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Lamping, Nele; Müller, Juliane; Esper, Oliver; Hillenbrand, Claus-Dieter; Smith, James A; Kuhn, Gerhard (2019): Winter sea ice concentrations derived from diatom transfer functions on sediment core PS69/274-1 from the western Amundsen Sea, Antarctic [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.904163, In supplement to: Lamping, N et al. (2020): Highly branched isoprenoids reveal onset of deglaciation followed by dynamic sea-ice conditions in the western Amundsen Sea, Antarctica. Quaternary Science Reviews, 228, 106103, https://doi.org/10.1016/j.quascirev.2019.106103

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Abstract:
Via a transfer function, we reconstructed winter sea ice concentrations derived from diatom assemblages on sediment core PS69/274-1 from the western Amundsen Sea, Antarctica. Those data were compared to sea ice reconstructions based on biomarker data.
Keyword(s):
Antarctica; palaeoclimatology; Sea ice
Coverage:
Latitude: -73.855900 * Longitude: -117.775700
Date/Time Start: 2006-03-07T02:48:00 * Date/Time End: 2006-03-07T02:48:00
Minimum DEPTH, sediment/rock: 0.04 m * Maximum DEPTH, sediment/rock: 2.94 m
Event(s):
PS69/274-1 * Latitude: -73.855900 * Longitude: -117.775700 * Date/Time: 2006-03-07T02:48:00 * Elevation: -1452.0 m * Recovery: 4.53 m * Campaign: ANT-XXIII/4 (PS69) * Basis: Polarstern * Method/Device: Gravity corer (GC) * Comment: 5 core sections: 0-0.53, 0.53-1.53, 1.53-2.53, 2.53-3.53, 3.53-4.53 m
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmLamping, NeleGeocode – mbsf
Sea ice concentration, winterSea ice con winter%Lamping, NeleModern analog technique (MAT)
Size:
34 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Depth sed [m]

Sea ice con winter [%]
0.0485.49
0.1482.81
0.2487.52
0.3473.45
0.4489.09
0.5488.41
0.6482.45
0.7491.10
0.8485.36
0.9491.82
1.0491.29
1.1485.36
1.2490.75
1.3490.57
1.4491.17
1.5477.00
1.6484.46
1.7484.55
1.8488.54
1.8991.26
1.9490.22
1.9883.48
2.0478.26
2.0979.37
2.1479.58
2.1876.50
2.2467.40
2.2973.06
2.3472.82
2.3879.28
2.4490.08
2.5488.86
2.8489.28
2.9483.39