Wilcox, Paul S (2020): Hendy test of stable carbon and oxygen isotope ratios of Speleothem M37-1-16A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.925780, In: Wilcox, PS (2020): Schrattenkarst speleothem geochemistry [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.925799
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Wilcox, Paul S; Honiat, Charlotte; Trüssel, Martin; Edwards, R Lawrence; Spötl, Christoph (2020): Exceptional warmth and climate instability occurred in the European Alps during the Last Interglacial period. Communications Earth & Environment, 1(1), https://doi.org/10.1038/s43247-020-00063-w
Coverage:
Latitude: 46.783000 * Longitude: 8.267000
Minimum DISTANCE: 2.1 cm * Maximum DISTANCE: 85.0 cm
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Wilcox, Paul S | |||
| 2 | DISTANCE | Distance | cm | Wilcox, Paul S | Geocode | |
| 3 | δ18O, calcite | δ18O cal | ‰ PDB | Wilcox, Paul S | Mass spectrometer ThermoFisher Delta V | vs. VPDB |
| 4 | δ13C, calcite | δ13C cal | ‰ PDB | Wilcox, Paul S | Mass spectrometer ThermoFisher Delta V | vs. VPDB |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
237 data points
Data
| 1 Sample label | 2 Distance [cm] | 3 δ18O cal [‰ PDB] | 4 δ13C cal [‰ PDB] |
|---|---|---|---|
| M37-H1-1 | 2.1 | 2.01 | -9.81 |
| M37-H1-2 | 2.1 | 2.19 | -9.52 |
| M37-H1-3 | 2.1 | 2.26 | -9.55 |
| M37-H1-4 | 2.1 | 2.19 | -9.54 |
| M37-H1-5 | 2.1 | 2.33 | -9.47 |
| M37-H1-6 | 2.1 | 2.31 | -9.47 |
| M37-H1-7 | 2.1 | 2.33 | -9.48 |
| M37-H2-1 | 7.5 | 1.62 | -9.06 |
| M37-H2-2 | 7.5 | 1.96 | -9.11 |
| M37-H2-3 | 7.5 | 1.84 | -9.21 |
| M37-H2-4 | 7.5 | 1.78 | -9.19 |
| M37-H2-5 | 7.5 | 1.84 | -9.26 |
| M37-H2-6 | 7.5 | 1.96 | -9.31 |
| M37-H2-7 | 7.5 | 1.95 | -9.16 |
| M37-H2-8 | 7.5 | 2.02 | -9.08 |
| M37-H3-1 | 8.4 | 0.58 | -7.90 |
| M37-H3-2 | 8.4 | 0.48 | -8.24 |
| M37-H3-3 | 8.4 | 0.40 | -7.82 |
| M37-H3-4 | 8.4 | 0.18 | -7.85 |
| M37-H3-5 | 8.4 | 0.19 | -7.85 |
| M37-H3-6 | 8.4 | 0.23 | -7.89 |
| M37-H3-7 | 8.4 | 0.13 | -7.80 |
| M37-H3-8 | 8.4 | 0.09 | -7.76 |
| M37-H4-1 | 19.0 | 0.18 | -8.23 |
| M37-H4-2 | 19.0 | 0.12 | -8.29 |
| M37-H4-3 | 19.0 | 0.23 | -8.31 |
| M37-H4-4 | 19.0 | 0.18 | -8.32 |
| M37-H4-5 | 19.0 | 0.25 | -8.44 |
| M37-H4-6 | 19.0 | -0.16 | -8.40 |
| M37-H4-7 | 19.0 | -0.05 | -8.34 |
| M37-H4-8 | 19.0 | -0.06 | -8.33 |
| M37-H5-1 | 26.8 | -0.58 | -8.27 |
| M37-H5-2 | 26.8 | -0.64 | -8.29 |
| M37-H5-3 | 26.8 | -0.58 | -8.29 |
| M37-H5-4 | 26.8 | -0.33 | -8.29 |
| M37-H5-5 | 26.8 | -0.31 | -8.35 |
| M37-H5-6 | 26.8 | -0.20 | -8.33 |
| M37-H5-7 | 26.8 | -0.34 | -8.29 |
| M37-H5-8 | 26.8 | -0.44 | -8.22 |
| M37-H6-1 | 45.0 | -0.52 | -8.33 |
| M37-H6-2 | 45.0 | -0.69 | -8.49 |
| M37-H6-3 | 45.0 | -0.67 | -8.47 |
| M37-H6-4 | 45.0 | -0.66 | -8.58 |
| M37-H6-5 | 45.0 | -0.77 | -8.52 |
| M37-H6-6 | 45.0 | -0.88 | -8.59 |
| M37-H6-7 | 45.0 | -0.94 | -8.38 |
| M37-H6-8 | 45.0 | -0.97 | -8.35 |
| M37-H7-1 | 50.0 | -1.37 | -8.52 |
| M37-H7-2 | 50.0 | -1.37 | -8.60 |
| M37-H7-3 | 50.0 | -1.47 | -8.66 |
| M37-H7-4 | 50.0 | -1.28 | -8.59 |
| M37-H7-5 | 50.0 | -1.31 | -8.63 |
| M37-H7-6 | 50.0 | -1.25 | -8.70 |
| M37-H7-7 | 50.0 | -1.15 | -8.88 |
| M37-H7-8 | 50.0 | -1.07 | -8.84 |
| M37-H8-1 | 62.5 | -0.94 | -8.46 |
| M37-H8-2 | 62.5 | -1.07 | -8.58 |
| M37-H8-3 | 62.5 | -1.08 | -8.57 |
| M37-H8-4 | 62.5 | -1.25 | -8.50 |
| M37-H8-5 | 62.5 | -1.23 | -8.56 |
| M37-H8-6 | 62.5 | -1.40 | -8.54 |
| M37-H8-7 | 62.5 | -1.35 | -8.57 |
| M37-H8-8 | 62.5 | -1.19 | -8.60 |
| M37-H9-1 | 75.0 | 0.60 | -8.89 |
| M37-H9-2 | 75.0 | 0.71 | -8.90 |
| M37-H9-3 | 75.0 | 0.63 | -8.85 |
| M37-H9-4 | 75.0 | 0.63 | -8.81 |
| M37-H9-5 | 75.0 | 0.71 | -8.81 |
| M37-H9-6 | 75.0 | 0.79 | -8.87 |
| M37-H9-7 | 75.0 | 0.72 | -8.85 |
| M37-H9-8 | 75.0 | 0.77 | -8.88 |
| M37-H10-1 | 85.0 | 2.45 | -9.16 |
| M37-H10-2 | 85.0 | 2.71 | -9.13 |
| M37-H10-3 | 85.0 | 2.39 | -9.14 |
| M37-H10-4 | 85.0 | 2.47 | -9.17 |
| M37-H10-5 | 85.0 | 2.81 | -9.09 |
| M37-H10-6 | 85.0 | 2.99 | -8.97 |
| M37-H10-7 | 85.0 | 2.53 | -9.09 |
| M37-H10-8 | 85.0 | 2.92 | -9.05 |