Schönfeld, Joachim; Zahn, Rainer; de Abreu, Lucia (2003): (Table 1) Age model of sediment core MD95-2039 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.82025, In supplement to: Schönfeld, J et al. (2003): Surface to deep water response to rapid climate changes at the western Iberian Margin. Global and Planetary Change, 36(4), 237-264, https://doi.org/10.1016/S0921-8181(02)00197-2
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Project(s):
Coverage:
Latitude: 40.578500 * Longitude: -10.348500
Date/Time Start: 1995-07-07T00:00:00 * Date/Time End: 1995-07-07T00:00:00
Minimum DEPTH, sediment/rock: 0.020 m * Maximum DEPTH, sediment/rock: 35.600 m
Event(s):
MD95-2039 (MD952039) * Latitude: 40.578500 * Longitude: -10.348500 * Date/Time: 1995-07-07T00:00:00 * Elevation: -3381.0 m * Recovery: 36 m * Location: Porto Seamount * Campaign: MD101 (IMAGES I) * Basis: Marion Dufresne (1995) * Method/Device: Calypso Corer (CALYPSO) * Comment: XXIV Sections
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Age, comment | Comm | Schönfeld, Joachim | Event (isotope stage, Heinrich event or radiocarbon sample no. | ||
| 3 | Age, dated | Age dated | ka | Schönfeld, Joachim | Age, 14C AMS | |
| 4 | Age, dated | Age dated | ka | Schönfeld, Joachim | Age, 14C milieu/reservoir corrected (-400 yr) | |
| 5 | Age, dated standard deviation | Age dated std dev | ± | Schönfeld, Joachim | Age, 14C AMS | |
| 6 | Depth, reference | Depth ref | m | Schönfeld, Joachim | Referenced sediment core: MD95-2040 | |
| 7 | Age model | Age model | ka | Schönfeld, Joachim | Age, 14C calibrated, CALIB 4.3 (Stuiver et al., 1998) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
277 data points
Data
| 1 Depth sed [m] | 2 Comm (Event (isotope stage, Heinric...) | 3 Age dated [ka] (Age, 14C AMS) | 4 Age dated [ka] (Age, 14C milieu/reservoir cor...) | 5 Age dated std dev [±] (Age, 14C AMS) | 6 Depth ref [m] (Referenced sediment core: MD9...) | 7 Age model [ka] (Age, 14C calibrated, CALIB 4....) |
|---|---|---|---|---|---|---|
| 0.020 | core top | 0.000 | 0.000 | |||
| 0.385 | KIA 779 | 6.150 | 5.750 | 0.050 | 6.578 | |
| 1.000 | 1.1 | 9.100 | 10.163 | |||
| 1.300 | (2.0) | |||||
| 1.520 | KIA13451 | 12.050 | 11.650 | 0.070 | 13.522 | |
| 1.600 | KIA13452 | 12.250 | 11.850 | 0.070 | 13.659 | |
| 1.685 | KIA 780 | 12.620 | 12.220 | 0.110 | 14.129 | |
| 1.700 | KIA13453 | 15.540 | 15.140 | 0.090 | /17.991 | |
| 1.800 | KIA13454 | 12.760 | 12.360 | 0.080 | 14.591 | |
| 1.900 | KIA13455 | 13.100 | 12.700 | 0.080 | 14.850 | |
| 2.085 | KIA 781/2 | 13.725 | 13.330 | 0.100 | 15.897 | |
| 2.100 | correlation IRD | 242.500 | 16.014 | |||
| 2.140 | H1 | 13.540 | /16.151 | |||
| 2.200 | correlation IRD | 245.500 | 16.075 | |||
| 2.250 | correlation IRD | 248.500 | 16.135 | |||
| 2.300 | KIA13456 | 13.600 | 13.200 | 0.090 | /15.746 | |
| 2.340 | correlation IRD | 254.500 | 16.257 | |||
| 2.520 | KIA13627 | 14.550 | 14.150 | 0.070 | 16.857 | |
| 2.885 | KIA 783/4 | 14.450 | 14.050 | 0.110 | /16.743 | |
| 2.915 | KIA13628 | 14.720 | 14.320 | 0.070 | /17.049 | |
| 2.975 | KIA13629 | 15.150 | 14.750 | 0.080 | 17.550 | |
| 3.020 | GRIP (1833.7m) | |||||
| 3.095 | KIA13630 | 15.230 | 14.830 | 0.080 | 17.643 | |
| 3.330 | correlation 18O | 329.500 | 18.719 | |||
| 3.445 | correlation 18O | 341.500 | 19.240 | |||
| 3.820 | correlation GISP2 | 20.300 | ||||
| 4.315 | correlation 18O | 413.500 | 21.155 | |||
| 4.900 | (3.0) | |||||
| 5.000 | correlation 18O | 467.500 | 22.437 | |||
| 5.100 | GRIP (1945.35m) | |||||
| 5.200 | correlation 18O | 497.500 | 23.034 | |||
| 5.400 | GRIP (1956.35m) | |||||
| 5.425 | KIA 785 | 20.140 | 19.740 | 0.210 | 23.297 | |
| 5.425 | KIA 786 | 20.720 | 20.320 | 0.220 | /23.919 | |
| 5.425 | KIA 785/6 (avg.) | 20.430 | 20.030 | 0.220 | /23.620 | |
| 5.440 | H2 | 20.460 | 23.777 | |||
| 5.600 | GRIP (1973m) | |||||
| 6.480 | KIA 787 | 22.810 | 22.410 | 0.280 | 25.731 | |
| 7.000 | MD952040 (?cm) | |||||
| 7.680 | H3 | 27.000 | 30.461 | |||
| 8.000 | Bond et al. (1993) | /29.000 | ||||
| 8.185 | KIA 788 | 27.980 | 27.580 | 0.520 | 31.017 | |
| 9.400 | KIA13631 | 32.530 | 32.130 | 0.480 | 34.978 | |
| 9.490 | KIA 789 | 29.000 | /28.600 | 0.590 | ||
| 9.500 | correlation 18O | 827.500 | 36.142 | |||
| 9.670 | correlation 18O | 836.500 | 36.684 | |||
| 9.820 | correlation 18O | 851.500 | 37.587 | |||
| 9.940 | correlation 18O | 860.500 | 38.129 | |||
| 10.100 | correlation 18O | 866.500 | 38.490 | |||
| 10.190 | KIA 790/1 | 31.040 | /30.640 | 0.690 | ||
| 10.200 | H4 | 34.150 | 39.379 | |||
| 10.250 | correlation 18O | 884.500 | 39.517 | |||
| 10.350 | correlation 18O | 896.500 | 40.068 | |||
| 10.500 | correlation 18O | 909.500 | 40.666 | |||
| 10.600 | correlation 18O | 914.500 | 40.896 | |||
| 10.720 | correlation 18O | 928.500 | 41.540 | |||
| 10.900 | correlation 18O | 938.500 | 42.022 | |||
| 11.100 | correlation 18O | 950.500 | 42.600 | |||
| 11.400 | correlation 18O | 962.500 | 43.256 | |||
| 11.850 | 3.13 | 42.000 | 43.880 | |||
| 12.160 | H5 | 45.800 | ||||
| 12.950 | 3.3 | 50.210 | ||||
| 13.600 | 3.31 | 55.450 | ||||
| 14.150 | (4.0) | 58.690 | ||||
| 14.600 | (H6) | |||||
| 15.500 | 5 | 73.910 | ||||
| 16.600 | 5.1 | 79.250 | ||||
| 17.100 | 5.2 | 90.950 | ||||
| 17.600 | 5.3 | 99.380 | ||||
| 18.500 | 5.4 | 110.790 | ||||
| 19.000 | 5.5 | 123.820 | ||||
| 19.700 | 6 | 129.840 | ||||
| 20.300 | 6.2 | 135.100 | ||||
| 22.300 | 6.3 | 142.280 | ||||
| 23.000 | 6.4 | 152.580 | ||||
| 23.300 | 6.41 | 161.340 | ||||
| 23.650 | 6.42 | 165.350 | ||||
| 24.020 | 6.5 | 175.050 | ||||
| 25.100 | 6.6 | 183.300 | ||||
| 25.400 | 7 | 189.610 | ||||
| 26.000 | 7.1 | 193.070 | ||||
| 26.200 | 7.2 | 200.570 | ||||
| 26.600 | 7.3 | 215.540 | ||||
| 27.400 | 7.4 | 224.890 | ||||
| 27.900 | 7.5 | 240.190 | ||||
| 28.100 | 8 | 244.180 | ||||
| 29.000 | 8.2 | 249.000 | ||||
| 29.800 | 8.3 | 257.000 | ||||
| 31.100 | 8.4 | 265.670 | ||||
| 32.400 | 8.5 | 288.540 | ||||
| 33.200 | 8.6 | 299.000 | ||||
| 33.400 | 9 | 303.000 | ||||
| 33.800 | 9.1 | 310.000 | ||||
| 34.700 | 9.2 | 320.000 | ||||
| 35.200 | 9.3 | 331.000 | ||||
| 35.600 | 10 | 339.000 |