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