGAEA.808946.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.
format Dataset Open Access
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institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle 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
Channell, James E T
303-U1308; ARM Susceptibility/susceptibility ratio; COMPCORE; Composite Core; Depth, composite; Exp303; IODP Site U1308; Joides Resolution; Magnetic susceptibility, volume; Magnetization directions; North Atlantic; North Atlantic Climate 1; North Atlantic Ocean; see Channell et al. (2016)
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.
title 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
topic 303-U1308; ARM Susceptibility/susceptibility ratio; COMPCORE; Composite Core; Depth, composite; Exp303; IODP Site U1308; Joides Resolution; Magnetic susceptibility, volume; Magnetization directions; North Atlantic; North Atlantic Climate 1; North Atlantic Ocean; see Channell et al. (2016)
url https://doi.org/10.1594/PANGAEA.931892