Channell, James E T (2019): Relative paleointensity proxy of sediment core JR298-PC726 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.904984, In supplement to: Channell, James E T; Xuan, Chuang; Hodell, David A; Crowhurst, Simon J; Larter, Robert D (2019): Relative paleointensity (RPI) and age control in Quaternary sediment drifts off the Antarctic Peninsula. Quaternary Science Reviews, 211, 17-33, https://doi.org/10.1016/j.quascirev.2019.03.006
Always quote citation above when using data! You can download the citation in several formats below.
Keyword(s):
Coverage:
Latitude: -69.531700 * Longitude: -93.915800
Date/Time Start: 2015-02-09T00:00:00 * Date/Time End: 2015-02-09T00:00:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 11.96 m
Event(s):
JR298-PC726 (PC726 CORE_NO 726) * Latitude: -69.531700 * Longitude: -93.915800 * Date/Time: 2015-02-09T00:00:00 * Elevation: -3663.0 m * Recovery: 12 m * Location: Bellingshausen Sea, Near crest of mound (IODP 732-FULL2 site BELS-2C) * Campaign: JR20150130 (JR298) * Basis: James Clark Ross * Method/Device: Piston corer (PC) * Comment: 8 sections (0-150 cmbsf, 150-300 cmbsf, 300-450 cmbsf, 450-600 cmbsf, 600-750 cmbsf, 750-900 cmbsf, 900-1050 cmbsf, 1050-1200 cmbsf); 1 core-top sample (disturbed; ca. 3 cm thick, stored in end cap in bag); 1 core-top suspension and sediment sample (disturbed, stored in bag); 2 core catcher samples; NOTE: thickness of core-top material could not be estimated reliably and therefore section depths were not corrected
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Channell, James E T | Geocode – meters below seafloor | |
| 2 | Relative paleointensity proxy | RPI | Channell, James E T | see Channell et al. (2019) | Slope of NRM/ARM |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
1136 data points