Winn, Kyaw; Erlenkeuser, Helmut; Nordberg, Kjell; Gustafsson, Mikael (1998): Stable isotopes measured on Ammonia beccarii from sediment core GIK12523-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.695501, In supplement to: Winn, K et al. (1998): Paleohydrography of the Great Belt, Denmark, during the Littorina Transgression: the isotope signal. Meyniana, 50, 237-251, https://doi.org/10.2312/meyniana.1998.50.237
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Coverage:
Latitude: 55.404000 * Longitude: 10.992000
Date/Time Start: 1972-11-15T00:00:00 * Date/Time End: 1972-11-15T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 2.99 m
Event(s):
GIK12523-1 * Latitude: 55.404000 * Longitude: 10.992000 * Date/Time: 1972-11-15T00:00:00 * Elevation: -23.5 m * Recovery: 3.005 m * Location: Great Belt, western Baltic Sea, off Denmark * Campaign: GIK-cruise * Method/Device: Box corer (BC) * Comment: 0-19.8 cm: dark olive grey, very soft muddy sand (Unit G); 19.8-30 cm: dark grey compacter muddy sand (Unit D); 30-152 cm: grey, clay with light to dark grey at 66-68 cm, and shell fragments, abundant at 91.3-92.2 cm, 143.6-146.5 cm (Unit D); 152-300.5 cm clay as above, shell layers at 161.5-163.3 cm, 200-210 cm (Cerastoderma sp., more compact below 163 cm.
Comment:
Stable isotopes were measured with VG and MAT251 mass spectrometers.
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
300 data points
Data
| 1 Depth sed [m] | 2 >63 µm [%] | 3 Coiling ratio [%] (of Ammonia beccarii) | 4 A. beccarii d [#] (125-200 µm fraction) | 5 A. beccarii d [#] (200-250 µm fraction) | 6 A. beccarii d [#] (> 250 µm fraction) | 7 A. beccarii d δ18O [‰ PDB] (125-200 µm fraction) | 8 A. beccarii d δ18O [‰ PDB] (200-250 µm fraction) | 9 A. beccarii d δ18O [‰ PDB] (> 250 µm fraction) | 10 A. beccarii d δ13C [‰ PDB] (125-200 µm fraction) | 11 A. beccarii d δ13C [‰ PDB] (200-250 µm fraction) | 12 A. beccarii d δ13C [‰ PDB] (> 250 µm fraction) | 13 A. beccarii s [#] (125-200 µm fraction) | 14 A. beccarii s [#] (200-250 µm fraction) | 15 A. beccarii s δ18O [‰ PDB] (125-200 µm fraction) | 16 A. beccarii s δ18O [‰ PDB] (200-250 µm fraction) | 17 A. beccarii s δ13C [‰ PDB] (125-200 µm fraction) | 18 A. beccarii s δ13C [‰ PDB] (200-250 µm fraction) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.01 | 71.6 | 11.8 | 1 | -2.95 | -0.93 | 2 | 6 | -0.18 | -0.04 | ||||||||
| 0.09 | 72.3 | 53.0 | |||||||||||||||
| 0.19 | 76.2 | ||||||||||||||||
| 0.31 | 53.9 | 35.3 | 11 | 13 | -3.04 | -2.32 | -0.06 | -0.18 | 20 | 15 | -2.64 | -2.95 | -0.49 | -0.02 | |||
| 0.41 | 50.7 | 38.0 | 22 | 15 | -3.29 | -0.58 | 21 | 15 | -2.35 | -2.46 | -0.29 | -0.59 | |||||
| 0.59 | 39.0 | 32.3 | 20 | 16 | -3.29 | -3.75 | -1.36 | -1.02 | 20 | 15 | -2.68 | -2.68 | -1.16 | -0.74 | |||
| 0.71 | 51.0 | 37.3 | 21 | 15 | -3.68 | -2.49 | -1.45 | -0.50 | 20 | 15 | -3.04 | -3.06 | -1.15 | -1.03 | |||
| 0.89 | 51.6 | 39.3 | 23 | 16 | -2.82 | -2.87 | -0.87 | -0.66 | 27 | 15 | -3.00 | -2.92 | -0.94 | -0.57 | |||
| 1.01 | 35.7 | 35.7 | 20 | 16 | -3.11 | -2.95 | -0.89 | -1.05 | 20 | 17 | -3.07 | -2.94 | -1.33 | -0.87 | |||
| 1.02 | 98 | -2.79 | -0.84 | 170 | -2.94 | -0.82 | |||||||||||
| 1.19 | 38.6 | 35.0 | 176 | 42 | -2.74 | -2.67 | -0.90 | -0.57 | 58 | 200 | -2.88 | -2.69 | -0.65 | -0.87 | |||
| 1.31 | 53.1 | 40.3 | 153 | 20 | -3.40 | -2.97 | -1.11 | -0.98 | 222 | -3.20 | -0.88 | ||||||
| 1.49 | 26.8 | 45.7 | 195 | 27 | -4.92 | -4.23 | -2.11 | -1.60 | 200 | 26 | -3.69 | -3.30 | -1.53 | -1.30 | |||
| 1.61 | 56.0 | 48.0 | 200 | 17 | -5.05 | -5.22 | -4.73 | -2.07 | -1.64 | -1.88 | 150 | 88 | -5.33 | -5.22 | -1.99 | -1.64 | |
| 1.69 | 20.0 | 56.3 | 108 | -4.79 | -2.04 | 88 | 7 | -4.04 | -3.56 | -1.68 | -1.18 | ||||||
| 1.79 | 23.0 | 52.0 | 226 | 13 | -5.84 | -5.23 | -2.61 | -2.37 | 183 | 9 | -5.55 | -2.66 | |||||
| 1.91 | 24.5 | 62.7 | 123 | 5 | -5.77 | -5.41 | -2.80 | -2.99 | 104 | 6 | -5.42 | -5.87 | -2.59 | -3.00 | |||
| 2.09 | 24.3 | 60.3 | 200 | 119 | -6.28 | -5.94 | -2.76 | -3.10 | 200 | 18 | -6.22 | -6.13 | -2.82 | -3.20 | |||
| 2.21 | 24.4 | 62.0 | 200 | 24 | -5.93 | -6.00 | -3.34 | -3.21 | 175 | 19 | -5.88 | -6.17 | -3.38 | -3.99 | |||
| 2.22 | 22 | 18 | -5.96 | -6.59 | -2.80 | -2.63 | 20 | 16 | -6.08 | -6.29 | -3.38 | -4.07 | |||||
| 2.39 | 17.3 | 56.0 | 20 | 9 | -5.78 | -6.03 | -2.68 | -3.19 | 19 | 10 | -6.13 | -5.99 | -2.53 | -2.33 | |||
| 2.51 | 9.1 | 60.0 | 18 | 15 | -6.32 | -5.84 | -2.62 | -3.07 | 8 | 5 | -6.15 | -2.84 | |||||
| 2.69 | 25.7 | 63.0 | 22 | 15 | -6.08 | -6.01 | -2.37 | -2.64 | 20 | 10 | -6.14 | -5.81 | -2.62 | -3.20 | |||
| 2.81 | 15.1 | 54.3 | 10 | 15 | -6.30 | -6.12 | -2.54 | -3.36 | 13 | 7 | -5.73 | -5.35 | -2.30 | -2.53 | |||
| 2.99 | 7.7 | 60.3 | 24 | 11 | -6.29 | -5.90 | -3.26 | -3.21 | 20 | 11 | -5.84 | -5.66 | -3.18 | -2.90 |