Bartels-Jonsdottir, Helga B; Voelker, Antje H L; Abrantes, Fatima F; Salgueiro, Emilia; Rodrigues, Teresa; Knudsen, Karen Luise (2015): Stable isotope ratios on G. inflata in sediment core POS287_26-3G [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.858739, In supplement to: Bartels-Jonsdottir, HB et al. (2015): High-frequency surface water changes in the Tagus prodelta off Lisbon, eastern North Atlantic, during the last two millennia. Marine Micropaleontology, 117, 13-24, https://doi.org/10.1016/j.marmicro.2015.03.001
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Coverage:
Latitude: 38.557670 * Longitude: -9.364500
Date/Time Start: 2002-04-29T10:08:00 * Date/Time End: 2002-04-29T10:08:00
Minimum DEPTH, sediment/rock: 0.180 m * Maximum DEPTH, sediment/rock: 1.500 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Bartels-Jonsdottir, Helga B | Geocode | |
| 2 | AGE | Age | ka BP | Bartels-Jonsdottir, Helga B | Geocode | |
| 3 | Age | Age | a AD/CE | Bartels-Jonsdottir, Helga B | ||
| 4 | Globorotalia inflata, δ18O | G. inflata δ18O | ‰ PDB | Bartels-Jonsdottir, Helga B | Mass spectrometer Finnigan MAT 251 | analysed at MARUM lab |
| 5 | Globorotalia inflata, δ13C | G. inflata δ13C | ‰ PDB | Bartels-Jonsdottir, Helga B | Mass spectrometer Finnigan MAT 251 | analysed at MARUM lab |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
45 data points
Data
| 1 Depth sed [m] | 2 Age [ka BP] | 3 Age [a AD/CE] | 4 G. inflata δ18O [‰ PDB] | 5 G. inflata δ13C [‰ PDB] |
|---|---|---|---|---|
| 0.180 | 0.047 | 1903 | 0.78 | 0.46 |
| 0.200 | 0.053 | 1897 | 0.74 | 0.79 |
| 0.310 | 0.085 | 1865 | 0.74 | 0.61 |
| 0.400 | 0.112 | 1838 | 0.88 | 0.70 |
| 0.500 | 0.142 | 1808 | 0.70 | 0.72 |
| 0.600 | 0.171 | 1779 | 0.61 | 0.59 |
| 0.700 | 0.201 | 1749 | 0.65 | 0.60 |
| 0.800 | 0.230 | 1720 | 0.79 | 0.73 |
| 0.910 | 0.285 | 1665 | 0.99 | 0.61 |
| 1.000 | 0.351 | 1599 | 0.91 | 0.45 |
| 1.100 | 0.424 | 1526 | 0.86 | 0.82 |
| 1.200 | 0.498 | 1452 | 0.65 | 0.64 |
| 1.300 | 0.571 | 1379 | 0.57 | 0.39 |
| 1.400 | 0.644 | 1306 | 0.69 | 0.50 |
| 1.500 | 0.703 | 1247 | 0.95 | 0.91 |