Hoogakker, Babette A A; Lu, Zunli; Umling, Natalie E; Jones, Luke; Zhou, Xiaoli; Rickaby, Rosalind E M; Thunell, Robert C; Cartapanis, Olivier; Galbraith, Eric Douglas (2018): Record of nitrogen stable isotopes in bulk sediment for TR163-25T and ODP Sites 202-1242 and 138-849 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.893218, In supplement to: Hoogakker, BAA et al. (2018): Glacial expansion of oxygen-depleted seawater in the eastern tropical Pacific. Nature, 562(7727), 410-413, https://doi.org/10.1038/s41586-018-0589-x
Always quote citation above when using data! You can download the citation in several formats below.
Further details:
Rafter, Patrick A; Charles, Christopher D (2012): Pleistocene equatorial Pacific dynamics inferred from the zonal asymmetry in sedimentary nitrogen isotopes. Paleoceanography, 27(3), https://doi.org/10.1029/2012PA002367
Robinson, Rebecca S; Martinez, P; Pena, Leopoldo D; Cacho, Isabel (2009): Nitrogen isotopic evidence for deglacial changes in nutrient supply in the eastern equatorial Pacific. Paleoceanography, 24(4), https://doi.org/10.1029/2008PA001702
Coverage:
Median Latitude: 2.129732 * Median Longitude: -94.191766 * South-bound Latitude: -1.650000 * West-bound Longitude: -110.518330 * North-bound Latitude: 7.855867 * East-bound Longitude: -83.606967
Date/Time Start: 1991-06-12T00:00:00 * Date/Time End: 2002-05-26T00:00:00
Minimum DEPTH, sediment/rock: 0.005 m * Maximum DEPTH, sediment/rock: 5.820 m
Event(s):
138-849 * Latitude: 0.183330 * Longitude: -110.518330 * Date/Time Start: 1991-09-07T00:00:00 * Date/Time End: 1991-06-12T00:00:00 * Elevation: -3839.0 m * Penetration: 791.4 m * Recovery: 777.62 m * Location: North Pacific Ocean * Campaign: Leg138 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 83 cores; 786.4 m cored; 0 m drilled; 98.9 % recovery
202-1242 * Latitude: 7.855867 * Longitude: -83.606967 * Date/Time: 2002-05-26T00:00:00 * Elevation: -1363.7 m * Penetration: 770.3 m * Recovery: 770.5 m * Location: North Pacific Ocean * Campaign: Leg202 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 80 cores; 743.8 m cored; 26.5 m drilled; 103.6 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | Hoogakker, Babette A A | |||
| 2 | DEPTH, sediment/rock | Depth sed | m | Hoogakker, Babette A A | Geocode | |
| 3 | AGE | Age | ka BP | Hoogakker, Babette A A | Geocode – this study | |
| 4 | AGE | Age | ka BP | Hoogakker, Babette A A | Geocode – see references | |
| 5 | δ15N | δ15N | ‰ air | Hoogakker, Babette A A | bulk sediment; see references | |
| 6 | Reference/source | Reference | Hoogakker, Babette A A |
License:
Creative Commons Attribution-ShareAlike 3.0 Unported (CC-BY-SA-3.0)
Size:
370 data points
Data
| 1 Event | 2 Depth sed [m] | 3 Age [ka BP] (this study) | 4 Age [ka BP] (see references) | 5 δ15N [‰ air] (bulk sediment; see references) | 6 Reference |
|---|---|---|---|---|---|
| TR163-25T | 0.005 | 3.7600 | 5.10 | This study | |
| TR163-25T | 0.050 | 4.2000 | 6.33 | This study | |
| TR163-25T | 0.100 | 4.7100 | 6.04 | This study | |
| TR163-25T | 0.150 | 5.2000 | 6.02 | This study | |
| TR163-25T | 0.200 | 5.7100 | 7.11 | This study | |
| TR163-25T | 0.250 | 6.2100 | 5.27 | This study | |
| TR163-25T | 0.300 | 7.2100 | 5.69 | This study | |
| TR163-25T | 0.350 | 7.7100 | 6.42 | This study | |
| TR163-25T | 0.500 | 9.7000 | 6.43 | This study | |
| TR163-25T | 0.550 | 10.3700 | 5.73 | This study | |
| TR163-25T | 0.650 | 11.7000 | 6.04 | This study | |
| TR163-25T | 0.700 | 12.3700 | 6.11 | This study | |
| TR163-25T | 0.750 | 12.3700 | 6.18 | This study | |
| TR163-25T | 0.800 | 13.0300 | 6.48 | This study | |
| TR163-25T | 0.850 | 13.5400 | 6.22 | This study | |
| TR163-25T | 0.900 | 14.0200 | 6.21 | This study | |
| TR163-25T | 0.950 | 14.5100 | 5.77 | This study | |
| TR163-25T | 1.000 | 15.0100 | 5.02 | This study | |
| TR163-25T | 1.025 | 15.3300 | 5.47 | This study | |
| TR163-25T | 1.050 | 15.6700 | 5.75 | This study | |
| TR163-25T | 1.075 | 16.0100 | 5.08 | This study | |
| TR163-25T | 1.100 | 16.3400 | 4.84 | This study | |
| TR163-25T | 1.125 | 16.6800 | 4.76 | This study | |
| TR163-25T | 1.150 | 17.0200 | 4.64 | This study | |
| TR163-25T | 1.200 | 17.7000 | 4.76 | This study | |
| TR163-25T | 1.250 | 18.3700 | 4.28 | This study | |
| TR163-25T | 1.300 | 19.0500 | 4.16 | This study | |
| TR163-25T | 1.350 | 19.7200 | 4.37 | This study | |
| TR163-25T | 1.400 | 20.3800 | 4.78 | This study | |
| TR163-25T | 1.450 | 21.0500 | 4.83 | This study | |
| TR163-25T | 1.500 | 21.5800 | 4.13 | This study | |
| TR163-25T | 1.555 | 22.1400 | 4.71 | This study | |
| TR163-25T | 1.605 | 22.6500 | 4.23 | This study | |
| TR163-25T | 1.655 | 23.1600 | 4.49 | This study | |
| TR163-25T | 1.705 | 23.6600 | 4.18 | This study | |
| TR163-25T | 1.755 | 24.1700 | 4.08 | This study | |
| TR163-25T | 1.805 | 24.6800 | 4.78 | This study | |
| TR163-25T | 1.855 | 25.1800 | 4.16 | This study | |
| TR163-25T | 1.905 | 25.6900 | 4.17 | This study | |
| TR163-25T | 1.955 | 26.2000 | 3.91 | This study | |
| TR163-25T | 2.005 | 26.7100 | 3.91 | This study | |
| 202-1242 | 0.030 | 0.1728 | 0.99 | 6.55 | Robinson et al. (2009) |
| 202-1242 | 0.070 | 0.4032 | 1.45 | 6.04 | Robinson et al. (2009) |
| 202-1242 | 0.110 | 0.6336 | 1.91 | 5.78 | Robinson et al. (2009) |
| 202-1242 | 0.110 | 0.6336 | 1.91 | 6.15 | Robinson et al. (2009) |
| 202-1242 | 0.150 | 0.8640 | 2.22 | 6.08 | Robinson et al. (2009) |
| 202-1242 | 0.190 | 1.0944 | 2.41 | 6.65 | Robinson et al. (2009) |
| 202-1242 | 0.230 | 1.3248 | 2.83 | 6.51 | Robinson et al. (2009) |
| 202-1242 | 0.270 | 1.5552 | 3.26 | 6.87 | Robinson et al. (2009) |
| 202-1242 | 0.310 | 1.7856 | 3.48 | 6.61 | Robinson et al. (2009) |
| 202-1242 | 0.320 | 1.8432 | 3.50 | 6.64 | Robinson et al. (2009) |
| 202-1242 | 0.350 | 2.0160 | 3.73 | 7.09 | Robinson et al. (2009) |
| 202-1242 | 0.390 | 2.2464 | 4.00 | 6.84 | Robinson et al. (2009) |
| 202-1242 | 0.430 | 2.4768 | 4.64 | 7.04 | Robinson et al. (2009) |
| 202-1242 | 0.470 | 2.7072 | 5.39 | 6.78 | Robinson et al. (2009) |
| 202-1242 | 0.510 | 2.9376 | 5.80 | 6.94 | Robinson et al. (2009) |
| 202-1242 | 0.550 | 3.1680 | 6.12 | 6.79 | Robinson et al. (2009) |
| 202-1242 | 0.590 | 3.3984 | 6.44 | 6.66 | Robinson et al. (2009) |
| 202-1242 | 0.600 | 3.4560 | 6.50 | 6.60 | Robinson et al. (2009) |
| 202-1242 | 0.630 | 3.6288 | 6.75 | 7.02 | Robinson et al. (2009) |
| 202-1242 | 0.670 | 3.8592 | 6.95 | 6.81 | Robinson et al. (2009) |
| 202-1242 | 0.710 | 4.0896 | 7.34 | 6.77 | Robinson et al. (2009) |
| 202-1242 | 0.750 | 4.3200 | 7.83 | 7.17 | Robinson et al. (2009) |
| 202-1242 | 0.790 | 4.5504 | 8.07 | 7.16 | Robinson et al. (2009) |
| 202-1242 | 0.830 | 4.7808 | 8.22 | 7.41 | Robinson et al. (2009) |
| 202-1242 | 0.850 | 4.8960 | 8.25 | 7.49 | Robinson et al. (2009) |
| 202-1242 | 0.870 | 5.0112 | 8.32 | 7.15 | Robinson et al. (2009) |
| 202-1242 | 0.910 | 5.2416 | 8.44 | 6.51 | Robinson et al. (2009) |
| 202-1242 | 0.950 | 5.4720 | 8.59 | 6.97 | Robinson et al. (2009) |
| 202-1242 | 0.990 | 5.7024 | 8.69 | 6.97 | Robinson et al. (2009) |
| 202-1242 | 1.030 | 5.9328 | 8.79 | 6.74 | Robinson et al. (2009) |
| 202-1242 | 1.070 | 6.1632 | 8.97 | 6.99 | Robinson et al. (2009) |
| 202-1242 | 1.110 | 6.3936 | 9.21 | 7.05 | Robinson et al. (2009) |
| 202-1242 | 1.150 | 6.6240 | 9.42 | 7.12 | Robinson et al. (2009) |
| 202-1242 | 1.190 | 6.8544 | 9.57 | 7.07 | Robinson et al. (2009) |
| 202-1242 | 1.230 | 7.0848 | 9.71 | 7.39 | Robinson et al. (2009) |
| 202-1242 | 1.270 | 7.3152 | 9.85 | 7.08 | Robinson et al. (2009) |
| 202-1242 | 1.310 | 7.5456 | 10.02 | 6.80 | Robinson et al. (2009) |
| 202-1242 | 1.350 | 7.7760 | 10.22 | 7.20 | Robinson et al. (2009) |
| 202-1242 | 1.390 | 8.0064 | 10.46 | 7.17 | Robinson et al. (2009) |
| 202-1242 | 1.430 | 8.2368 | 10.61 | 6.93 | Robinson et al. (2009) |
| 202-1242 | 1.520 | 8.7552 | 11.23 | 7.07 | Robinson et al. (2009) |
| 202-1242 | 1.560 | 8.9856 | 11.43 | 7.00 | Robinson et al. (2009) |
| 202-1242 | 1.600 | 9.2160 | 11.54 | 6.59 | Robinson et al. (2009) |
| 202-1242 | 1.640 | 9.4464 | 11.72 | 6.26 | Robinson et al. (2009) |
| 202-1242 | 1.680 | 9.6768 | 11.96 | 7.12 | Robinson et al. (2009) |
| 202-1242 | 1.720 | 9.9072 | 12.21 | 6.74 | Robinson et al. (2009) |
| 202-1242 | 1.760 | 10.1376 | 12.64 | 6.96 | Robinson et al. (2009) |
| 202-1242 | 1.800 | 10.3680 | 13.21 | 6.43 | Robinson et al. (2009) |
| 202-1242 | 1.840 | 10.5984 | 13.65 | 5.76 | Robinson et al. (2009) |
| 202-1242 | 1.850 | 10.6560 | 13.75 | 6.54 | Robinson et al. (2009) |
| 202-1242 | 1.880 | 10.8288 | 14.00 | 6.11 | Robinson et al. (2009) |
| 202-1242 | 1.920 | 11.9232 | 14.35 | 6.64 | Robinson et al. (2009) |
| 202-1242 | 1.960 | 13.0340 | 14.57 | 6.93 | Robinson et al. (2009) |
| 202-1242 | 2.000 | 13.3000 | 14.67 | 6.74 | Robinson et al. (2009) |
| 202-1242 | 2.040 | 13.5660 | 14.99 | 6.80 | Robinson et al. (2009) |
| 202-1242 | 2.080 | 13.8320 | 15.33 | 7.21 | Robinson et al. (2009) |
| 202-1242 | 2.120 | 14.0980 | 15.48 | 6.44 | Robinson et al. (2009) |
| 202-1242 | 2.160 | 14.3640 | 15.65 | 6.75 | Robinson et al. (2009) |
| 202-1242 | 2.200 | 14.6300 | 15.91 | 5.70 | Robinson et al. (2009) |
| 202-1242 | 2.240 | 14.8960 | 16.16 | 6.00 | Robinson et al. (2009) |
| 202-1242 | 2.280 | 15.1620 | 16.35 | 5.67 | Robinson et al. (2009) |
| 202-1242 | 2.320 | 15.4280 | 16.55 | 5.96 | Robinson et al. (2009) |
| 202-1242 | 2.360 | 15.6940 | 16.83 | 5.59 | Robinson et al. (2009) |
| 202-1242 | 2.360 | 15.6940 | 16.83 | 6.23 | Robinson et al. (2009) |
| 202-1242 | 2.400 | 15.9600 | 17.23 | 5.47 | Robinson et al. (2009) |
| 202-1242 | 2.440 | 16.2260 | 17.62 | 4.98 | Robinson et al. (2009) |
| 202-1242 | 2.480 | 16.4920 | 17.92 | 5.16 | Robinson et al. (2009) |
| 202-1242 | 2.520 | 16.7580 | 18.15 | 5.15 | Robinson et al. (2009) |
| 202-1242 | 2.560 | 17.0240 | 18.31 | 4.59 | Robinson et al. (2009) |
| 202-1242 | 2.600 | 17.2900 | 18.40 | 5.04 | Robinson et al. (2009) |
| 202-1242 | 2.600 | 17.2900 | 18.40 | 4.33 | Robinson et al. (2009) |
| 202-1242 | 2.640 | 17.5032 | 18.52 | 5.27 | Robinson et al. (2009) |
| 202-1242 | 2.680 | 17.7684 | 18.67 | 4.75 | Robinson et al. (2009) |
| 202-1242 | 2.720 | 18.0336 | 18.81 | 5.12 | Robinson et al. (2009) |
| 202-1242 | 2.760 | 18.2988 | 19.12 | 4.77 | Robinson et al. (2009) |
| 202-1242 | 2.800 | 18.5640 | 19.41 | 4.73 | Robinson et al. (2009) |
| 202-1242 | 2.840 | 18.8292 | 19.54 | 4.75 | Robinson et al. (2009) |
| 202-1242 | 2.850 | 18.8955 | 19.62 | 4.66 | Robinson et al. (2009) |
| 202-1242 | 2.880 | 19.0944 | 19.84 | 4.47 | Robinson et al. (2009) |
| 202-1242 | 2.920 | 19.3596 | 20.15 | 4.47 | Robinson et al. (2009) |
| 202-1242 | 2.960 | 19.6248 | 20.38 | 4.81 | Robinson et al. (2009) |
| 202-1242 | 3.030 | 20.0889 | 20.75 | 4.89 | Robinson et al. (2009) |
| 202-1242 | 3.070 | 20.3541 | 20.93 | 3.93 | Robinson et al. (2009) |
| 202-1242 | 3.110 | 20.6193 | 21.13 | 4.54 | Robinson et al. (2009) |
| 202-1242 | 3.150 | 20.8845 | 21.50 | 4.49 | Robinson et al. (2009) |
| 202-1242 | 3.190 | 21.1497 | 21.81 | 4.40 | Robinson et al. (2009) |
| 202-1242 | 3.230 | 21.4149 | 21.92 | 4.08 | Robinson et al. (2009) |
| 202-1242 | 3.270 | 21.6801 | 22.14 | 4.43 | Robinson et al. (2009) |
| 202-1242 | 3.310 | 21.9453 | 22.44 | 4.79 | Robinson et al. (2009) |
| 202-1242 | 3.350 | 22.2105 | 22.74 | 4.65 | Robinson et al. (2009) |
| 202-1242 | 3.390 | 22.4757 | 22.99 | 4.75 | Robinson et al. (2009) |
| 202-1242 | 3.430 | 22.7409 | 23.20 | 5.03 | Robinson et al. (2009) |
| 202-1242 | 3.470 | 23.0061 | 23.39 | 4.67 | Robinson et al. (2009) |
| 202-1242 | 3.510 | 23.2713 | 23.56 | 4.68 | Robinson et al. (2009) |
| 202-1242 | 3.550 | 23.5365 | 23.83 | 4.47 | Robinson et al. (2009) |
| 202-1242 | 3.590 | 23.8017 | 24.06 | 4.55 | Robinson et al. (2009) |
| 202-1242 | 3.630 | 24.0669 | 24.17 | 4.63 | Robinson et al. (2009) |
| 202-1242 | 3.670 | 24.3321 | 24.29 | 4.93 | Robinson et al. (2009) |
| 202-1242 | 3.710 | 24.5973 | 24.40 | 4.51 | Robinson et al. (2009) |
| 202-1242 | 3.750 | 24.8625 | 24.52 | 4.47 | Robinson et al. (2009) |
| 202-1242 | 3.790 | 25.1277 | 24.72 | 4.56 | Robinson et al. (2009) |
| 202-1242 | 3.830 | 25.3929 | 25.01 | 4.67 | Robinson et al. (2009) |
| 202-1242 | 3.830 | 25.3929 | 25.01 | 3.76 | Robinson et al. (2009) |
| 202-1242 | 3.870 | 25.6581 | 25.32 | 4.65 | Robinson et al. (2009) |
| 202-1242 | 3.910 | 25.9233 | 25.61 | 5.13 | Robinson et al. (2009) |
| 202-1242 | 3.950 | 26.1885 | 25.84 | 5.17 | Robinson et al. (2009) |
| 202-1242 | 3.990 | 26.4537 | 26.30 | 5.08 | Robinson et al. (2009) |
| 202-1242 | 4.030 | 26.7189 | 27.22 | 5.43 | Robinson et al. (2009) |
| 202-1242 | 4.070 | 26.9841 | 28.22 | 5.20 | Robinson et al. (2009) |
| 202-1242 | 4.070 | 26.9841 | 28.22 | 6.27 | Robinson et al. (2009) |
| 202-1242 | 4.110 | 27.2493 | 28.90 | 5.65 | Robinson et al. (2009) |
| 202-1242 | 4.150 | 27.5145 | 29.18 | 5.06 | Robinson et al. (2009) |
| 202-1242 | 4.190 | 27.7797 | 29.27 | 4.89 | Robinson et al. (2009) |
| 202-1242 | 4.230 | 28.0449 | 29.37 | 5.42 | Robinson et al. (2009) |
| 202-1242 | 4.270 | 28.3101 | 29.53 | 5.16 | Robinson et al. (2009) |
| 202-1242 | 4.310 | 28.5753 | 29.78 | 4.67 | Robinson et al. (2009) |
| 202-1242 | 4.350 | 28.8405 | 30.07 | 4.70 | Robinson et al. (2009) |
| 202-1242 | 4.390 | 29.1057 | 30.51 | 4.94 | Robinson et al. (2009) |
| 202-1242 | 4.390 | 29.1057 | 30.51 | 4.41 | Robinson et al. (2009) |
| 202-1242 | 4.430 | 29.3709 | 30.95 | 5.01 | Robinson et al. (2009) |
| 202-1242 | 4.470 | 29.6361 | 31.39 | 4.88 | Robinson et al. (2009) |
| 202-1242 | 4.600 | 30.7280 | 32.82 | 5.99 | Robinson et al. (2009) |
| 202-1242 | 5.100 | 34.0680 | 38.31 | 5.74 | Robinson et al. (2009) |
| 202-1242 | 5.350 | 35.7380 | 41.06 | 6.46 | Robinson et al. (2009) |
| 202-1242 | 5.580 | 37.2744 | 43.58 | 6.79 | Robinson et al. (2009) |
| 202-1242 | 5.820 | 38.8776 | 46.22 | 6.22 | Robinson et al. (2009) |
| 138-849 | 6.00 | 4.10 | Rafter and Charles (2012) | ||
| 138-849 | 8.00 | 4.80 | Rafter and Charles (2012) | ||
| 138-849 | 10.00 | 3.90 | Rafter and Charles (2012) | ||
| 138-849 | 12.00 | 3.50 | Rafter and Charles (2012) | ||
| 138-849 | 14.00 | 3.70 | Rafter and Charles (2012) | ||
| 138-849 | 16.00 | 3.40 | Rafter and Charles (2012) | ||
| 138-849 | 18.00 | 3.90 | Rafter and Charles (2012) | ||
| 138-849 | 20.00 | 4.10 | Rafter and Charles (2012) | ||
| 138-849 | 22.00 | 4.30 | Rafter and Charles (2012) | ||
| 138-849 | 24.00 | 4.60 | Rafter and Charles (2012) | ||
| 138-849 | 26.00 | 5.00 | Rafter and Charles (2012) | ||
| 138-849 | 28.00 | 4.90 | Rafter and Charles (2012) | ||
| 138-849 | 30.00 | 5.00 | Rafter and Charles (2012) | ||
| 138-849 | 32.00 | 4.80 | Rafter and Charles (2012) | ||
| 138-849 | 34.00 | 4.30 | Rafter and Charles (2012) | ||
| 138-849 | 36.00 | 4.80 | Rafter and Charles (2012) | ||
| 138-849 | 38.00 | 4.50 | Rafter and Charles (2012) | ||
| 138-849 | 40.00 | 4.60 | Rafter and Charles (2012) |