Citation:

PANGAEA.611254

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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: * 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

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

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