Channell, James E T (2021): 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 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.931892, In: Channell, JET (2021): Magnetization directions (Declination, Inclination, MAD), relative paleointensity (RPI) and susceptibility for IODP Site 303-U1308 for 100-248 mcd (1.3-3.2 Ma) [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.931821
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Abstract:
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Channell et al. 2008 (Earth and Planetary Science Letters, 274, 59-71, 2008, doi 10.1016/j.epsl.2008.07.005) and have been archived at: https://doi.org/10.1594/PANGAEA.808942, https://doi.org/10.1594/PANGAEA.808945, https://doi.org/10.1594/PANGAEA.808946.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.
Related to:
Channell, James E T; Hodell, David A; Curtis, Jason H (2016): Relative paleointensity (RPI) and oxygen isotope stratigraphy at IODP Site U1308: North Atlantic RPI stack for 1.2–2.2 Ma (NARPI-2200) and age of the Olduvai Subchron. Quaternary Science Reviews, 131, 1-19, https://doi.org/10.1016/j.quascirev.2015.10.011
Channell, James E T; Hodell, David A; Xuang, Chuang; Mazaud, Alain; Stoner, Joseph S (2008): Age calibrated relative paleointensity for the last 1.5 Myr from IODP Site U1308 (North Atlantic). Earth and Planetary Science Letters, 274, 59-71, https://doi.org/10.1016/j.epsl.2008.07.005
Hodell, David A; Channell, James E T (2016): Mode transitions in Northern Hemisphere glaciation: co-evolution of millennial and orbital variability in Quaternary climate. Climate of the Past, 12(9), 1805-1828, https://doi.org/10.5194/cp-12-1805-2016
Coverage:
Latitude: 49.877760 * Longitude: -24.238110
Date/Time Start: 2004-10-30T00:00:00 * Date/Time End: 2004-10-30T00:00:00
Minimum Elevation: -3871.0 m * Maximum Elevation: -3871.0 m
Event(s):
303-U1308 * Latitude: 49.877760 * Longitude: -24.238110 * Date/Time: 2004-10-30T00:00:00 * Elevation: -3871.0 m * Penetration: 1253.5 m * Recovery: 1246 m * Location: North Atlantic * Campaign: Exp303 (North Atlantic Climate 1) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 134 cores; 1246.0 m cored; 7.5 m drilled; 95.4 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Depth, composite | Depth comp | mcd | Channell, James E T | ||
| 2 | Magnetic susceptibility, volume | kappa | 10-6 SI | Channell, James E T | see Channell et al. (2016) | |
| 3 | ARM Susceptibility/susceptibility ratio | ARM/kappa | A/m | Channell, James E T | see Channell et al. (2016) |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
44169 data points
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