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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):
Schwalbenberg_II * Latitude: 50.557000 * Longitude: 7.236000 * Method/Device: Outcrop sample (OUTCROP) * Comment: loess-paleosol sequence
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample IDSample IDSchirmer, Wolfgang
2SECTION, heightSectionmSchirmer, WolfgangGeocode – Composite Depth, the middle depth of each sample from base (0 m) to top (13.2 m)
3Lithology/composition/faciesLithologyProfe, JörnAccording to color coding in Fig. 2 and description in Tab. 1 in Schirmer (2012)
4Susceptibility, specific, low-field mass-normalizedchi_lf10-9 m3/kgProfe, JörnBartington MS2B bulk 465 Hz, Brementriple measurement
5Susceptibility, specific, low-field mass-normalized, standard deviationchi_lf std dev±Profe, JörnBartington MS2B bulk 465 Hz, Brementriple measurement
6Susceptibility, specific, high-field mass-normalizedchi_hf10-9 m3/kgProfe, JörnBartington MS2B bulk 4650 Hz, Brementriple measurement
7Susceptibility, specific, high-field mass-normalized, standard deviationchi_hf std dev±Profe, JörnBartington MS2B bulk 4650 Hz, Brementriple measurement
8Magnetic susceptibility, frequency dependencechi_fd%Profe, Jörnafter Dearing et al. (1996)triple measurement
9Magnetic susceptibility, frequency dependence, standard deviationchi_fd std dev±Profe, Jörnafter Dearing et al. (1996)triple measurement
10Carbon, organic, totalTOC%Profe, JörnCombustion at 480°C in a Dimatec laboratory furnace (Schirmer, 2012)
11U-ratioU-ratioProfe, JörnGrain Size, gravityGrainsize 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).
Size:
2160 data points

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