Jenkyns, Hugh C; Gröcke, Darren R; Hesselbo, Stephen P (2001): Stable isotopic composition of Pliensbachian-Toarcian samples from Winterborne Kingston Borehole, Dorset, Wessex Basin [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.846586, In supplement to: Jenkyns, HC et al. (2001): Nitrogen isotope evidence for water mass denitrification during the Early Toarcian (Jurassic) oceanic anoxic event. Paleoceanography, 16(6), 593-603, https://doi.org/10.1029/2000PA000558
Always quote citation above when using data! You can download the citation in several formats below.
Other version:
Gröcke, Darren R; Hesselbo, Stephen P; Jenkyns, Hugh C (2003): Lower Jurassic Stable Isotope and Chemical Data. NOAA National Centers for Environmental Information, https://doi.org/10.25921/NC2J-QB03
Coverage:
Latitude: 50.780000 * Longitude: -2.200000
Minimum SECTION, height: 1100.09 m * Maximum SECTION, height: 1118.69 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Jenkyns, Hugh C | |||
| 2 | SECTION, height | Section | m | Jenkyns, Hugh C | Geocode | |
| 3 | δ13C, organic carbon | δ13C Corg | ‰ PDB | Jenkyns, Hugh C | Isotope ratio mass spectrometry | |
| 4 | δ13C, carbonate | δ13C carb | ‰ PDB | Jenkyns, Hugh C | Isotope ratio mass spectrometry | |
| 5 | δ15N | δ15N | ‰ air | Jenkyns, Hugh C | Isotope ratio mass spectrometry | |
| 6 | Carbon, organic, total | TOC | % | Jenkyns, Hugh C | Coulomat 702 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
217 data points
Data
| 1 Sample label | 2 Section [m] | 3 δ13C Corg [‰ PDB] | 4 δ13C carb [‰ PDB] | 5 δ15N [‰ air] | 6 TOC [%] |
|---|---|---|---|---|---|
| wk 44 | 1100.09 | -24.67 | 0.52 | -0.86 | 0.27 |
| wk 43 | 1100.50 | -24.53 | 0.85 | -0.12 | 0.79 |
| wk 42 | 1100.89 | -25.21 | 0.92 | 0.14 | 0.81 |
| wk 41 | 1101.37 | -25.85 | 0.95 | -0.59 | 0.69 |
| wk 40 | 1101.82 | -26.49 | 1.33 | -1.24 | 0.30 |
| wk 39 | 1102.24 | -26.65 | 0.03 | -1.16 | 0.46 |
| wk 38 | 1102.69 | -25.85 | 1.26 | -1.98 | 0.52 |
| wk 37 | 1103.33 | -25.94 | 1.88 | -1.56 | 0.38 |
| wk 36 | 1103.88 | 0.74 | |||
| wk 35 | 1104.02 | -26.18 | 1.97 | -1.26 | 0.45 |
| wk 34 | 1104.35 | -26.43 | 1.75 | -1.32 | 0.28 |
| wk 33 | 1104.74 | -26.08 | 1.75 | -1.09 | 0.62 |
| wk 32 | 1105.15 | -24.95 | 1.75 | -1.31 | 0.78 |
| wk 31 | 1105.61 | -25.54 | 1.97 | -1.47 | 0.78 |
| wk 30 | 1106.06 | -25.77 | 1.72 | -1.69 | 0.55 |
| wk 29 | 1106.47 | -25.24 | 0.93 | -1.95 | 1.08 |
| wk 28 | 1106.89 | -25.55 | 1.66 | -0.83 | 0.39 |
| wk 27 | 1107.33 | -25.63 | 2.27 | -1.89 | 0.74 |
| wk 26 | 1107.75 | -25.71 | 2.06 | -2.12 | 0.85 |
| wk 25 | 1108.19 | -25.97 | 2.36 | -2.89 | 0.56 |
| wk 24 | 1108.65 | -24.81 | 1.56 | -0.53 | 0.24 |
| wk 23 | 1109.07 | -25.46 | 1.87 | -1.40 | 0.42 |
| wk 22 | 1109.45 | -25.59 | 2.52 | -1.72 | 0.81 |
| wk 21 | 1109.84 | -24.82 | 2.90 | -0.43 | 0.82 |
| wk 20 | 1110.28 | -25.11 | 2.71 | -0.65 | 0.72 |
| wk 19 | 1110.71 | -26.60 | 1.36 | -0.46 | 1.13 |
| wk 18 | 1111.13 | -27.53 | 1.52 | -0.07 | 1.09 |
| wk 17 | 1111.56 | -30.28 | -0.84 | 0.41 | 4.18 |
| wk 16 | 1112.00 | -29.45 | -0.87 | 0.88 | 4.08 |
| wk 15 | 1112.44 | -29.17 | -0.41 | 1.50 | 1.99 |
| wk 14 | 1112.88 | -30.85 | -0.70 | 1.48 | 0.91 |
| wk 13 | 1113.33 | -28.75 | -0.24 | 1.34 | 0.69 |
| wk 12 | 1113.78 | -28.10 | -1.95 | -0.27 | 1.22 |
| wk 11 | 1114.20 | -27.69 | -0.04 | -1.04 | 0.60 |
| wk 10 | 1114.60 | -27.75 | -0.16 | -2.12 | 1.11 |
| wk 9 | 1115.00 | -27.12 | -0.41 | -1.31 | 0.37 |
| wk 8 | 1115.39 | -27.01 | 0.58 | -0.38 | 0.22 |
| wk 7 | 1115.81 | -26.81 | -0.25 | -1.08 | 0.16 |
| wk 6 | 1116.27 | -27.12 | -0.09 | 0.04 | 0.24 |
| wk 5 | 1116.72 | -26.98 | -0.14 | 0.00 | 0.82 |
| wk 4 | 1117.18 | -26.23 | -0.50 | -0.44 | 0.63 |
| wk 3 | 1117.69 | -26.32 | -1.11 | -0.67 | 0.47 |
| wk 2 | 1118.22 | -25.68 | -1.69 | -1.42 | 0.32 |
| wk 1 | 1118.69 | -25.43 | -2.00 | -0.84 | 0.71 |