Wang, Rong; Biskaborn, Boris K; Ramisch, Arne; Ren, Jian; Zhang, Yongzhan; Gersonde, Rainer; Diekmann, Bernhard (2016): Clay mineral composition of surface sediment cores obtained during Sonne cruise SO202/1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.858571, In supplement to: Wang, R et al. (2016): Modern modes of provenance and dispersal of terrigenous sediments in the North Pacific and the Bering Sea: Implications and perspectives for palaeoenvironmental reconstructions. Geo-Marine Letters, 36(4), 259-270, https://doi.org/10.1007/s00367-016-0445-7
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Coverage:
Median Latitude: 49.504777 * Median Longitude: -179.852646 * South-bound Latitude: 37.767500 * West-bound Longitude: 149.485000 * North-bound Latitude: 60.403000 * East-bound Longitude: -148.884300
Date/Time Start: 2009-07-10T15:29:00 * Date/Time End: 2009-08-23T09:56:00
Minimum DEPTH, sediment/rock: 0 m * Maximum DEPTH, sediment/rock: 0 m
Event(s):
SO202/1_01-3 * Latitude: 44.025900 * Longitude: 152.919900 * Date/Time: 2009-07-10T15:29:00 * Elevation: -5282.0 m * Recovery: 0.32 m * Location: North Pacific Ocean * Campaign: SO202/1 (INOPEX) * Basis: Sonne * Method/Device: MultiCorer (MUC) * Comment: 11x(0.23-0.32)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | Wang, Rong | |||
| 2 | DEPTH, sediment/rock | Depth sed | m | Wang, Rong | Geocode | |
| 3 | Smectite | Sme | % | Wang, Rong | ||
| 4 | Illite | Ill | % | Wang, Rong | ||
| 5 | Chlorite | Chl | % | Wang, Rong | ||
| 6 | Kaolinite | Kln | % | Wang, Rong | ||
| 7 | Quartz | Qz | % | Wang, Rong | +% | |
| 8 | Feldspar | Fsp | % | Wang, Rong | +% | |
| 9 | Hornblende | Hbl | % | Wang, Rong | +% | |
| 10 | Illite | Ill | Wang, Rong | chemistry | ||
| 11 | Chlorite | Chl | Wang, Rong | chemistry | ||
| 12 | Illite crystallinity | Ill cryst | d2Theta | Wang, Rong |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
390 data points
Data
| 1 Event | 2 Depth sed [m] | 3 Sme [%] | 4 Ill [%] | 5 Chl [%] | 6 Kln [%] | 7 Qz [%] | 8 Fsp [%] | 9 Hbl [%] | 10 Ill | 11 Chl | 12 Ill cryst [d2Theta] |
|---|---|---|---|---|---|---|---|---|---|---|---|
| SO202/1_01-3 | 0 | 16.9 | 45.1 | 30.0 | 8.1 | 108.7 | 49.9 | 1.69 | 0.5 | 6.88 | 0.318 |
| SO202/1_02-4 | 0 | 19.9 | 36.1 | 34.9 | 9.0 | 65.9 | 39.4 | 0.58 | 0.53 | 5.49 | 0.292 |
| SO202/1_03-4 | 0 | 10.5 | 44.6 | 34.9 | 10.1 | 110.3 | 56.6 | 1.24 | 0.43 | 6.91 | 0.232 |
| SO202/1_04-3 | 0 | 17.8 | 39.1 | 34.4 | 8.7 | 119.0 | 60.8 | 2.56 | 0.61 | 6.33 | 0.317 |
| SO202/1_05-3 | 0 | 8.6 | 33.7 | 46.4 | 11.3 | 118.1 | 71.9 | 2.14 | 0.78 | 5.89 | 0.318 |
| SO202/1_06-2 | 0 | 16.3 | 38.7 | 37.8 | 7.2 | 60.8 | 38.1 | 2.14 | 0.37 | 5.47 | 0.297 |
| SO202/1_07-2 | 0 | 7.0 | 40.4 | 45.0 | 7.6 | 68.7 | 48.6 | 2.80 | 0.51 | 5.9 | 0.253 |
| SO202/1_08-1 | 0 | 16.2 | 35.7 | 42.1 | 6.0 | 74.4 | 51.6 | 2.05 | 0.39 | 6.59 | 0.269 |
| SO202/1_09-2 | 0 | 11.6 | 40.1 | 41.8 | 6.5 | 67.2 | 45.2 | 2.01 | 0.44 | 6.5 | 0.328 |
| SO202/1_10-2 | 0 | 11.7 | 38.6 | 43.8 | 5.9 | 70.2 | 62.9 | 2.81 | 0.32 | 7.92 | 0.289 |
| SO202/1_11-1 | 0 | 17.5 | 37.3 | 39.3 | 6.0 | 86.0 | 76.8 | 3.25 | 0.69 | 5.84 | 0.351 |
| SO202/1_12-2 | 0 | 18.4 | 37.8 | 37.7 | 6.0 | 97.0 | 92.5 | 3.36 | 0.6 | 5 | 0.251 |
| SO202/1_13-4 | 0 | 13.5 | 38.6 | 40.6 | 7.2 | 65.0 | 43.0 | 1.85 | 0.4 | 6.07 | 0.278 |
| SO202/1_14-5 | 0 | 10.6 | 45.2 | 38.2 | 6.0 | 90.2 | 53.6 | 2.43 | 0.53 | 6.88 | 0.301 |
| SO202/1_15-4 | 0 | 11.1 | 50.5 | 32.2 | 6.1 | 70.8 | 33.7 | 1.10 | 0.52 | 5.62 | 0.258 |
| SO202/1_16-1 | 0 | 13.7 | 38.7 | 37.6 | 9.9 | 23.3 | 9.4 | 0.53 | 0.68 | 6.36 | 0.314 |
| SO202/1_18-1 | 0 | 9.6 | 51.1 | 32.7 | 6.6 | 52.6 | 21.3 | 1.81 | 0.48 | 6.32 | 0.241 |
| SO202/1_19-5 | 0 | 10.5 | 46.5 | 36.9 | 6.1 | 78.4 | 40.6 | 1.53 | 0.44 | 6.74 | 0.216 |
| SO202/1_21-2 | 0 | 10.3 | 40.8 | 42.4 | 6.5 | 71.9 | 63.1 | 2.43 | 0.35 | 6.54 | 0.306 |
| SO202/1_22-1 | 0 | 13.3 | 39.5 | 41.5 | 5.7 | 67.0 | 59.5 | 2.91 | 0.61 | 6.27 | 0.342 |
| SO202/1_23-4 | 0 | 6.6 | 40.8 | 46.7 | 5.9 | 39.8 | 31.2 | 2.54 | 0.47 | 6.28 | 0.326 |
| SO202/1_24-2 | 0 | 6.7 | 40.5 | 47.0 | 5.7 | 51.7 | 42.0 | 3.04 | 0.46 | 6.47 | 0.307 |
| SO202/1_25-1 | 0 | 4.4 | 38.4 | 49.4 | 7.7 | 39.5 | 33.1 | 2.86 | 0.51 | 6.08 | 0.330 |
| SO202/1_26-1 | 0 | 6.7 | 41.8 | 45.4 | 6.1 | 38.1 | 24.9 | 3.56 | 0.37 | 5.94 | 0.274 |
| SO202/1_27-1 | 0 | 6.6 | 36.9 | 50.1 | 6.4 | 47.6 | 37.0 | 3.81 | 0.42 | 6.14 | 0.317 |
| SO202/1_28-1 | 0 | 5.5 | 39.5 | 47.9 | 7.1 | 41.6 | 32.0 | 3.45 | 0.39 | 5.94 | 0.332 |
| SO202/1_29-5 | 0 | 7.9 | 44.9 | 39.7 | 7.5 | 65.2 | 41.4 | 2.25 | 0.46 | 5.89 | 0.298 |
| SO202/1_31-5 | 0 | 21.8 | 45.3 | 25.5 | 7.4 | 67.6 | 50.0 | 1.50 | 0.58 | 7.07 | 0.284 |
| SO202/1_32-5 | 0 | 6.0 | 60.2 | 26.1 | 7.8 | 74.8 | 29.1 | 0.67 | 0.56 | 6.37 | 0.259 |
| SO202/1_33-5 | 0 | 4.3 | 60.5 | 27.6 | 7.5 | 67.7 | 25.6 | 0.50 | 0.56 | 5.57 | 0.263 |
| SO202/1_34-4 | 0 | 4.8 | 63.7 | 24.6 | 6.8 | 70.5 | 24.1 | 0.70 | 0.48 | 5.71 | 0.256 |
| SO202/1_36-6 | 0 | 1.5 | 58.0 | 31.4 | 9.0 | 114.8 | 42.1 | 0.62 | 0.77 | 5.38 | 0.297 |
| SO202/1_37-1 | 0 | 11.6 | 55.7 | 24.8 | 7.8 | 73.7 | 21.7 | 1.57 | 0.73 | 4.65 | 0.331 |
| SO202/1_38-1 | 0 | 8.1 | 59.8 | 24.8 | 7.2 | 82.6 | 32.7 | 0.69 | 0.57 | 6.17 | 0.267 |
| SO202/1_39-2 | 0 | 7.3 | 60.0 | 25.8 | 6.9 | 75.7 | 29.6 | 0.63 | 0.5 | 6.28 | 0.245 |
| SO202/1_40-2 | 0 | 8.4 | 57.5 | 25.7 | 8.4 | 40.3 | 13.0 | 1.00 | 0.56 | 5.78 | 0.271 |
| SO202/1_41-3 | 0 | 8.8 | 59.2 | 25.4 | 6.7 | 90.4 | 32.4 | 0.75 | 0.58 | 6.19 | 0.264 |
| SO202/1_42-3 | 0 | 8.3 | 60.0 | 25.2 | 6.6 | 94.9 | 35.1 | 0.45 | 0.47 | 5.52 | 0.257 |
| SO202/1_45-2 | 0 | 10.0 | 57.5 | 25.4 | 7.1 | 88.8 | 34.7 | 0.73 | 0.5 | 6.8 | 0.244 |