Hultzsch, Nadja (2007): Bulk mineral composition of sediment core Lz1005 (Table A14) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.611252, 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 | Quartz | Qz | # | Diekmann, Bernhard | X-ray diffraction, bulk mineralogy | |
5 | Plagioclase | Pl | % | Diekmann, Bernhard | X-ray diffraction, bulk mineralogy | |
6 | Kalifeldspar | Kfs | % | Diekmann, Bernhard | X-ray diffraction, bulk mineralogy | |
7 | Feldspar | Fsp | % | Diekmann, Bernhard | X-ray diffraction, bulk mineralogy | |
8 | Amphibole | Amp | % | Diekmann, Bernhard | X-ray diffraction, bulk mineralogy | |
9 | Pyroxene | Pyrox | % | Diekmann, Bernhard | X-ray diffraction, bulk mineralogy | |
10 | Illite 10Å | Ill10Å | % | Diekmann, Bernhard | X-ray diffraction, bulk mineralogy | |
11 | Kaolinite+Chlorite (7Å) | Kln+Chl 7Å | % | Diekmann, Bernhard | X-ray diffraction, bulk mineralogy | |
12 | Quartz/Feldspar ratio | Qz/Fsp | Diekmann, Bernhard | Calculated | ||
13 | Plagioclase/Kalifeldspar ratio | Pl/Kfs | Diekmann, Bernhard | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
660 data points
Data
1 Depth sed [m] | 2 Depth comp [mcd] | 3 Sample label | 4 Qz [#] | 5 Pl [%] | 6 Kfs [%] | 7 Fsp [%] | 8 Amp [%] | 9 Pyrox [%] | 10 Ill10Å [%] | 11 Kln+Chl 7Å [%] | 12 Qz/Fsp | 13 Pl/Kfs |
---|---|---|---|---|---|---|---|---|---|---|---|---|
0.01 | 0.01 | Lz1005-1 | 35 | 23 | 12 | 35 | 2 | 20 | 5 | 3 | 1.0 | 1.9 |
0.02 | 0.02 | Lz1005-1 | 44 | 18 | 11 | 29 | 2 | 18 | 5 | 2 | 1.5 | 1.6 |
0.03 | 0.03 | Lz1005-1 | 37 | 20 | 11 | 32 | 2 | 21 | 6 | 3 | 1.2 | 1.8 |
0.04 | 0.04 | Lz1005-1 | 38 | 21 | 13 | 34 | 1 | 19 | 5 | 3 | 1.1 | 1.6 |
0.07 | 0.07 | Lz1005-1 | 32 | 24 | 12 | 36 | 2 | 22 | 4 | 4 | 0.9 | 1.9 |
0.11 | 0.11 | Lz1005-1 | 48 | 21 | 11 | 32 | 1 | 14 | 4 | 2 | 1.5 | 2.0 |
0.17 | 0.17 | Lz1005-1 | 40 | 22 | 11 | 33 | 2 | 17 | 6 | 3 | 1.2 | 2.0 |
0.26 | 0.26 | Lz1005-1 | 32 | 23 | 13 | 35 | 7 | 17 | 5 | 4 | 0.9 | 1.8 |
0.29 | 0.29 | Lz1005-1 | 31 | 23 | 12 | 35 | 2 | 23 | 6 | 4 | 0.9 | 1.8 |
0.32 | 0.32 | Lz1005-1 | 34 | 22 | 12 | 33 | 2 | 22 | 5 | 4 | 1.0 | 1.9 |
0.53 | 0.36 | Lz1005-2 | 47 | 15 | 14 | 29 | 0 | 16 | 6 | 2 | 1.6 | 1.1 |
0.57 | 0.40 | Lz1005-2 | 32 | 21 | 12 | 33 | 2 | 22 | 6 | 4 | 1.0 | 1.8 |
0.62 | 0.45 | Lz1005-2 | 35 | 20 | 12 | 33 | 2 | 21 | 6 | 4 | 1.1 | 1.7 |
0.67 | 0.50 | Lz1005-2 | 30 | 24 | 11 | 35 | 2 | 23 | 7 | 3 | 0.9 | 2.1 |
0.75 | 0.58 | Lz1005-2 | 33 | 21 | 13 | 33 | 2 | 20 | 7 | 4 | 1.0 | 1.7 |
0.86 | 0.69 | Lz1005-2 | 35 | 19 | 14 | 33 | 2 | 21 | 6 | 4 | 1.1 | 1.4 |
1.04 | 0.87 | Lz1005-2 | 34 | 21 | 12 | 33 | 2 | 19 | 7 | 4 | 1.0 | 1.7 |
1.29 | 1.12 | Lz1005-2 | 37 | 19 | 11 | 30 | 2 | 21 | 6 | 4 | 1.2 | 1.7 |
2.24 | 2.07 | Lz1005-2 | 30 | 21 | 12 | 33 | 3 | 25 | 6 | 3 | 0.9 | 1.8 |
2.43 | 2.26 | Lz1005-2 | 32 | 19 | 12 | 31 | 7 | 20 | 6 | 3 | 1.0 | 1.6 |
2.51 | 2.49 | Lz1005-3 | 38 | 19 | 10 | 30 | 2 | 23 | 5 | 3 | 1.3 | 1.9 |
2.53 | 2.36 | Lz1005-2 | 39 | 20 | 11 | 31 | 2 | 19 | 6 | 3 | 1.3 | 1.9 |
2.56 | 2.54 | Lz1005-3 | 35 | 28 | 12 | 40 | 1 | 18 | 4 | 2 | 0.9 | 2.3 |
2.60 | 2.43 | Lz1005-2 | 38 | 21 | 12 | 33 | 2 | 18 | 5 | 3 | 1.2 | 1.7 |
2.62 | 2.60 | Lz1005-3 | 34 | 21 | 16 | 37 | 1 | 23 | 4 | 1 | 0.9 | 1.3 |
2.72 | 2.70 | Lz1005-3 | 41 | 26 | 8 | 35 | 1 | 19 | 3 | 1 | 1.2 | 3.1 |
2.74 | 2.72 | Lz1005-3 | 41 | 25 | 11 | 36 | 2 | 17 | 3 | 1 | 1.1 | 2.2 |
2.84 | 2.82 | Lz1005-3 | 45 | 22 | 17 | 39 | 1 | 14 | 1 | 0 | 1.2 | 1.3 |
2.94 | 2.92 | Lz1005-3 | 44 | 23 | 15 | 38 | 2 | 15 | 1 | 0 | 1.2 | 1.6 |
3.05 | 3.03 | Lz1005-3 | 46 | 23 | 15 | 38 | 1 | 15 | 1 | 0 | 1.2 | 1.6 |
3.12 | 3.10 | Lz1005-3 | 51 | 21 | 11 | 32 | 1 | 15 | 1 | 0 | 1.6 | 2.0 |
3.24 | 3.22 | Lz1005-3 | 44 | 26 | 15 | 41 | 2 | 13 | 1 | 0 | 1.1 | 1.8 |
3.34 | 3.32 | Lz1005-3 | 43 | 25 | 15 | 40 | 1 | 16 | 1 | 0 | 1.1 | 1.6 |
3.44 | 3.42 | Lz1005-3 | 45 | 25 | 14 | 40 | 1 | 14 | 0 | 0 | 1.1 | 1.8 |
3.54 | 3.52 | Lz1005-3 | 43 | 27 | 15 | 42 | 2 | 13 | 0 | 0 | 1.0 | 1.8 |
3.64 | 3.62 | Lz1005-3 | 45 | 27 | 15 | 42 | 1 | 12 | 1 | 0 | 1.1 | 1.7 |
3.74 | 3.72 | Lz1005-3 | 39 | 27 | 19 | 46 | 1 | 13 | 1 | 0 | 0.8 | 1.4 |
3.84 | 3.82 | Lz1005-3 | 47 | 23 | 15 | 39 | 1 | 13 | 0 | 0 | 1.2 | 1.5 |
3.94 | 3.92 | Lz1005-3 | 46 | 27 | 13 | 40 | 0 | 12 | 1 | 0 | 1.1 | 2.0 |
4.05 | 4.03 | Lz1005-3 | 43 | 27 | 17 | 44 | 1 | 11 | 1 | 0 | 1.0 | 1.6 |
4.15 | 4.13 | Lz1005-3 | 47 | 23 | 17 | 40 | 1 | 12 | 1 | 0 | 1.2 | 1.4 |
4.25 | 4.23 | Lz1005-3 | 34 | 30 | 24 | 54 | 1 | 9 | 1 | 0 | 0.6 | 1.3 |
4.35 | 4.33 | Lz1005-3 | 48 | 25 | 12 | 37 | 0 | 14 | 1 | 0 | 1.3 | 2.1 |
4.45 | 4.43 | Lz1005-3 | 42 | 28 | 15 | 43 | 1 | 12 | 1 | 0 | 1.0 | 1.9 |
4.55 | 4.53 | Lz1005-3 | 42 | 24 | 19 | 43 | 1 | 12 | 2 | 0 | 1.0 | 1.3 |
4.65 | 4.63 | Lz1005-3 | 45 | 25 | 16 | 41 | 1 | 12 | 1 | 0 | 1.1 | 1.6 |
4.75 | 4.73 | Lz1005-3 | 42 | 26 | 16 | 42 | 2 | 13 | 1 | 0 | 1.0 | 1.7 |
4.85 | 4.83 | Lz1005-3 | 39 | 29 | 17 | 46 | 1 | 12 | 2 | 0 | 0.9 | 1.7 |
4.95 | 4.93 | Lz1005-3 | 40 | 27 | 18 | 45 | 2 | 10 | 4 | 0 | 0.9 | 1.5 |
5.04 | 5.02 | Lz1005-4 | 33 | 31 | 24 | 55 | 2 | 8 | 2 | 0 | 0.6 | 1.3 |
5.14 | 5.12 | Lz1005-4 | 38 | 26 | 24 | 50 | 2 | 7 | 3 | 0 | 0.7 | 1.1 |
5.24 | 5.22 | Lz1005-4 | 39 | 26 | 19 | 45 | 1 | 11 | 3 | 0 | 0.9 | 1.4 |
5.34 | 5.32 | Lz1005-4 | 44 | 25 | 20 | 45 | 1 | 9 | 1 | 0 | 1.0 | 1.3 |
5.42 | 5.40 | Lz1005-4 | 46 | 24 | 15 | 38 | 2 | 12 | 1 | 0 | 1.2 | 1.6 |
5.54 | 5.52 | Lz1005-4 | 43 | 25 | 16 | 42 | 2 | 11 | 2 | 0 | 1.0 | 1.5 |