Keigwin, Lloyd D; Jones, Glenn A (1995): Stable isotopes on foraminifera from sediment core HU72-021-7. PANGAEA, https://doi.org/10.1594/PANGAEA.51940, In supplement to: Keigwin, LD; Jones, GA (1995): The marine record of deglaciation from the continental margin off Nova Scotia. Paleoceanography, 10(6), 973-986, https://doi.org/10.1029/95PA02643
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Coverage:
Latitude: 42.346700 * Longitude: -59.528300
Date/Time Start: 1972-01-01T00:00:00 * Date/Time End: 1972-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.015 m * Maximum DEPTH, sediment/rock: 4.013 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Calcium carbonate | CaCO3 | % | Keigwin, Lloyd D | % of >63 µm fraction | |
3 | Neogloboquadrina pachyderma sinistral, δ18O | N. pachyderma s δ18O | ‰ PDB | Keigwin, Lloyd D |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
91 data points
Data
1 Depth sed [m] | 2 CaCO3 [%] | 3 N. pachyderma s δ18O [‰ PDB] |
---|---|---|
0.015 | 0.50 | 1.36 |
0.065 | 0.68 | 1.21 |
0.110 | 0.42 | 1.77 |
0.160 | 0.37 | 1.98 |
0.210 | 0.45 | 1.94 |
0.260 | 0.49 | 2.05 |
0.310 | 0.77 | 2.08 |
0.360 | 0.40 | 2.42 |
0.410 | 1.02 | 2.69 |
0.460 | 0.85 | 2.64 |
0.510 | 1.34 | 2.99 |
0.612 | 1.93 | 3.14 |
0.710 | 1.02 | 2.84 |
0.810 | 0.53 | 2.86 |
0.912 | 1.17 | 2.80 |
1.012 | 0.37 | 2.84 |
1.112 | 0.22 | 2.59 |
1.212 | 0.49 | 2.68 |
1.312 | 1.48 | 2.90 |
1.412 | 0.34 | 3.12 |
1.512 | 0.28 | 3.03 |
1.612 | 0.08 | 3.40 |
1.712 | 0.20 | 3.08 |
1.812 | 0.30 | 3.26 |
1.912 | 0.14 | 3.45 |
2.012 | 0.66 | 3.22 |
2.112 | 0.11 | 3.18 |
2.212 | 0.79 | 3.47 |
2.312 | 0.41 | 3.40 |
2.412 | 1.59 | 3.25 |
2.512 | 1.19 | 3.32 |
2.612 | 1.36 | 3.43 |
2.712 | 0.70 | 3.37 |
2.812 | 0.72 | 3.51 |
2.922 | 0.06 | 3.56 |
3.012 | 0.11 | 3.58 |
3.112 | 0.08 | 3.67 |
3.212 | 0.09 | 3.40 |
3.312 | 0.10 | 3.67 |
3.412 | 0.31 | 3.65 |
3.512 | 0.13 | 3.84 |
3.612 | 0.02 | 3.88 |
3.712 | 0.02 | 3.87 |
3.812 | 0.02 | 3.67 |
3.912 | 0.02 | 3.78 |
4.012 | 0.02 |