Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Hillenbrand, Claus-Dieter; Baesler, Anja; Grobe, Hannes (2003): Clay mineralogy of sediment core PS2533-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.89698, In supplement to: Hillenbrand, C-D et al. (2005): The sedimentary record of the last glaciation in the western Bellingshausen Sea (West Antarctica): Implications for the interpretation of diamictons in a polar-marine setting. Marine Geology, 216(4), 191-204, https://doi.org/10.1016/j.margeo.2005.01.007

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Related to:
Baesler, Anja (2003): Glazialmarine Sedimentation am westantarktischen Kontinentalrand (zentrales Bellingshausenmeer) im Verlauf des letzten Glazial-Interglazial-Zyklus. Diploma Thesis, Geographisches Institut der Georg-August-Universität zu Göttingen & Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, 60 pp, hdl:10013/epic.6e8162eb-5d28-45ef-8ed7-48152551d3a4
Coverage:
Latitude: -71.025000 * Longitude: -85.898330
Date/Time Start: 1994-02-13T18:50:00 * Date/Time End: 1994-02-13T18:50:00
Minimum DEPTH, sediment/rock: 0.02 m * Maximum DEPTH, sediment/rock: 1.90 m
Event(s):
PS2533-2 (PS29/040) * Latitude: -71.025000 * Longitude: -85.898330 * Date/Time: 1994-02-13T18:50:00 * Elevation: -588.0 m * Penetration: 3 m * Recovery: 1.93 m * Location: Bellingshausen Sea * Campaign: ANT-XI/3 (PS29) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 2 core sections: 0-0.93, 0.93-1.93 m
Size:
140 data points

Data

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


Depth sed [m]

Sme [%]

Ill [%]

Kln [%]

Chl [%]

Qz/Fsp

Ill cryst [d2Theta]

Ill EI
0.0218.554.44.023.11.440.530.33
0.1020.950.15.124.01.420.520.39
0.2022.448.43.725.51.430.490.40
0.3015.554.65.924.01.580.500.41
0.4015.156.84.024.11.350.530.38
0.5010.661.44.024.11.630.510.35
0.608.162.83.026.21.700.520.37
0.706.463.95.723.91.760.500.39
0.8010.859.03.726.41.640.500.35
0.909.961.24.224.81.640.480.36
1.009.261.73.725.41.730.490.38
1.1010.461.53.724.41.720.490.36
1.2011.158.53.127.41.600.480.38
1.308.460.25.126.41.560.490.41
1.408.162.44.125.41.560.520.35
1.509.361.44.325.01.770.490.35
1.608.860.66.024.61.720.470.37
1.7011.757.85.025.51.550.510.41
1.808.962.13.425.71.610.480.32
1.9011.059.14.625.31.510.480.35