Keigwin, Lloyd D; Jones, Glenn A (1995): Stable isotopes on foraminifera from sediment core V17-178 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51937, 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
Always quote citation above when using data! You can download the citation in several formats below.
Coverage:
Latitude: 43.383000 * Longitude: -54.870000
Date/Time Start: 1961-08-21T00:00:00 * Date/Time End: 1961-08-21T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 4.410 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Globigerinoides ruber white, δ18O | G. ruber w δ18O | ‰ PDB | Keigwin, Lloyd D | ||
| 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:
74 data points
Data
| 1 Depth sed [m] | 2 G. ruber w δ18O [‰ PDB] | 3 N. pachyderma s δ18O [‰ PDB] |
|---|---|---|
| 0.000 | 1.610 | |
| 0.085 | -0.730 | 1.720 |
| 0.210 | -0.400 | 1.680 |
| 0.295 | -0.770 | 1.620 |
| 0.415 | -1.000 | 1.450 |
| 0.515 | -0.720 | 1.760 |
| 0.615 | -0.650 | 1.740 |
| 0.715 | -0.830 | 1.540 |
| 0.785 | -1.160 | 1.500 |
| 0.915 | -0.810 | 1.520 |
| 0.995 | -0.920 | 1.410 |
| 1.095 | -1.000 | 1.300 |
| 1.195 | -0.720 | 1.410 |
| 1.295 | -1.130 | 1.250 |
| 1.405 | -1.210 | 0.890 |
| 1.495 | -1.320 | 1.140 |
| 1.595 | -0.990 | 1.360 |
| 1.705 | -0.820 | 1.520 |
| 1.810 | -1.350 | 1.830 |
| 1.905 | -1.060 | 2.010 |
| 2.020 | -1.010 | 2.080 |
| 2.115 | 2.430 | |
| 2.205 | -0.820 | 2.260 |
| 2.320 | -0.600 | 2.360 |
| 2.410 | -1.340 | 2.200 |
| 2.495 | -0.410 | 2.380 |
| 2.575 | -0.560 | 2.600 |
| 2.660 | -0.060 | 3.060 |
| 2.715 | 0.130 | 2.960 |
| 2.795 | 3.130 | |
| 2.940 | 3.140 | |
| 3.015 | 3.300 | |
| 3.110 | 3.220 | |
| 3.220 | 3.060 | |
| 3.260 | 3.080 | |
| 3.330 | 3.500 | |
| 3.410 | 3.270 | |
| 3.510 | 3.450 | |
| 3.610 | 3.580 | |
| 3.700 | 3.230 | |
| 3.810 | 3.060 | |
| 3.910 | 3.530 | |
| 4.010 | 3.030 | |
| 4.090 | 3.080 | |
| 4.210 | 3.500 | |
| 4.300 | 3.550 | |
| 4.410 | 3.340 |