Hultzsch, Nadja (2007): Bulk mineral composition of sediment core Lz1010 (Table A12) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.611254
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: -70.815380 * Longitude: 68.017360
Date/Time Start: 2002-01-21T00:00:00 * Date/Time End: 2002-01-21T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 5.93 m
Event(s):
Lz1010 * Latitude: -70.815380 * Longitude: 68.017360 * Date/Time: 2002-01-21T00:00:00 * Lake water depth: 79 m * Location: Lake Radok, 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:
336 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 | Lz1010-1 | 66 | 11 | 10 | 21 | 1 | 10 | 1 | 1 | 3.2 | 1.1 |
0.06 | 0.06 | Lz1010-1 | 71 | 9 | 9 | 18 | 1 | 8 | 1 | 1 | 3.9 | 1.1 |
0.11 | 0.11 | Lz1010-1 | 57 | 13 | 9 | 22 | 2 | 11 | 3 | 5 | 2.6 | 1.4 |
0.17 | 0.17 | Lz1010-1 | 59 | 13 | 14 | 27 | 2 | 8 | 2 | 3 | 2.2 | 0.9 |
0.18 | 0.18 | Lz1010-1 | 61 | 13 | 12 | 24 | 2 | 10 | 1 | 2 | 2.5 | 1.1 |
0.32 | 0.26 | Lz1010-2 | 53 | 13 | 13 | 26 | 2 | 11 | 3 | 4 | 2.0 | 1.0 |
0.40 | 0.34 | Lz1010-2 | 57 | 13 | 9 | 21 | 2 | 10 | 3 | 6 | 2.7 | 1.5 |
0.52 | 0.46 | Lz1010-2 | 54 | 12 | 11 | 23 | 2 | 8 | 4 | 8 | 2.4 | 1.0 |
0.68 | 0.62 | Lz1010-2 | 60 | 15 | 11 | 26 | 1 | 10 | 1 | 2 | 2.3 | 1.4 |
0.76 | 0.70 | Lz1010-2 | 62 | 14 | 11 | 24 | 3 | 9 | 1 | 1 | 2.6 | 1.3 |
0.88 | 0.82 | Lz1010-2 | 52 | 19 | 15 | 34 | 3 | 7 | 2 | 2 | 1.5 | 1.3 |
1.26 | 1.20 | Lz1010-2 | 48 | 21 | 17 | 38 | 2 | 7 | 2 | 2 | 1.3 | 1.3 |
1.54 | 1.48 | Lz1010-2 | 55 | 17 | 14 | 30 | 2 | 11 | 1 | 1 | 1.8 | 1.2 |
1.68 | 1.62 | Lz1010-2 | 54 | 20 | 14 | 34 | 2 | 9 | 1 | 1 | 1.6 | 1.4 |
1.74 | 1.68 | Lz1010-2 | 47 | 26 | 16 | 42 | 1 | 7 | 1 | 2 | 1.1 | 1.7 |
1.78 | 1.72 | Lz1010-2 | 64 | 12 | 14 | 26 | 2 | 6 | 1 | 2 | 2.5 | 0.8 |
1.86 | 1.80 | Lz1010-2 | 67 | 10 | 14 | 24 | 1 | 5 | 1 | 2 | 2.8 | 0.7 |
1.88 | 1.82 | Lz1010-2 | 56 | 16 | 13 | 29 | 6 | 6 | 1 | 2 | 2.0 | 1.2 |
1.98 | 1.92 | Lz1010-2 | 70 | 9 | 14 | 22 | 0 | 4 | 1 | 2 | 3.1 | 0.6 |
2.73 | 2.68 | Lz1010-3 | 65 | 8 | 20 | 27 | 1 | 4 | 1 | 2 | 2.4 | 0.4 |
3.19 | 3.14 | Lz1010-3 | 66 | 6 | 18 | 25 | 1 | 4 | 1 | 3 | 2.7 | 0.3 |
3.57 | 3.52 | Lz1010-3 | 58 | 10 | 21 | 31 | 1 | 4 | 2 | 4 | 1.8 | 0.5 |
3.97 | 3.92 | Lz1010-3 | 64 | 7 | 18 | 25 | 1 | 3 | 2 | 4 | 2.5 | 0.4 |
4.57 | 4.52 | Lz1010-3 | 64 | 6 | 18 | 24 | 1 | 4 | 2 | 4 | 2.7 | 0.3 |
4.71 | 4.66 | Lz1010-3 | 61 | 9 | 20 | 29 | 1 | 4 | 2 | 4 | 2.1 | 0.5 |
5.29 | 5.24 | Lz1010-4 | 69 | 8 | 13 | 21 | 0 | 4 | 2 | 3 | 3.2 | 0.6 |
5.53 | 5.48 | Lz1010-4 | 60 | 8 | 18 | 26 | 1 | 6 | 2 | 4 | 2.3 | 0.5 |
5.93 | 5.88 | Lz1010-4 | 57 | 7 | 23 | 30 | 3 | 5 | 2 | 4 | 1.9 | 0.3 |