Andrews, John T; Bjørk, Anders Anker; Eberl, Dennis D; Jennings, Anne E; Verplanck, Emily P (2015): (Table S4) Mineral composition of sediment core JR175-VC24 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.854003, In supplement to: Andrews, JT et al. (2015): Significant differences in late Quaternary bedrock erosion and transport: East versus West Greenland -70°N - evidence from the mineralogy of offshore glacial marine sediments. Journal of Quaternary Science, 30(5), 452-463, https://doi.org/10.1002/jqs.2787
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Coverage:
Latitude: 68.448000 * Longitude: -55.252700
Date/Time Start: 2009-08-22T00:00:00 * Date/Time End: 2009-08-22T00:00:00
Minimum DEPTH, sediment/rock: 0.010 m * Maximum DEPTH, sediment/rock: 5.600 m
Event(s):
JR175-VC24 * Latitude: 68.448000 * Longitude: -55.252700 * Date/Time: 2009-08-22T00:00:00 * Elevation: -432.0 m * Recovery: 5.63 m * Location: Davis Strait * Campaign: JR20090804 (JR175) * Basis: James Clark Ross * Method/Device: Vibro corer (VC)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Andrews, John T | Geocode | |
2 | Quartz | Qz | # | Andrews, John T | ||
3 | Kalifeldspar | Kfs | % | Andrews, John T | ||
4 | Anorthoclase | Anor | % | Andrews, John T | Anorthoclase feldspar | |
5 | Plagioclase | Pl | % | Andrews, John T | ||
6 | Carbonates | Carb | % | Andrews, John T | ||
7 | Halite | Hl | % | Andrews, John T | ||
8 | Amphibole | Amp | % | Andrews, John T | ferrotschermakite | |
9 | Pyroxene | Pyrox | % | Andrews, John T | diopside | |
10 | Iron oxide, FeO | FeO | % | Andrews, John T | ||
11 | Silica, amorphous | ASi | % | Andrews, John T | ||
12 | Kaolinite | Kln | % | Andrews, John T | Dry Branch | |
13 | Smectite | Sme | % | Andrews, John T | ||
14 | Illite | Ill | % | Andrews, John T | ||
15 | Biotite and Chlorite | Bt+Chl | % | Andrews, John T | ||
16 | Principal component 1 | PC1 | Score | Andrews, John T | Principal component analyses (PCA) | |
17 | Principal component 2 | PC2 | Score | Andrews, John T | Principal component analyses (PCA) | |
18 | Principal component 3 | PC3 | Score | Andrews, John T | Principal component analyses (PCA) | |
19 | Principal component 4 | PC4 | Score | Andrews, John T | Principal component analyses (PCA) | |
20 | Principal component 5 | PC5 | Score | Andrews, John T | Principal component analyses (PCA) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
304 data points
Data
1 Depth sed [m] | 2 Qz [#] | 3 Kfs [%] | 4 Anor [%] | 5 Pl [%] | 6 Carb [%] | 7 Hl [%] | 8 Amp [%] | 9 Pyrox [%] | 10 FeO [%] | 11 ASi [%] | 12 Kln [%] | 13 Sme [%] | 14 Ill [%] | 15 Bt+Chl [%] | 16 PC1 [Score] | 17 PC2 [Score] | 18 PC3 [Score] | 19 PC4 [Score] | 20 PC5 [Score] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.010 | 18.7 | 7.4 | 17.9 | 23.5 | 1.0 | 1.1 | 4.2 | 0.8 | 1.5 | 10.9 | 0.3 | 4.6 | 2.4 | 5.8 | 1.61 | 0.89 | -0.54 | 0.91 | 0.70 |
0.210 | 10.6 | 6.9 | 20.4 | 21.9 | 2.5 | 0.0 | 6.5 | 0.0 | 2.4 | 10.1 | 0.0 | 7.6 | 3.0 | 8.2 | 0.94 | 0.93 | -0.47 | 0.41 | 0.33 |
0.310 | 10.7 | 6.2 | 19.9 | 23.5 | 2.3 | 1.7 | 5.1 | 0.1 | 2.2 | 10.6 | 0.2 | 5.0 | 3.5 | 8.7 | 2.46 | 0.43 | 0.55 | -0.32 | 0.93 |
0.410 | 10.0 | 6.9 | 18.5 | 24.2 | 1.8 | 0.2 | 5.2 | 0.3 | 1.6 | 10.9 | 0.8 | 5.7 | 3.7 | 10.1 | 1.93 | 0.77 | 0.23 | 0.15 | 0.37 |
0.110 | 18.6 | 7.4 | 16.2 | 27.5 | 1.3 | 0.3 | 4.1 | 0.7 | 2.0 | 9.0 | 0.2 | 2.4 | 3.1 | 7.0 | 1.75 | 1.17 | -0.48 | 0.88 | 0.78 |
0.510 | 8.9 | 6.7 | 17.9 | 23.7 | 1.6 | 0.5 | 5.4 | 0.3 | 1.8 | 10.2 | 1.1 | 7.5 | 4.3 | 9.9 | 1.68 | 0.66 | 0.37 | 0.05 | 0.32 |
0.610 | 8.9 | 6.7 | 16.5 | 24.1 | 1.1 | 0.7 | 4.6 | 0.0 | 2.8 | 10.2 | 0.9 | 9.0 | 3.7 | 10.7 | 0.72 | 0.90 | -0.18 | 0.57 | 0.14 |
0.710 | 11.9 | 7.6 | 18.4 | 20.3 | 1.9 | 0.4 | 5.1 | 0.0 | 2.0 | 6.8 | 1.7 | 7.1 | 5.0 | 12.1 | 0.87 | 1.12 | 0.19 | 0.59 | 0.18 |
0.810 | 9.1 | 7.5 | 16.3 | 22.9 | 0.8 | 0.0 | 4.4 | 0.1 | 2.1 | 9.2 | 2.0 | 7.0 | 5.7 | 12.4 | 2.23 | 0.36 | 1.14 | -0.21 | 0.57 |
0.910 | 10.9 | 7.7 | 16.9 | 22.7 | 1.8 | 0.0 | 5.2 | 0.0 | 1.8 | 7.3 | 1.5 | 7.0 | 5.1 | 12.4 | 0.90 | 1.05 | 0.16 | 0.66 | 0.01 |
1.010 | 11.7 | 6.2 | 16.4 | 24.9 | 1.7 | 1.2 | 4.8 | 0.0 | 1.1 | 9.6 | 1.2 | 5.2 | 5.4 | 10.4 | 1.17 | 0.83 | -0.02 | 0.75 | -0.17 |
1.210 | 8.0 | 6.0 | 16.5 | 20.5 | 1.6 | 1.2 | 4.5 | 0.0 | 2.4 | 10.0 | 1.7 | 9.2 | 5.6 | 12.3 | 0.55 | 0.66 | 0.10 | 0.46 | -0.13 |
1.710 | 9.3 | 6.3 | 14.7 | 25.4 | 1.4 | 0.4 | 4.3 | 0.3 | 1.7 | 10.2 | 2.0 | 7.0 | 5.2 | 11.6 | 1.64 | 0.57 | 0.55 | 0.26 | 0.15 |
5.600 | 9.6 | 6.5 | 14.5 | 22.1 | 1.1 | 2.4 | 5.3 | 0.1 | 1.6 | 9.1 | 1.8 | 8.1 | 5.4 | 11.7 | 2.28 | 0.33 | 1.14 | -0.28 | 0.38 |
5.050 | 11.4 | 8.1 | 13.3 | 20.3 | 1.6 | 0.1 | 3.4 | 0.0 | 0.9 | 3.2 | 4.0 | 8.7 | 8.7 | 16.3 | 0.28 | 1.54 | 1.01 | 0.71 | 0.32 |
4.690 | 8.8 | 6.8 | 11.4 | 23.3 | 0.7 | 1.0 | 3.9 | 0.0 | 0.4 | 7.1 | 2.9 | 9.5 | 8.8 | 15.4 | 0.64 | 1.00 | 0.69 | 0.72 | -0.43 |