Knutz, Paul Cornils; Zahn, Rainer; Hall, Ian R (2007): (Table 2) Petrological composition of sediment core DAPC2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.833176, In supplement to: Knutz, PC et al. (2007): Centennial-scale variability of the British Ice Sheet: Implications for climate forcing and Atlantic meridional overturning circulation during the last deglaciation. Paleoceanography, 22(1), PA1207, https://doi.org/10.1029/2006PA001298
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Coverage:
Latitude: 59.000000 * Longitude: -9.600000
Minimum DEPTH, sediment/rock: 0.80 m * Maximum DEPTH, sediment/rock: 5.84 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Number | No | Knutz, Paul Cornils | IRD Peak | ||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Lithic grains | Lithic | # | Knutz, Paul Cornils | Counting >250 µm fraction | |
| 4 | Quartz, fractionated | Qz frac | % | Knutz, Paul Cornils | fractured | |
| 5 | Quartz, rounded | Qz round | % | Knutz, Paul Cornils | ||
| 6 | Minerals, other | Min other | % | Knutz, Paul Cornils | ||
| 7 | Carbonate, detritic/terrigenic | Carb detr | % | Knutz, Paul Cornils | ||
| 8 | Basalt | Basalt | # | Knutz, Paul Cornils |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
91 data points
Data
| 1 No | 2 Depth sed [m] | 3 Lithic [#] | 4 Qz frac [%] | 5 Qz round [%] | 6 Min other [%] | 7 Carb detr [%] | 8 Basalt [#] |
|---|---|---|---|---|---|---|---|
| 1 | 0.80 | 557 | 12 | 71 | 11 | 0 | 0 |
| 2 | 1.44 | 487 | 14 | 60 | 17 | 0 | 8 |
| 3 | 1.50 | 363 | 22 | 50 | 14 | 11 | 0 |
| 4 | 1.73 | 480 | 17 | 52 | 26 | 0 | 5 |
| 5 | 1.97 | 583 | 14 | 58 | 23 | 0 | 3 |
| 6 | 2.55 | 222 | 10 | 61 | 27 | 0 | 0 |
| 7 | 4.65 | 541 | 26 | 48 | 22 | 0 | 5 |
| 8 | 5.28 | 2400 | 22 | 48 | 24 | 0 | 5 |
| 9 | 5.30 | 2222 | 31 | 41 | 13 | 11 | 3 |
| 10 | 5.56 | 1230 | 29 | 38 | 21 | 8 | 4 |
| 11 | 5.64 | 1200 | 23 | 40 | 33 | 0 | 3 |
| 12 | 5.72 | 756 | 27 | 42 | 27 | 0 | 4 |
| 13 | 5.84 | 500 | 24 | 27 | 20 | 0 | 29 |