Colin, Christophe; Duhamel, Maxence (2021): Radiocarbon ages of Mediterranean Sea sediment cores [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.926898, In: Colin, C; Duhamel, M (2021): Nd isotope composition obtained on mixed planktonic foraminifera samples from cores MD01-2472, KET82-21, MD90-912, RECORD23 and MD90-917 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.926899
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Related to:
Colin, Christophe; Duhamel, Maxence; Siani, Giuseppe; Dubois-Dauphin, Quentin; Ducassou, Emmanuelle; Liu, Zhiqiang; Wu, J; Revel, M; Dapoigny, Arnaud; Douville, Eric; Taviani, Marco; Montagna, Paolo (submitted): Changes in the intermediate water masses of the Mediterranean Sea during the last climatic cycle - New constraints from neodymium isotopes in foraminifera. Paleoceanography and Paleoclimatology
Coverage:
Median Latitude: 38.668056 * Median Longitude: 12.037056 * South-bound Latitude: 38.311167 * West-bound Longitude: 8.912500 * North-bound Latitude: 38.990000 * East-bound Longitude: 17.430000
Date/Time Start: 1982-01-01T00:00:00 * Date/Time End: 1990-01-01T00:00:00
Minimum Elevation: -1020.0 m * Maximum Elevation: -414.0 m
Event(s):
KET82-21 * Latitude: 38.990000 * Longitude: 17.430000 * Date/Time: 1982-01-01T00:00:00 * Elevation: -599.0 m * Recovery: 11.11 m * Location: Mediterranean Sea * Campaign: ETNA82 * Method/Device: Piston corer (PC)
MD90-912 * Latitude: 38.311167 * Longitude: 9.768667 * Date/Time: 1990-01-01T00:00:00 * Elevation: -1020.0 m * Recovery: 16.33 m * Location: Mediterranean Sea * Campaign: PROMETEI * Basis: Marion Dufresne (1972) * Method/Device: Piston corer (PC)
Comment:
Radiocarbon dating was undertaken at the UMS-ARTEMIS Facility (CNRS-CEA Saclay, France) using a Pelletron 3MV AMS on 8 mg of well-preserved calcareous test samples of planktonic foraminifera (monospecific samples of Globigerinoides ruber, Globigerina bulloides and Globigerina inflata and a mix of planktonic foraminifera for one sample) in the size fraction >150 µm (Table 1). The age models for the cores were derived from the calibrated planktonic ages by applying a variable sea-surface reservoir ¹⁴C correction (Siani et al., 2000, 2001) and using INTCAL20 (Reimer et al., 2020) calibration curve in the Oxcal 4.4 software (Bronk Ramsey, 2009).
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | Colin, Christophe | |||
2 | Accumulation rate, calcium carbonate | Acc rate CaCO3 | g/cm2/ka | Colin, Christophe | ||
3 | Age, dated material | Dated material | Colin, Christophe | |||
4 | Age, dated | Age dated | ka | Colin, Christophe | Age, 14C AMS | |
5 | Age, dated standard deviation | Age dated std dev | ± | Colin, Christophe | calculated, 1 sigma | |
6 | Calendar age | Cal age | ka BP | Colin, Christophe | Age, 14C calibrated, IntCal20 (Reimer et al. 2020) | |
7 | Calendar age, standard deviation | Cal age std dev | ± | Colin, Christophe | calculated, 1 sigma |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
78 data points
Data
1 Event | 2 Acc rate CaCO3 [g/cm2/ka] | 3 Dated material | 4 Age dated [ka] | 5 Age dated std dev [±] | 6 Cal age [ka BP] | 7 Cal age std dev [±] |
---|---|---|---|---|---|---|
KET82-21 | 0.00 | G. ruber & G. inflata | 1.705 | 0.030 | 1.230 | 0.050 |
KET82-21 | 0.89 | G. ruber | 7.970 | 0.035 | 8.380 | 0.020 |
KET82-21 | 1.15 | G. bulloides | 13.760 | 0.060 | 16.080 | 0.100 |
KET82-21 | 1.99 | G. bulloides | 25.830 | 0.200 | 29.650 | 0.315 |
KET82-21 | 2.50 | G. bulloides | 29.030 | 0.290 | 32.940 | 0.550 |
MD90-912 | 0.02 | G. inflata | 3.895 | 0.030 | 3.770 | 0.055 |
MD90-912 | 0.25 | G. inflata | 10.710 | 0.040 | 12.090 | 0.240 |
MD90-912 | 0.39 | G. inflata | 14.780 | 0.060 | 17.520 | 0.160 |
MD90-912 | 1.25 | G. inflata | 34.810 | 0.580 | 39.630 | 0.680 |
RECORD23 | 0.13 | G. inflata | 0.225 | 0.030 | 0.000 | 0.030 |
RECORD23 | 0.79 | G. inflata | 2.965 | 0.030 | 2.720 | 0.060 |
RECORD23 | 1.14 | G. inflata | 5.525 | 0.030 | 5.830 | 0.080 |
RECORD23 | 1.92 | G. inflata | 8.190 | 0.035 | 8.560 | 0.040 |