Stumpf, Roland; Frank, Martin; Schönfeld, Joachim; Haley, Brian A (2011): (Table 2) Clay mineral abundances of sediment cores from the Gulf of Cadiz and the Portuguese margin [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.774224, In supplement to: Stumpf, R et al. (2011): Climatically driven changes in sediment supply on the SW Iberian shelf since the Last Glacial Maximum. Earth and Planetary Science Letters, 312(1-2), 80-90, https://doi.org/10.1016/j.epsl.2011.10.002
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Coverage:
Median Latitude: 37.741667 * Median Longitude: -9.143889 * South-bound Latitude: 36.380000 * West-bound Longitude: -10.680000 * North-bound Latitude: 39.040000 * East-bound Longitude: -7.071667
Date/Time Start: 1997-04-24T14:30:00 * Date/Time End: 1997-05-04T18:14:00
Minimum DEPTH, sediment/rock: 0.005 m * Maximum DEPTH, sediment/rock: 5.670 m
Event(s):
M39/1_08-3 (M39008-3) * Latitude: 36.380000 * Longitude: -7.071667 * Date/Time: 1997-04-24T14:30:00 * Elevation: -577.0 m * Recovery: 5.77 m * Campaign: M39/1 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL)
M39/1_36-4 * Latitude: 37.805000 * Longitude: -9.680000 * Date/Time: 1997-05-02T16:46:00 * Elevation: -1745.0 m * Recovery: 7.17 m * Campaign: M39/1 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL)
M39/1_58-2 (M39058-2) * Latitude: 39.040000 * Longitude: -10.680000 * Date/Time: 1997-05-04T18:14:00 * Elevation: -1974.0 m * Recovery: 3.2 m * Campaign: M39/1 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL)
Comment:
The age model for core M39008 was published by Cacho et al. (2001, doi:10.1029/2000PA000502) and Löwemark et al. (2004, doi:10.1016/S0025-3227(03)00351-7). The age models for cores M39036 and M39058 were published by Löwemark et al. (2004, doi:10.1016/S0025-3227(03)00351-7) and Schönfeld and Zahn (2000, doi:10.1016/S0031-0182(00)00035-3). Clay mineral abundances in weighted peak area percentage.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | AGE | Age | ka BP | Geocode | ||
| 4 | Kaolinite | Kln | % | Stumpf, Roland | X-ray diffraction, clay fraction | |
| 5 | Chlorite | Chl | % | Stumpf, Roland | X-ray diffraction, clay fraction | |
| 6 | Illite | Ill | % | Stumpf, Roland | X-ray diffraction, clay fraction | |
| 7 | Smectite | Sme | % | Stumpf, Roland | X-ray diffraction, clay fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
164 data points
Data
| 1 Event | 2 Depth sed [m] | 3 Age [ka BP] | 4 Kln [%] | 5 Chl [%] | 6 Ill [%] | 7 Sme [%] |
|---|---|---|---|---|---|---|
| M39/1_08-3 | 0.005 | 0.173 | 23 | 14 | 28 | 35 |
| M39/1_08-3 | 0.130 | 3.760 | 21 | 11 | 27 | 40 |
| M39/1_08-3 | 0.255 | 5.403 | 23 | 13 | 26 | 38 |
| M39/1_08-3 | 0.430 | 6.901 | 24 | 13 | 25 | 38 |
| M39/1_08-3 | 1.070 | 8.684 | 23 | 14 | 30 | 34 |
| M39/1_08-3 | 3.070 | 10.028 | 22 | 17 | 30 | 31 |
| M39/1_08-3 | 3.670 | 11.556 | 20 | 18 | 30 | 32 |
| M39/1_08-3 | 3.970 | 12.488 | 13 | 12 | 23 | 52 |
| M39/1_08-3 | 4.280 | 14.355 | 18 | 18 | 28 | 36 |
| M39/1_08-3 | 4.480 | 15.178 | 22 | 19 | 27 | 32 |
| M39/1_08-3 | 4.630 | 16.511 | 15 | 12 | 29 | 44 |
| M39/1_08-3 | 5.120 | 17.971 | 17 | 8 | 28 | 47 |
| M39/1_08-3 | 5.370 | 19.287 | 16 | 13 | 32 | 40 |
| M39/1_08-3 | 5.470 | 20.298 | 14 | 10 | 28 | 48 |
| M39/1_08-3 | 5.670 | 22.320 | 14 | 12 | 31 | 43 |
| M39/1_36-4 | 0.005 | 0.035 | 21 | 14 | 33 | 32 |
| M39/1_36-4 | 0.550 | 3.796 | 24 | 14 | 35 | 27 |
| M39/1_36-4 | 0.800 | 5.540 | 23 | 13 | 35 | 30 |
| M39/1_36-4 | 1.060 | 7.828 | 27 | 14 | 34 | 26 |
| M39/1_36-4 | 1.560 | 10.364 | 19 | 16 | 31 | 34 |
| M39/1_36-4 | 1.710 | 11.080 | 20 | 14 | 33 | 33 |
| M39/1_36-4 | 1.860 | 12.273 | 17 | 12 | 34 | 36 |
| M39/1_36-4 | 2.100 | 13.817 | 22 | 17 | 36 | 25 |
| M39/1_36-4 | 2.300 | 14.310 | 19 | 15 | 34 | 31 |
| M39/1_36-4 | 2.600 | 14.753 | 17 | 12 | 29 | 42 |
| M39/1_36-4 | 2.700 | 16.530 | 20 | 15 | 33 | 32 |
| M39/1_36-4 | 3.140 | 17.816 | 21 | 10 | 31 | 37 |
| M39/1_36-4 | 3.640 | 19.841 | 19 | 13 | 34 | 34 |
| M39/1_36-4 | 4.230 | 22.384 | 17 | 11 | 40 | 31 |
| M39/1_58-2 | 0.005 | 0.073 | 26 | 12 | 29 | 33 |
| M39/1_58-2 | 0.250 | 3.645 | 25 | 12 | 30 | 33 |
| M39/1_58-2 | 0.340 | 4.957 | 27 | 13 | 33 | 27 |
| M39/1_58-2 | 0.450 | 10.247 | 20 | 12 | 29 | 39 |
| M39/1_58-2 | 0.500 | 12.324 | 21 | 12 | 29 | 37 |
| M39/1_58-2 | 0.600 | 13.878 | 23 | 13 | 31 | 34 |
| M39/1_58-2 | 0.745 | 15.165 | 19 | 7 | 27 | 48 |
| M39/1_58-2 | 0.840 | 16.008 | 21 | 7 | 32 | 40 |
| M39/1_58-2 | 0.900 | 16.541 | 22 | 12 | 33 | 33 |
| M39/1_58-2 | 1.030 | 17.261 | 22 | 10 | 33 | 35 |
| M39/1_58-2 | 1.130 | 17.910 | 24 | 9 | 32 | 35 |
| M39/1_58-2 | 1.380 | 21.729 | 21 | 12 | 32 | 34 |