Berg, Sonja (2018): Elemental analysis of the total carbon, total nitrogen and total sulphur on mumiyo deposit PRM8 from Petermann Range [dataset]. Institute of Geology and Mineralogy, University of Cologne, PANGAEA, https://doi.org/10.1594/PANGAEA.896498, In supplement to: Berg, Sonja; Melles, Martin; Hermichen, Wolf-Dieter; McClymont, Erin L; Bentley, Michael J; Hodgson, Dominic A; Kuhn, Gerhard (2019): Evaluation of mumiyo deposits from East Antarctica as archives for the late quaternary environmental and climatic history. Geochemistry, Geophysics, Geosystems, 19, https://doi.org/10.1029/2018GC008054
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Project(s):
Funding:
German Research Foundation (DFG), grant/award no. 5472008: Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas
Coverage:
Latitude: -71.366700 * Longitude: 12.583300
Date/Time Start: 1996-01-22T00:00:00 * Date/Time End: 1996-01-22T00:00:00
Minimum DEPTH, sediment/rock: 0.0018 m * Maximum DEPTH, sediment/rock: 0.1410 m
Event(s):
PRM-8 * Latitude: -71.366700 * Longitude: 12.583300 * Date/Time: 1996-01-22T00:00:00 * Elevation: 1420.0 m * Location: Petermann Range * Campaign: GeoMaud95/96 * Basis: Sampling on land * Method/Device: Multiple investigations (MULT)
Comment:
Elemental analysis of the total carbon (C), total nitrogen (N) and total sulphur (S) content was measured with a vario microcube (Elementar, Germany) on 2 mm thick sub-samples of the profile PRM8-A. Due to the sticky consistence of the material the samples could not be homogenized prior to analysis and each sample was measured in four replicates of c. 2.5 mg (± standard deviation of the mean).
Contents of total carbon, total nitrogen and total sulphur %, reported values are mean values of 4 replicates and standard deviation of the mean.
Parameter(s):
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
242 data points
Data
1 Profile ID | 2 Depth sed [m] | 3 Depth top [m] | 4 Depth bot [m] | 5 TC [%] | 6 TC std dev [±] | 7 TN [%] | 8 TN std dev [±] | 9 C/N | 10 C/N std dev [±] | 11 TS [%] | 12 S std dev [±] |
---|---|---|---|---|---|---|---|---|---|---|---|
PRM-8_A | 0.0018 | 0.0008 | 0.0028 | 40.6 | 2.7 | 2.25 | 0.10 | 18.0 | 0.5 | 0.16 | 0.02 |
PRM-8_A | 0.0110 | 0.0100 | 0.0120 | 49.8 | 2.1 | 3.72 | 0.35 | 13.4 | 0.9 | 0.18 | 0.02 |
PRM-8_A | 0.0190 | 0.0180 | 0.0200 | 43.6 | 11.4 | 2.64 | 0.67 | 16.5 | 3.1 | 0.18 | 0.03 |
PRM-8_A | 0.0210 | 0.0200 | 0.0220 | 45.0 | 7.9 | 3.25 | 0.61 | 13.9 | 2.2 | 0.19 | 0.02 |
PRM-8_A | 0.0310 | 0.0300 | 0.0320 | 55.3 | 2.2 | 4.05 | 0.33 | 13.7 | 1.3 | 0.18 | 0.02 |
PRM-8_A | 0.0390 | 0.0380 | 0.0400 | 39.3 | 0.9 | 3.89 | 0.64 | 10.1 | 1.4 | 0.19 | 0.02 |
PRM-8_A | 0.0410 | 0.0400 | 0.0420 | 46.3 | 3.4 | 4.21 | 0.17 | 11.0 | 0.6 | 0.22 | 0.02 |
PRM-8_A | 0.0510 | 0.0500 | 0.0520 | 47.2 | 4.9 | 5.06 | 0.57 | 9.3 | 1.4 | 0.22 | 0.02 |
PRM-8_A | 0.0610 | 0.0600 | 0.0620 | 43.9 | 5.5 | 11.97 | 2.86 | 3.7 | 0.6 | 0.18 | 0.02 |
PRM-8_A | 0.0610 | 0.0600 | 0.0620 | 47.3 | 2.6 | 10.33 | 1.55 | 4.6 | 0.7 | 0.19 | 0.03 |
PRM-8_A | 0.0710 | 0.0700 | 0.0720 | 49.6 | 4.5 | 5.19 | 0.64 | 9.5 | 1.7 | 0.20 | 0.02 |
PRM-8_A | 0.0790 | 0.0780 | 0.0800 | 46.6 | 1.4 | 4.67 | 0.29 | 10.0 | 0.4 | 0.22 | 0.04 |
PRM-8_A | 0.0810 | 0.0800 | 0.0820 | 46.7 | 4.4 | 4.89 | 1.10 | 9.5 | 1.8 | 0.23 | 0.03 |
PRM-8_A | 0.0910 | 0.0900 | 0.0920 | 46.6 | 3.7 | 6.26 | 0.63 | 7.4 | 0.3 | 0.26 | 0.01 |
PRM-8_A | 0.0990 | 0.0980 | 0.1000 | 48.5 | 2.8 | 3.65 | 0.63 | 13.3 | 3.3 | 0.18 | 0.01 |
PRM-8_A | 0.1010 | 0.1000 | 0.1020 | 44.5 | 9.8 | 3.62 | 1.17 | 12.3 | 1.5 | 0.29 | 0.14 |
PRM-8_A | 0.1110 | 0.1100 | 0.1120 | 49.1 | 2.7 | 4.77 | 1.49 | 10.3 | 3.6 | 0.15 | 0.02 |
PRM-8_A | 0.1190 | 0.1180 | 0.1200 | 54.9 | 3.4 | 3.53 | 0.48 | 15.6 | 2.8 | 0.12 | 0.01 |
PRM-8_A | 0.1210 | 0.1200 | 0.1220 | 33.9 | 3.4 | 4.40 | 1.03 | 7.7 | 1.4 | 0.14 | 0.02 |
PRM-8_A | 0.1310 | 0.1300 | 0.1320 | 50.5 | 3.4 | 5.47 | 0.54 | 9.2 | 0.5 | 0.15 | 0.02 |
PRM-8_A | 0.1390 | 0.1380 | 0.1400 | 41.1 | 6.2 | 5.58 | 1.15 | 7.4 | 0.5 | 0.16 | 0.03 |
PRM-8_A | 0.1410 | 0.1400 | 0.1420 | 49.2 | 2.4 | 4.11 | 1.57 | 12.0 | 7.9 | 0.15 | 0.03 |