Atar, Elizabeth; März, Christian; Aplin, Andrew C; Dellwig, Olaf; Herringshaw, Liam; Lamoureux-Var, Violaine; Leng, Melanie J; Schnetger, Bernhard; Wagner, Thomas (2019): Sulfur concentration from the Ebberston 87 Core (Cleveland Basin, Yorkshire, UK) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.903742, In supplement to: Atar, Elizabeth; März, Christian; Aplin, Andrew C; Dellwig, Olaf; Herringshaw, Liam G; Lamoureux-Var, Violaine; Leng, Melanie J; Schnetger, Bernhard; Wagner, Thomas (2019): Dynamic climate-driven controls on the deposition of the Kimmeridge Clay Formation in the Cleveland Basin, Yorkshire, UK. Climate of the Past, 15(4), 1581-1601, https://doi.org/10.5194/cp-15-1581-2019
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Coverage:
Latitude: 54.230000 * Longitude: -0.623000
Minimum DEPTH, sediment/rock: 31.07 m * Maximum DEPTH, sediment/rock: 72.00 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Atar, Elizabeth | Geocode | |
| 2 | Sulfur, total | TS | % | Atar, Elizabeth |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
50 data points
Data
| 1 Depth sed [m] | 2 TS [%] |
|---|---|
| 31.07 | 1.44 |
| 32.57 | 0.94 |
| 33.17 | 1.28 |
| 34.17 | 1.28 |
| 35.67 | 0.75 |
| 36.92 | 6.94 |
| 37.10 | 3.48 |
| 37.30 | 2.44 |
| 37.50 | 1.70 |
| 37.70 | 2.01 |
| 37.90 | 2.04 |
| 38.50 | 3.85 |
| 39.50 | 3.50 |
| 40.50 | 1.67 |
| 42.50 | 0.84 |
| 44.00 | 1.12 |
| 45.10 | 0.26 |
| 45.50 | 1.26 |
| 45.80 | 1.08 |
| 46.20 | 1.03 |
| 46.30 | 1.65 |
| 46.50 | 3.62 |
| 46.70 | 2.67 |
| 46.90 | 0.34 |
| 47.50 | 1.98 |
| 48.50 | 1.43 |
| 49.50 | 1.56 |
| 50.00 | 1.02 |
| 51.00 | 0.40 |
| 52.50 | 0.99 |
| 53.30 | 0.21 |
| 54.30 | 0.96 |
| 55.70 | 0.19 |
| 57.20 | 0.70 |
| 58.20 | 0.70 |
| 59.70 | 1.25 |
| 62.00 | 0.82 |
| 63.00 | 0.97 |
| 64.50 | 1.11 |
| 65.50 | 3.08 |
| 65.70 | 3.64 |
| 65.90 | 2.51 |
| 66.10 | 1.40 |
| 66.30 | 3.64 |
| 66.50 | 0.97 |
| 67.50 | 0.94 |
| 68.50 | 2.03 |
| 69.50 | 0.93 |
| 70.50 | 1.19 |
| 72.00 | 1.36 |