Hultzsch, Nadja (2007): Clay mineral composition of sediment core Lz1005 (Table A19) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.611257, In supplement to: Hultzsch, Nadja; Wagner, Bernd; Diekmann, Bernhard; White, Duanne A (2008): Mineralogical implications for the Late Pleistocene glaciation in Amery Oasis, East Antarctica, from a lake sediment core. Antarctic Science, 20(02), 169-172, https://doi.org/10.1017/S0954102007000880
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Hultzsch, Nadja (2007): Lakustrine Sedimente als Archive des spätquartären Umweltwandels in der Amery-Oase, Ostantarktis (The Late Quaternary climatic and environmental history of Amery Oasis, East Antarctica). Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 545, 168 pp, https://doi.org/10.2312/BzPM_0545_2007
Project(s):
Permafrost Research (Periglacial Dynamics) @ AWI (AWI_PerDyn)
Coverage:
Latitude: -70.555400 * Longitude: 68.025660
Date/Time Start: 2001-12-29T00:00:00 * Date/Time End: 2001-12-31T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 5.54 m
Event(s):
Lz1005 * Latitude: -70.555400 * Longitude: 68.025660 * Date/Time Start: 2001-12-29T00:00:00 * Date/Time End: 2001-12-31T00:00:00 * Lake water depth: 30.5 m * Location: Lake Terrasovoje, East Antarctica * Campaign: AmeryOasis2001/2002 * Basis: Sampling/drilling in lake * Method/Device: Composite Core (COMPCORE)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Depth, composite | Depth comp | mcd | Diekmann, Bernhard | Intercore correlation | |
3 | Sample code/label | Sample label | Diekmann, Bernhard | |||
4 | Smectite | Sme | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
5 | Illite | Ill | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
6 | Kaolinite | Kln | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
7 | Chlorite | Chl | % | Diekmann, Bernhard | X-ray diffraction, clay fraction | |
8 | Mica 5Å/10Å | Mica 5Å/10Å | Diekmann, Bernhard | Calculated | ||
9 | Quartz/Feldspar ratio | Qz/Fsp | Diekmann, Bernhard | Calculated | ||
10 | Plagioclase/Kalifeldspar ratio | Pl/Kfs | Diekmann, Bernhard | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
555 data points
Data
1 Depth sed [m] | 2 Depth comp [mcd] | 3 Sample label | 4 Sme [%] | 5 Ill [%] | 6 Kln [%] | 7 Chl [%] | 8 Mica 5Å/10Å | 9 Qz/Fsp | 10 Pl/Kfs |
---|---|---|---|---|---|---|---|---|---|
0.01 | 0.01 | Lz1005-1 | 0.99 | 1.85 | |||||
0.02 | 0.02 | Lz1005-1 | 1.51 | 1.58 | |||||
0.03 | 0.03 | Lz1005-1 | 1.17 | 1.77 | |||||
0.04 | 0.04 | Lz1005-1 | 1.13 | 1.64 | |||||
0.06 | 0.06 | Lz1005-1 | 10.14 | 62.21 | 22.63 | 5.01 | 0.14 | ||
0.07 | 0.07 | Lz1005-1 | 17.06 | 54.98 | 23.82 | 4.13 | 0.14 | 0.88 | 1.94 |
0.09 | 0.09 | Lz1005-1 | 14.56 | 58.32 | 21.47 | 5.66 | 0.14 | ||
0.10 | 0.10 | Lz1005-1 | 16.05 | 57.75 | 21.23 | 4.96 | 0.13 | ||
0.11 | 0.11 | Lz1005-1 | 1.51 | 2.00 | |||||
0.15 | 0.15 | Lz1005-1 | 19.03 | 58.41 | 18.07 | 4.49 | 0.11 | ||
0.17 | 0.17 | Lz1005-1 | 1.21 | 1.96 | |||||
0.25 | 0.25 | Lz1005-1 | 13.79 | 60.86 | 19.49 | 5.86 | 0.12 | ||
0.26 | 0.26 | Lz1005-1 | 0.91 | 1.75 | |||||
0.29 | 0.29 | Lz1005-1 | 0.87 | 1.83 | |||||
0.31 | 0.31 | Lz1005-1 | 12.94 | 59.63 | 21.86 | 5.57 | 0.24 | ||
0.32 | 0.32 | Lz1005-1 | 4.90 | 63.60 | 25.46 | 6.05 | 0.30 | 1.01 | 1.86 |
0.53 | 0.36 | Lz1005-2 | 9.40 | 64.66 | 21.84 | 4.10 | 0.35 | 1.60 | 1.12 |
0.57 | 0.40 | Lz1005-2 | 0.97 | 1.82 | |||||
0.59 | 0.42 | Lz1005-2 | 12.97 | 57.76 | 23.22 | 6.05 | 0.17 | ||
0.62 | 0.45 | Lz1005-2 | 1.06 | 1.70 | |||||
0.63 | 0.46 | Lz1005-2 | 11.67 | 60.61 | 20.89 | 6.83 | 0.27 | ||
0.67 | 0.50 | Lz1005-2 | 0.85 | 2.12 | |||||
0.69 | 0.52 | Lz1005-2 | 3.76 | 68.98 | 22.89 | 4.37 | 0.14 | ||
0.73 | 0.56 | Lz1005-2 | 9.71 | 62.78 | 20.08 | 7.43 | 0.09 | ||
0.75 | 0.58 | Lz1005-2 | 1.01 | 1.65 | |||||
0.79 | 0.62 | Lz1005-2 | 6.54 | 64.04 | 22.34 | 7.09 | 0.13 | ||
0.83 | 0.66 | Lz1005-2 | 10.75 | 62.71 | 22.15 | 4.40 | 0.16 | ||
0.86 | 0.69 | Lz1005-2 | 1.05 | 1.35 | |||||
0.87 | 0.70 | Lz1005-2 | 5.67 | 64.04 | 23.82 | 6.47 | 0.19 | ||
0.95 | 0.78 | Lz1005-2 | 6.69 | 64.54 | 22.79 | 5.98 | 0.13 | ||
1.04 | 0.87 | Lz1005-2 | 1.02 | 1.73 | |||||
1.15 | 0.98 | Lz1005-2 | 7.69 | 62.26 | 23.56 | 6.50 | 0.13 | ||
1.29 | 1.12 | Lz1005-2 | 3.44 | 66.79 | 24.83 | 4.94 | 0.14 | 1.22 | 1.65 |
1.85 | 1.68 | Lz1005-2 | 12.06 | 61.45 | 22.59 | 3.90 | 0.12 | ||
2.24 | 2.07 | Lz1005-2 | 0.91 | 1.83 | |||||
2.25 | 2.08 | Lz1005-2 | 6.76 | 61.79 | 25.65 | 5.80 | 0.15 | ||
2.37 | 2.20 | Lz1005-2 | 6.82 | 64.54 | 22.81 | 5.83 | 0.15 | ||
2.43 | 2.26 | Lz1005-2 | 8.99 | 60.98 | 23.11 | 6.92 | 0.17 | 1.02 | 1.59 |
2.49 | 2.32 | Lz1005-2 | 8.06 | 62.46 | 23.24 | 6.23 | 0.17 | ||
2.50 | 2.48 | Lz1005-3 | 7.31 | 62.00 | 25.70 | 4.99 | 0.16 | ||
2.51 | 2.49 | Lz1005-3 | 1.29 | 1.89 | |||||
2.53 | 2.36 | Lz1005-2 | 1.28 | 1.89 | |||||
2.54 | 2.52 | Lz1005-3 | 8.23 | 62.65 | 22.83 | 6.28 | 0.13 | ||
2.55 | 2.38 | Lz1005-2 | 14.02 | 60.60 | 20.55 | 4.84 | 0.14 | ||
2.56 | 2.54 | Lz1005-3 | 0.86 | 2.26 | |||||
2.60 | 2.43 | Lz1005-2 | 7.80 | 58.90 | 28.86 | 4.45 | 0.22 | 1.16 | 1.71 |
2.60 | 2.58 | Lz1005-3 | 10.55 | 60.75 | 23.45 | 5.25 | 0.13 | ||
2.62 | 2.60 | Lz1005-3 | 0.93 | 1.27 | |||||
2.72 | 2.70 | Lz1005-3 | 1.20 | 3.09 | |||||
2.74 | 2.72 | Lz1005-3 | 7.00 | 63.65 | 23.62 | 5.73 | 0.16 | 1.14 | 2.16 |
2.84 | 2.82 | Lz1005-3 | 46.93 | 43.61 | 6.26 | 3.21 | 0.08 | 1.15 | 1.27 |
2.94 | 2.92 | Lz1005-3 | 39.64 | 45.00 | 9.23 | 6.12 | 0.10 | 1.15 | 1.57 |
3.05 | 3.03 | Lz1005-3 | 44.77 | 42.83 | 5.59 | 6.80 | 0.08 | 1.22 | 1.57 |
3.12 | 3.10 | Lz1005-3 | 1.60 | 2.00 | |||||
3.14 | 3.12 | Lz1005-3 | 46.37 | 40.50 | 7.67 | 5.45 | 0.12 | ||
3.24 | 3.22 | Lz1005-3 | 36.54 | 47.44 | 7.93 | 8.10 | 0.17 | 1.07 | 1.79 |
3.34 | 3.32 | Lz1005-3 | 52.56 | 33.57 | 7.36 | 6.51 | 0.14 | 1.07 | 1.59 |
3.44 | 3.42 | Lz1005-3 | 53.09 | 35.08 | 6.27 | 5.56 | 0.15 | 1.13 | 1.80 |
3.54 | 3.52 | Lz1005-3 | 52.76 | 35.62 | 4.85 | 6.78 | 0.10 | 1.04 | 1.76 |
3.64 | 3.62 | Lz1005-3 | 54.35 | 33.47 | 5.85 | 6.32 | 0.10 | 1.07 | 1.74 |
3.74 | 3.72 | Lz1005-3 | 48.98 | 38.85 | 4.85 | 7.32 | 0.20 | 0.83 | 1.41 |
3.84 | 3.82 | Lz1005-3 | 55.99 | 31.65 | 5.87 | 6.50 | 0.17 | 1.21 | 1.54 |
3.94 | 3.92 | Lz1005-3 | 54.26 | 33.20 | 5.63 | 6.91 | 0.19 | 1.15 | 2.04 |
4.05 | 4.03 | Lz1005-3 | 50.12 | 36.24 | 6.38 | 7.26 | 0.12 | 0.96 | 1.60 |
4.15 | 4.13 | Lz1005-3 | 52.92 | 33.83 | 6.48 | 6.78 | 0.10 | 1.18 | 1.39 |
4.25 | 4.23 | Lz1005-3 | 55.65 | 36.68 | 5.16 | 2.51 | 0.15 | 0.64 | 1.25 |
4.35 | 4.33 | Lz1005-3 | 50.20 | 37.94 | 6.70 | 5.16 | 0.15 | 1.31 | 2.07 |
4.45 | 4.43 | Lz1005-3 | 36.54 | 50.15 | 9.89 | 3.43 | 0.16 | 0.96 | 1.87 |
4.55 | 4.53 | Lz1005-3 | 26.16 | 60.75 | 7.90 | 5.19 | 0.17 | 0.97 | 1.31 |
4.65 | 4.63 | Lz1005-3 | 31.84 | 55.54 | 7.31 | 5.32 | 0.11 | 1.09 | 1.57 |
4.75 | 4.73 | Lz1005-3 | 38.88 | 46.98 | 7.98 | 6.16 | 0.13 | 1.00 | 1.68 |
4.85 | 4.83 | Lz1005-3 | 36.18 | 50.95 | 7.20 | 5.67 | 0.13 | 0.86 | 1.72 |
4.95 | 4.93 | Lz1005-3 | 0.88 | 1.52 | |||||
5.04 | 5.02 | Lz1005-4 | 39.34 | 49.35 | 6.45 | 4.86 | 0.12 | 0.61 | 1.32 |
5.14 | 5.12 | Lz1005-4 | 37.10 | 51.18 | 7.53 | 4.19 | 0.11 | 0.75 | 1.08 |
5.24 | 5.22 | Lz1005-4 | 46.52 | 43.17 | 6.20 | 4.12 | 0.10 | 0.87 | 1.37 |
5.34 | 5.32 | Lz1005-4 | 54.04 | 37.85 | 5.83 | 2.27 | 0.14 | 0.98 | 1.28 |
5.42 | 5.40 | Lz1005-4 | 1.21 | 1.60 | |||||
5.44 | 5.42 | Lz1005-4 | 68.89 | 25.06 | 3.87 | 2.19 | 0.24 | ||
5.54 | 5.52 | Lz1005-4 | 51.42 | 37.92 | 5.17 | 5.48 | 0.08 | 1.04 | 1.55 |