Citation:

PANGAEA.917734

Name: Fig. 8 RPI Süttö compared to Glopis and Piso data
Published: 2020-05-29
License: https://creativecommons.org/licenses/by/4.0/
Keywords: data correlation; Piso and Glopis data stack; RPI; Süttö

Always quote citation above when using data! You can download the citation in several formats below.

Published: 2020-05-29 • DOI registered: 2020-07-16

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Keyword(s):

data correlation; Piso and Glopis data stack; RPI; Süttö

Related to:

Rolf, Christian; Hambach, Ulrich; Novothny, Ágnes; Horváth, Erzsébet; Schnepp, Elisabeth (2014): Dating of a Last Glacial loess sequence by relative geomagnetic palaeointensity: A case study from the Middle Danube Basin (Süttő, Hungary). Quaternary International, 319, 99-108, https://doi.org/10.1016/j.quaint.2013.08.050

Coverage:

Latitude: 47.738000 * Longitude: 18.448000

Minimum DEPTH, sediment/rock: 3.095 m * Maximum DEPTH, sediment/rock: 9.240 m

Event(s):

Suettoe * Latitude: 47.738000 * Longitude: 18.448000 * Location: Hungary * Comment: LPSS-profile outcropping at Hegyhati quarry (Süttö)

Comment:

Comparison between the RPI record obtained at Sütto and the GLOPIS (Laj et al., 2004) and the PISO stack (cut-out PISO 1.5 Ma; Channell et al., 2009). Correlation intervals for indirect dating. Above depths of 6 m, the RPI signal at Sütto is ambiguous. Nevertheless, based on the reasonable assumption of strongly increased accumulation rates, a possible correlation of the upper part of the section near 4 m to the time span between 22 and 24 ka is proposed.

Parameter(s):

#	Name	Short Name	Unit	Principal Investigator	Comment
1	DEPTH, sediment/rock	Depth sed	m	Rolf, Christian	Geocode
2	Relative paleointensity proxy	RPI		Rolf, Christian	RPI trend corrected 0-1
3	Year of observation	Year obs	a AD	Rolf, Christian
4	Profile ID	Profile ID		Rolf, Christian

License:

Creative Commons Attribution 4.0 International (CC-BY-4.0)

Size:

825 data points

Data

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

1 Depth sed [m]	2 RPI	3 Year obs [a AD]	4 Profile ID
3.120	0.42	2008	CY_A
3.200	0.53	2008	CY_A
3.300	0.47	2008	CY_A
3.400	0.44	2008	CY_A
3.500	0.59	2008	CY_A
3.600	0.37	2008	CY_A
3.700	0.49	2008	CY_A
3.850	0.67	2008	CY_A
3.900	0.52	2008	CY_A
4.000	0.60	2008	CY_A
4.100	0.50	2008	CY_A
4.200	0.39	2008	CY_A
4.300	0.42	2008	CY_A
4.400	0.31	2008	CY_A
4.500	0.35	2008	CY_A
4.600	0.31	2008	CY_A
4.700	0.25	2008	CY_A
4.800	0.20	2008	CY_A
4.900	0.27	2008	CY_A
5.000	0.24	2008	CY_A
5.100	0.25	2008	CY_A
5.200	0.28	2008	CY_A
5.300	0.32	2008	CY_A
5.400	0.25	2008	CY_A
5.600	0.29	2008	CY_A
5.560	0.20	2008	CY_B
5.660	0.21	2008	CY_B
5.760	0.22	2008	CY_B
6.060	0.32	2008	CY_B
6.160	0.47	2008	CY_B
6.260	0.23	2008	CY_B
6.420	0.30	2008	CY_C
6.460	0.21	2008	CY_C
6.560	0.18	2008	CY_C
6.660	0.17	2008	CY_C
6.760	0.04	2008	CY_C
6.860	0.06	2008	CY_C
6.960	0.08	2008	CY_C
7.060	0.14	2008	CY_C
7.160	0.28	2008	CY_C
7.260	0.65	2008	CY_C
7.360	0.48	2008	CY_C
7.460	0.53	2008	CY_C
8.460	0.41	2008	CYE
8.540	0.18	2008	CYE
8.640	0.19	2008	CYE
8.740	0.06	2008	CYE
8.840	0.02	2008	CYE
9.040	0.12	2008	CYE
9.240	0.06	2008	CYE
7.540	0.56	2008	Cu D
7.540	0.54	2008	Cu D
7.540	0.50	2008	Cu D
7.540	0.47	2008	Cu D
7.560	0.62	2008	Cu D
7.560	0.61	2008	Cu D
7.580	0.60	2008	Cu D
7.600	0.74	2008	Cu D
7.620	0.82	2008	Cu D
7.640	0.86	2008	Cu D
7.640	0.65	2008	Cu D
7.640	0.63	2008	Cu D
7.640	0.75	2008	Cu D
7.660	0.70	2008	Cu D
7.680	0.60	2008	Cu D
7.700	0.66	2008	Cu D
7.720	0.50	2008	Cu D
7.740	0.51	2008	Cu D
7.740	0.69	2008	Cu D
7.740	0.69	2008	Cu D
7.740	0.60	2008	Cu D
7.760	0.77	2008	Cu D
7.780	0.59	2008	Cu D
7.800	0.59	2008	Cu D
7.840	0.72	2008	Cu D
7.840	0.15	2008	Cu D
7.840	0.10	2008	Cu D
7.840	0.07	2008	Cu D
7.860	0.09	2008	Cu D
7.880	0.36	2008	Cu D
7.900	0.21	2008	Cu D
7.920	0.34	2008	Cu D
7.940	0.41	2008	Cu D
3.325	0.82	2009	CY_A
3.345	0.40	2009	CY_A
3.365	0.41	2009	CY_A
3.385	0.33	2009	CY_A
3.405	0.86	2009	CY_A
3.425	0.50	2009	CY_A
3.445	0.67	2009	CY_A
3.465	0.50	2009	CY_A
3.485	0.44	2009	CY_A
3.505	0.59	2009	CY_A
3.525	0.65	2009	CY_A
3.545	0.51	2009	CY_A
3.565	0.68	2009	CY_A
3.585	0.44	2009	CY_A
3.605	0.66	2009	CY_A
3.625	0.47	2009	CY_A
3.645	0.65	2009	CY_A
3.665	0.58	2009	CY_A
3.685	0.59	2009	CY_A
3.690	0.73	2009	CY_A
3.730	0.65	2009	CY_A
3.750	0.60	2009	CY_A
3.770	0.92	2009	CY_A
3.790	0.69	2009	CY_A
3.810	0.70	2009	CY_A
3.830	0.72	2009	CY_A
3.850	0.79	2009	CY_A
3.870	0.65	2009	CY_A
3.890	0.79	2009	CY_A
3.910	0.73	2009	CY_A
3.930	0.85	2009	CY_A
3.950	0.86	2009	CY_A
3.970	0.74	2009	CY_A
3.990	0.36	2009	CY_A
4.010	0.51	2009	CY_A
4.030	0.49	2009	CY_A
4.050	0.54	2009	CY_A
4.070	0.49	2009	CY_A
4.090	0.41	2009	CY_A
4.110	0.33	2009	CY_A
4.130	0.49	2009	CY_A
4.150	0.49	2009	CY_A
4.170	0.51	2009	CY_A
4.190	0.43	2009	CY_A
4.210	0.37	2009	CY_A
4.230	0.36	2009	CY_A
4.250	0.52	2009	CY_A
4.270	0.36	2009	CY_A
4.290	0.38	2009	CY_A
4.310	0.35	2009	CY_A
4.330	0.52	2009	CY_A
4.350	0.57	2009	CY_A
4.370	0.81	2009	CY_A
4.390	0.35	2009	CY_A
4.410	0.34	2009	CY_A
4.430	0.36	2009	CY_A
4.450	0.29	2009	CY_A
4.470	0.47	2009	CY_A
4.490	0.46	2009	CY_A
4.510	0.47	2009	CY_A
4.530	0.37	2009	CY_A
4.550	0.43	2009	CY_A
4.570	0.33	2009	CY_A
4.590	0.37	2009	CY_A
4.600	0.31	2009	CY_A
4.620	0.30	2009	CY_A
4.640	0.35	2009	CY_A
4.660	0.43	2009	CY_A
4.680	0.51	2009	CY_A
4.700	0.40	2009	CY_A
4.720	0.44	2009	CY_A
4.740	0.29	2009	CY_A
4.760	0.40	2009	CY_A
4.780	0.42	2009	CY_A
4.800	0.45	2009	CY_A
4.820	0.38	2009	CY_A
4.840	0.33	2009	CY_A
4.860	0.38	2009	CY_A
4.880	0.24	2009	CY_A
4.900	0.25	2009	CY_A
4.920	0.34	2009	CY_A
4.940	0.33	2009	CY_A
4.960	0.23	2009	CY_A
4.980	0.30	2009	CY_A
5.000	0.30	2009	CY_A
5.020	0.27	2009	CY_A
5.040	0.31	2009	CY_A
5.060	0.28	2009	CY_A
5.080	0.31	2009	CY_A
5.100	0.25	2009	CY_A
5.120	0.32	2009	CY_A
5.140	0.38	2009	CY_A
5.160	0.26	2009	CY_A
5.180	0.39	2009	CY_A
5.200	0.42	2009	CY_A
5.220	0.46	2009	CY_A
5.240	0.44	2009	CY_A
5.260	0.35	2009	CY_A
5.280	0.31	2009	CY_A
5.300	0.45	2009	CY_A
5.320	0.52	2009	CY_A
5.340	0.29	2009	CY_A
5.360	0.30	2009	CY_A
5.380	0.25	2009	CY_A
5.400	0.37	2009	CY_A
5.420	0.44	2009	CY_A
5.440	0.33	2009	CY_A
5.460	0.36	2009	CY_A
5.480	0.34	2009	CY_A
5.500	0.27	2009	CY_A
5.520	0.30	2009	CY_A
5.540	0.26	2009	CY_A
5.560	0.28	2009	CY_A
5.580	0.34	2009	CY_A
5.600	0.27	2009	CY_A
5.450	0.29	2009	CY_B
5.460	0.20	2009	CY_B
5.470	0.25	2009	CY_B
5.480	0.33	2009	CY_B
5.498	0.30	2009	CY_B
5.520	0.31	2009	CY_B
5.537	0.32	2009	CY_B
5.545	0.33	2009	CY_B
5.560	0.35	2009	CY_B
5.575	0.40	2009	CY_B
5.590	0.28	2009	CY_B
5.602	0.39	2009	CY_B
5.618	0.35	2009	CY_B
5.630	0.33	2009	CY_B
5.645	0.29	2009	CY_B
5.655	0.21	2009	CY_B
5.672	0.25	2009	CY_B
5.700	0.22	2009	CY_B
5.716	0.28	2009	CY_B
5.725	0.22	2009	CY_B
5.740	0.14	2009	CY_B
5.755	0.22	2009	CY_B
5.765	0.25	2009	CY_B
5.780	0.26	2009	CY_B
5.805	0.23	2009	CY_B
5.820	0.26	2009	CY_B
5.830	0.25	2009	CY_B
5.845	0.20	2009	CY_B
5.855	0.22	2009	CY_B
5.870	0.31	2009	CY_B
5.885	0.29	2009	CY_B
5.895	0.20	2009	CY_B
5.910	0.15	2009	CY_B
5.925	0.12	2009	CY_B
5.940	0.19	2009	CY_B
5.955	0.20	2009	CY_B
5.960	0.19	2009	CY_B
5.982	0.19	2009	CY_B
6.000	0.24	2009	CY_B
6.010	0.18	2009	CY_B
6.040	0.18	2009	CY_B
6.055	0.29	2009	CY_B
6.070	0.24	2009	CY_B
6.085	0.27	2009	CY_B
6.100	0.31	2009	CY_B
6.130	0.44	2009	CY_B
6.150	0.56	2009	CY_B
6.170	0.21	2009	CY_B
6.185	0.49	2009	CY_B
6.200	0.47	2009	CY_B
6.215	0.50	2009	CY_B
6.230	0.42	2009	CY_B
6.245	0.41	2009	CY_B
6.270	0.39	2009	CY_B
6.295	0.36	2009	CY_B
6.310	0.33	2009	CY_B
6.325	0.36	2009	CY_B
6.340	0.31	2009	CY_B
6.355	0.28	2009	CY_B
6.370	0.25	2009	CY_B
6.390	0.29	2009	CY_B
6.420	0.28	2009	CY_B
3.095	0.25	2009	Cu_A
3.115	0.45	2009	Cu_A
3.135	0.34	2009	Cu_A
3.155	0.32	2009	Cu_A
3.175	0.38	2009	Cu_A
3.180	0.38	2009	Cu_A
3.195	0.38	2009	Cu_A
3.200	0.28	2009	Cu_A
3.240	0.63	2009	Cu_A
3.260	0.43	2009	Cu_A
3.275	0.58	2009	Cu_A
3.295	0.56	2009	Cu_A
3.315	0.54	2009	Cu_A
3.335	0.39	2009	Cu_A
3.355	0.45	2009	Cu_A