Winn, Kyaw; Erlenkeuser, Helmut; Nordberg, Kjell; Gustafsson, Mikael (1998): Stable isotopes measured on Ammonia beccarii from sediment core GIK12594-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.695500, 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: 55.085830 * Longitude: 11.015500
Date/Time Start: 1994-01-29T00:00:00 * Date/Time End: 1994-01-29T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 2.35 m
Event(s):
GIK12594-2 * Latitude: 55.085830 * Longitude: 11.015500 * Date/Time: 1994-01-29T00:00:00 * Elevation: -39.6 m * Recovery: 2.55 m * Location: Großer Belt, Nord-Langelandbelt * Campaign: GIK-cruise * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 0-20 cm:dark grey, fine to medium grained clayey sand; 20-41 cm:dark grey to grey sand; 41-90.5 cm:fine grained sand with peat and wood pieces abundant 86-90.5 cm; 90.5-104 cm:grey sandiger clay with shell fragments; 104-110.8 cm:sandy clay with small shells, abundant scattered peat and layers rich in organic matter (0-110.8 is Unit E); 110.8-142.5 cm (transition Unit E to D):more lightly laminated, grey clays with scattered pieces of peat, forming layers around 129 cm; 142.5-253 cm Unit D):thin alternations of light grey to grey, fine to medium grained sands, calcareous as above, with grey clays (mm-thick laminations, varve-like).
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:
128 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 [#] (>250 µm fraction) | 16 A. beccarii s δ18O [‰ PDB] (125-200 µm fraction) | 17 A. beccarii s δ18O [‰ PDB] (200-250 µm fraction) | 18 A. beccarii s δ18O [‰ PDB] (>250 µm fraction) | 19 A. beccarii s δ13C [‰ PDB] (125-200 µm fraction) | 20 A. beccarii s δ13C [‰ PDB] (200-250 µm fraction) | 21 A. beccarii s δ13C [‰ PDB] (>250 µm fraction) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.01 | 84.9 | |||||||||||||||||||
| 0.29 | 89.9 | |||||||||||||||||||
| 0.59 | 91.9 | |||||||||||||||||||
| 0.89 | 59.6 | 17 | 13 | -3.41 | -3.01 | -0.68 | -0.31 | 17 | 11 | -2.91 | -2.75 | -0.11 | -0.32 | |||||||
| 0.90 | 105 | -2.49 | -0.39 | 215 | -2.48 | -0.33 | ||||||||||||||
| 1.09 | 73.1 | 40.3 | 171 | 172 | -2.73 | -2.50 | -0.22 | -0.19 | 200 | 242 | -2.75 | -2.37 | -0.37 | -0.18 | ||||||
| 1.19 | 30.8 | 42.0 | 120 | 35 | -2.78 | -2.60 | -0.49 | -0.50 | 200 | 45 | -2.91 | -2.44 | -0.47 | -0.33 | ||||||
| 1.29 | 57.1 | 38.2 | 72 | 10 | -3.00 | -2.99 | -0.27 | -0.37 | 108 | 16 | -2.91 | -2.74 | -0.56 | 0.09 | ||||||
| 1.39 | 18.0 | 36.7 | 48 | 32 | -3.06 | -2.36 | -0.51 | -0.44 | 95 | 27 | -3.10 | -2.31 | -0.84 | -0.18 | ||||||
| 1.69 | 50.8 | 40.3 | 228 | 39 | -4.34 | -3.31 | -1.30 | -0.75 | 124 | 55 | -3.38 | -2.98 | -0.84 | -0.62 | ||||||
| 1.99 | 45.3 | 55.0 | 206 | 19 | -5.39 | -4.74 | -1.80 | -1.72 | 185 | 26 | -5.34 | -4.68 | -1.72 | -1.43 | ||||||
| 2.29 | 18.9 | 51.7 | 62 | -4.40 | -1.45 | 54 | -3.84 | -1.19 | ||||||||||||
| 2.35 | 28.5 | 57.3 | 162 | 19 | -5.79 | -5.85 | -2.38 | -2.06 | 133 | 15 | -5.73 | -5.73 | -2.47 | -1.99 |