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Melles, Martin (1991): Sedimentology of core PS1494-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51666, In supplement to: Melles, M (1991): Paläoglaziologie und Paläozeanographie im Spätquartär am Kontinentalrand des südlichen Weddellmeeres, Antarktis (Late Quaternary paleoglaciology and paleoceanography at the continental margin of the southern Weddell Sea, Antarctica). Berichte zur Polarforschung = Reports on Polar Research, 81, 190 pp, https://doi.org/10.2312/BzP_0081_1991

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Coverage:
Latitude: -74.181830 * Longitude: -35.500500
Date/Time Start: 1987-02-11T20:18:00 * Date/Time End: 1987-02-11T20:18:00
Minimum DEPTH, sediment/rock: 0.06 m * Maximum DEPTH, sediment/rock: 3.01 m
Event(s):
PS1494-2 (PS10/760) * Latitude: -74.181830 * Longitude: -35.500500 * Date/Time: 1987-02-11T20:18:00 * Elevation: -1942.0 m * Penetration: 3.3 m * Recovery: 3.02 m * Location: Filchner Trough * Campaign: ANT-V/4 (PS10) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 4 core sections: 0-0.33, 0.33-1.33, 1.33-2.02, 2.02-3.02 m; Korrektur fuer die Tiefe der Grobkornlage in PS1494: die von Melles angegebene composite depth bei 135 cmcd entspricht 96 cmbsf in PS1494-2 SL, denn die Basis des 41 cm langen GKG wurde mit der SL-Tiefe bei 2 cm verspleist.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2Depth, compositeDepth compmcdMelles, Martin
3Ice rafted debris, generalIRDarbitrary unitsMelles, Martincalculated as mean of a 3 cm thick horizon
4Size fraction > 2 mm, gravel>2 mm%Melles, MartinGrain size, sieving
5SandSand%Melles, MartinGrain size, sieving
6SiltSilt%Melles, MartinGrain size, sieving
7Size fraction < 0.002 mm, clay<2 µm%Melles, MartinGrain size, sieving/settling tube
8Neogloboquadrina pachyderma sinistral, δ18ON. pachyderma s δ18O‰ PDBMelles, MartinMass spectrometer Finnigan MAT 251
9Neogloboquadrina pachyderma sinistral, δ13CN. pachyderma s δ13C‰ PDBMelles, MartinMass spectrometer Finnigan MAT 251
Size:
136 data points

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