Profe, Jörn; Zolitschka, Bernd; Schirmer, Wolfgang; Frechen, Manfred; Ohlendorf, Christian (2015): Magnetic susceptibility, organic carbon, total sulphur and U-ratio as grainsize index on the Schwalbenberg II loess-paleosol sequence [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.855567, In supplement to: Profe, J et al. (2016): Geochemistry unravels MIS 3/2 paleoenvironmental dynamics at the loess–paleosol sequence Schwalbenberg II, Germany. Palaeogeography, Palaeoclimatology, Palaeoecology, 459, 537-551, https://doi.org/10.1016/j.palaeo.2016.07.022
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Related to:
Schirmer, Wolfgang (2012): Rhine loess at Schwalbenberg II - MIS 4 and 3. E&G - Eiszeitalter und Gegenwart - Quaternary Science Journal, 61(1)32-47, https://doi.org/10.3285/eg.61.1.03
Coverage:
Latitude: 50.557000 * Longitude: 7.236000
Minimum SECTION, height: 0.038 m * Maximum SECTION, height: 12.940 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample ID | Sample ID | Schirmer, Wolfgang | |||
2 | SECTION, height | Section | m | Schirmer, Wolfgang | Geocode – Composite Depth, the middle depth of each sample from base (0 m) to top (13.2 m) | |
3 | Lithology/composition/facies | Lithology | Profe, Jörn | According to color coding in Fig. 2 and description in Tab. 1 in Schirmer (2012) | ||
4 | Susceptibility, specific, low-field mass-normalized | chi_lf | 10-9 m3/kg | Profe, Jörn | Bartington MS2B bulk 465 Hz, Bremen | triple measurement |
5 | Susceptibility, specific, low-field mass-normalized, standard deviation | chi_lf std dev | ± | Profe, Jörn | Bartington MS2B bulk 465 Hz, Bremen | triple measurement |
6 | Susceptibility, specific, high-field mass-normalized | chi_hf | 10-9 m3/kg | Profe, Jörn | Bartington MS2B bulk 4650 Hz, Bremen | triple measurement |
7 | Susceptibility, specific, high-field mass-normalized, standard deviation | chi_hf std dev | ± | Profe, Jörn | Bartington MS2B bulk 4650 Hz, Bremen | triple measurement |
8 | Magnetic susceptibility, frequency dependence | chi_fd | % | Profe, Jörn | after Dearing et al. (1996) | triple measurement |
9 | Magnetic susceptibility, frequency dependence, standard deviation | chi_fd std dev | ± | Profe, Jörn | after Dearing et al. (1996) | triple measurement |
10 | Carbon, organic, total | TOC | % | Profe, Jörn | Combustion at 480°C in a Dimatec laboratory furnace (Schirmer, 2012) | |
11 | U-ratio | U-ratio | Profe, Jörn | Grain Size, gravity | Grainsize analysis was carried out by Wolfgang Schirmer (Schirmer, 2012). The U-ratio is calculated as coarse silt (63-20µm) divided by fine silt (6.3-2µm) plus clay (<2µm). |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2160 data points
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