Shemesh, Aldo; Hodell, David A; Crosta, Xavier; Kanfoush, Sharon L; Charles, Christopher D; Guilderson, Thomas P (2002): (Table 1) Age-depth relation in sediment core TTN057-13-PC4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.842939, Supplement to: Shemesh, A et al. (2002): Sequence of events during the last deglaciation in Southern Ocean sediments and Antarctic ice cores. Paleoceanography, 17(4), 1056, https://doi.org/10.1029/2000PA000599
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Abstract:
The last glacial to interglacial transition was studied using down core records of stable isotopes in diatoms and foraminifera as well as surface water temperature, sea ice extent, and ice-rafted debris (IRD) concentrations from a piston core retrieved from the Atlantic sector of the Southern Ocean. Sea ice is the first variable to change during the last deglaciation, followed by nutrient proxies and sea surface temperature. This sequence of events is independent of the age model adopted for the core. The comparison of the marine records to Antarctic ice CO2 variation depends on the age model as 14C determinations cannot be obtained for the time interval of 29.5-14.5 ka. Assuming a constant sedimentation rate for this interval, our data suggest that sea ice and nutrient changes at about 19 ka B.P. lead the increase in atmospheric pCO2 by approximately 2000 years. Our diatom-based sea ice record is in phase with the sodium record of the Vostok ice core, which is related to sea ice cover and similarly leads the increase in atmospheric CO2. If gas exchange played a major role in determining glacial to interglacial CO2 variations, then a delay mechanism of a few thousand years is needed to explain the observed sequence of events. Otherwise, the main cause of atmospheric pCO2 change must be sought elsewhere, rather than in the Southern Ocean.
Related to:
Bard, Edouard; Arnold, Maurice; Hamelin, Bruno; Tisnérat-Laborde, Nadine; Cabioch, Guy (1998): Radiocarbon calibration by means of mass spectrometric 230Th/234U and 14C ages of corals: an updated database including samples from Barbados, Mururoa and Tahiti. Radiocarbon, 40(3), 1085-1092, https://doi.org/10.1017/S0033822200019135
Stuiver, Minze; Reimer, Paula J; Braziunas, Thomas F (1998): High-precision radiocarbon age calibration for terrestrial and marine samples. Radiocarbon, 40(3), 1127-1151, https://doi.org/10.1017/S0033822200019172
Coverage:
Latitude: -53.033333 * Longitude: 5.016667
Minimum DEPTH, sediment/rock: 0.20 m * Maximum DEPTH, sediment/rock: 12.89 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Shemesh, Aldo | |||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Age, dated | Age dated | ka | Shemesh, Aldo | Age, 14C AMS | |
| 4 | Age, dated standard deviation | Age dated std dev | ± | Shemesh, Aldo | Age, 14C AMS | |
| 5 | Calendar age | Cal age | ka BP | Shemesh, Aldo | Age, 14C calibrated | |
| 6 | Calendar age | Cal age | ka BP | Shemesh, Aldo | Age, 14C calibrated | maximum |
| 7 | Calendar age | Cal age | ka BP | Shemesh, Aldo | Age, 14C calibrated | #2 |
| 8 | Reference/source | Reference | Shemesh, Aldo |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
74 data points
Data
| 1 Sample label | 2 Depth sed [m] | 3 Age dated [ka] (Age, 14C AMS) | 4 Age dated std dev [±] (Age, 14C AMS) | 5 Cal age [ka BP] (Age, 14C calibrated) | 6 Cal age [ka BP] (maximum, Age, 14C calibrated) | 7 Cal age [ka BP] (#2, Age, 14C calibrated) | 8 Reference |
|---|---|---|---|---|---|---|---|
| X 18-23 | 0.20 | 1.590 | 0.08 | 0.72 | Stuiver et al. (1998) | ||
| X 63-65 | 0.63 | 2.630 | 0.06 | 1.83 | Stuiver et al. (1998) | ||
| VIII 21-26 | 2.56 | 6.850 | 0.06 | 6.93 | Stuiver et al. (1998) | ||
| VII 63-68 | 4.49 | 9.340 | 0.06 | 9.48 | 9.59 | Stuiver et al. (1998) | |
| VII 87-92 | 4.73 | 9.370 | 0.08 | 9.60 | Stuiver et al. (1998) | ||
| VI 0-5 | 5.36 | 10.050 | 0.04 | 10.31 | Stuiver et al. (1998) | ||
| VI 12-17 | 5.48 | 9.970 | 0.09 | 10.29 | Stuiver et al. (1998) | ||
| V 60-62 | 7.41 | 13.140 | 0.05 | 14.40 | 14.55 | Bard et al. (1998) | |
| V 81-86 | 7.63 | 13.070 | 0.08 | 14.32 | 14.47 | Bard et al. (1998) | |
| IV 90-92 | 9.19 | 26.360 | 0.15 | 29.13 | 29.98 | Bard et al. (1998) | |
| IV 90-92repl. | 9.19 | 26.360 | 0.15 | 29.13 | 29.98 | Bard et al. (1998) | |
| IV 141-143 | 9.70 | 33.420 | 0.25 | 36.99 | 37.83 | Bard et al. (1998) | |
| II 50-52 | 11.80 | 53.720 | 3.60 | ||||
| II 50-52repl. | 11.80 | 52.060 | 2.20 | ||||
| I 50-67 | 12.89 | >42.560 |