Razik, Sebastian; Chiessi, Cristiano Mazur; Romero, Oscar E; von Dobeneck, Tilo (2013): (Figure 4g) Carbonate-free mass-specific Saturation Isothermal Remanent Magnetization of sediment core GeoB6211-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.805102, In supplement to: Razik, S et al. (2013): Interaction of the South American Monsoon System and the Southern Westerly Wind Belt during the last 14 kyr. Palaeogeography, Palaeoclimatology, Palaeoecology, 374, 28-40, https://doi.org/10.1016/j.palaeo.2012.12.022
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Project(s):
Coverage:
Latitude: -32.505200 * Longitude: -50.242700
Date/Time Start: 1999-12-12T17:21:00 * Date/Time End: 1999-12-12T17:21:00
Minimum DEPTH, sediment/rock: 0.070 m * Maximum DEPTH, sediment/rock: 1.250 m
Event(s):
GeoB6211-2 * Latitude Start: -32.505200 * Longitude Start: -50.242700 * Latitude End: -32.505200 * Longitude End: -50.242700 * Date/Time: 1999-12-12T17:21:00 * Elevation Start: -657.0 m * Elevation End: -657.0 m * Recovery: 7.74 m * Location: Argentine Basin * Campaign: M46/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | AGE | Age | ka BP | Geocode | ||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Saturation isothermal remanent magnetization | SIRM | 10-6 A m2/kg | Razik, Sebastian | Magnetometer, U-channel, Model 755R, 2G Enterprises | carbonate-free |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
24 data points
Data
| 1 Age [ka BP] | 2 Depth sed [m] | 3 SIRM [10-6 A m2/kg] |
|---|---|---|
| 0.44 | 0.070 | 8190 |
| 0.81 | 0.120 | 7850 |
| 1.18 | 0.170 | 9040 |
| 1.65 | 0.220 | 8260 |
| 2.16 | 0.270 | 7860 |
| 2.66 | 0.320 | 8710 |
| 3.15 | 0.370 | 8410 |
| 3.57 | 0.415 | 8740 |
| 4.09 | 0.470 | 8350 |
| 4.57 | 0.520 | 7740 |
| 5.16 | 0.570 | 7360 |
| 5.92 | 0.620 | 7680 |
| 6.69 | 0.670 | 6760 |
| 7.46 | 0.720 | 7790 |
| 8.41 | 0.770 | 8360 |
| 9.40 | 0.820 | 7460 |
| 10.40 | 0.900 | 5250 |
| 10.65 | 0.950 | 5540 |
| 11.06 | 1.000 | 5150 |
| 11.71 | 1.050 | 5910 |
| 12.36 | 1.100 | 5600 |
| 13.01 | 1.150 | 5730 |
| 13.66 | 1.200 | 5210 |
| 14.09 | 1.250 | 5370 |