MacLeod, Kenneth G; Huber, Brian T; Pletsch, Thomas; Röhl, Ursula; Kucera, Michal (2015): (Table 5) Correspondence analysis for Maastrichtian foraminifera of ODP Hole 171-1050C, sample scores [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.847732, In supplement to: MacLeod, KG et al. (2001): Maastrichtian foraminiferal and paleoceanographic changes on Milankovitch time scales. Paleoceanography, 16(2), 133-154, https://doi.org/10.1029/2000PA000514
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 30.099910 * Longitude: -76.234970
Date/Time Start: 1997-02-08T19:30:00 * Date/Time End: 1997-02-08T19:30:00
Minimum DEPTH, sediment/rock: 453.95 m * Maximum DEPTH, sediment/rock: 454.95 m
Event(s):
171-1050C * Latitude: 30.099910 * Longitude: -76.234970 * Date/Time: 1997-02-08T19:30:00 * Elevation: -2296.5 m * Penetration: 606 m * Recovery: 200.19 m * Location: Blake Nose, North Atlantic Ocean * Campaign: Leg171B * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 31 core; 288.5 m cored; 317.5 m drilled; 69.4 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | MacLeod, Kenneth G | |||
2 | DEPTH, sediment/rock | Depth sed | m | MacLeod, Kenneth G | Geocode | |
3 | Axis 1 | Axis 1 | MacLeod, Kenneth G | Detrended Correspondence Analysis | ||
4 | Axis 2 | Axis 2 | MacLeod, Kenneth G | Detrended Correspondence Analysis | ||
5 | Axis 3 | Axis 3 | MacLeod, Kenneth G | Detrended Correspondence Analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
88 data points
Data
1 Sample label | 2 Depth sed [m] | 3 Axis 1 | 4 Axis 2 | 5 Axis 3 |
---|---|---|---|---|
171-1050C-16R-2,25-27 | 453.95 | 0.26 | 0.13 | -0.06 |
171-1050C-16R-2,30-32 | 454.00 | 0.13 | 0.22 | -0.01 |
171-1050C-16R-2,35-37 | 454.05 | 0.09 | 0.08 | 0.14 |
171-1050C-16R-2,40-42 | 454.10 | -0.27 | 0.24 | -0.13 |
171-1050C-16R-2,45-47 | 454.15 | 0.02 | 0.13 | 0.03 |
171-1050C-16R-2,50-52 | 454.20 | 0.12 | 0.01 | 0.31 |
171-1050C-16R-2,55-57 | 454.25 | -0.10 | -0.11 | 0.60 |
171-1050C-16R-2,60-62 | 454.30 | -0.06 | 0.20 | -0.17 |
171-1050C-16R-2.,65-67 | 454.35 | -0.20 | 0.13 | -0.08 |
171-1050C-16R-2,70-72 | 454.40 | -0.47 | -0.09 | -0.13 |
171-1050C-16R-2,75-77 | 454.45 | -0.33 | -0.14 | -0.06 |
171-1050C-16R-2,80-82 | 454.50 | 0.12 | -0.25 | -0.17 |
171-1050C-16R-2,83-84 | 454.53 | 0.12 | 0.16 | -0.05 |
171-1050C-16R-2,85-87 | 454.55 | 0.34 | -0.31 | -0.14 |
171-1050C-16R-2,90-92 | 454.60 | 0.37 | -0.02 | 0.10 |
171-1050C-16R-2,95-97 | 454.65 | -0.24 | -0.33 | 0.00 |
171-1050C-16R-2,100-102 | 454.70 | -0.13 | -0.16 | 0.07 |
171-1050C-16R-2,105-106 | 454.75 | -0.09 | 0.18 | 0.05 |
171-1050C-16R-2,110-111 | 454.80 | -0.03 | 0.19 | -0.02 |
171-1050C-16R-2,115-117 | 454.85 | -0.16 | -0.19 | 0.03 |
171-1050C-16R-2,120-122 | 454.90 | 0.28 | -0.39 | -0.17 |
171-1050C-16R-2,125-127 | 454.95 | 0.15 | 0.19 | -0.07 |