Citation:

PANGAEA.81229

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

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Related to:

Frank, Martin; Gersonde, Rainer; Mangini, Augusto (1999): Sediment redistribution, 230Thex - nomalization and implications for the reconstruction of particle flux and export productivity. In: Fischer, G & Wefer, G (eds.), Use of Proxies in Paleoceanography - Examples from the South Atlantic, Springer, Berlin, Heidelberg, 409-426

Project(s):

Paleoenvironmental Reconstructions from Marine Sediments @ AWI (AWI_Paleo)

South Atlantic in Late Quaternary: Reconstruction of Budget and Currents (SFB261)

Coverage:

Latitude: -48.900000 * Longitude: 6.714660

Date/Time Start: 1989-11-08T06:24:00 * Date/Time End: 1989-11-08T06:24:00

Minimum DEPTH, sediment/rock: 0.07 m * Maximum DEPTH, sediment/rock: 8.57 m

Event(s):

PS1756-5 (PS16/284) * Latitude: -48.900000 * Longitude: 6.714660 * Date/Time: 1989-11-08T06:24:00 * Elevation: -3828.0 m * Recovery: 8.62 m * Location: Meteor Rise * Campaign: (PS16) * Basis: * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 9 core sections: 0.04-0.77, 0.77-1.77, 1.77-2.77, 2.77-3.77, 3.77-4.62, 4.62-5.62, 5.62-6.62, 6.62-7.62, 7.62-8.62 m; 0-4 fehlt

Parameter(s):

#	Name	Short Name	Unit	Principal Investigator	Method/Device	Comment
1	DEPTH, sediment/rock	Depth sed	m			Geocode
2	Accumulation rate, mass	MAR	g/cm²/ka	Frank, Martin	Calculated
3	Accumulation rate, sediment, standard deviation	MAR std dev	±	Frank, Martin	Calculated
4	Vertical rain rate	Rain rate	g/cm²/ka	Frank, Martin
5	Vertical rain rate, standard deviation	Rain rate std dev	±	Frank, Martin

License:

Creative Commons Attribution 3.0 Unported (CC-BY-3.0)

Size:

348 data points

Data

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

1 Depth sed [m]	2 MAR [g/cm²/ka]	3 MAR std dev [±]	4 Rain rate [g/cm²/ka]	5 Rain rate std dev [±]
0.07	0.31	0.01	1.83	0.08
0.15	3.46	0.24	2.40	0.16
0.25	4.29	0.35	2.99	0.24
0.35	4.31	0.35	3.00	0.24
0.45	5.37	0.56	3.74	0.39
0.55	4.61	0.42	3.21	0.29
0.65	4.70	0.38	3.27	0.26
0.75	4.70	0.44	3.27	0.30
0.85	4.82	0.38	3.36	0.27
0.95	4.39	0.27	3.05	0.19
1.05	4.73	0.38	3.29	0.26
1.15	4.74	0.36	3.30	0.25
1.25	4.58	0.39	3.19	0.27
1.35	5.25	0.52	3.65	0.36
1.45	4.61	0.34	3.21	0.24
1.55	4.54	0.36	3.16	0.25
1.65	4.12	0.29	2.87	0.20
1.75	4.86	0.40	3.38	0.28
1.85	4.82	0.42	3.35	0.29
1.95	4.47	0.38	3.11	0.26
2.05	4.28	0.35	2.98	0.24
2.15	4.43	0.37	3.08	0.25
2.25	4.52	0.36	3.14	0.25
2.35	4.98	0.41	3.47	0.28
2.45	1.89	0.20	4.30	0.45
2.55	1.88	0.20	4.29	0.46
2.65	1.80	0.19	4.11	0.42
2.75	1.62	0.15	3.70	0.34
2.85	1.91	0.21	4.35	0.48
2.95	1.73	0.15	3.95	0.34
3.03	1.91	0.19	4.36	0.43
3.09	1.82	0.21	4.16	0.47
3.16	1.96	0.22	4.46	0.49
3.26	1.69	0.17	3.84	0.39
3.36	1.64	0.17	3.73	0.39
3.46	1.65	0.19	3.75	0.43
3.56	1.21	0.10	2.74	0.22
3.66	1.20	0.09	2.73	0.21
3.76	1.00	0.07	2.28	0.17
3.86	1.07	0.09	2.42	0.20
3.96	0.99	0.06	2.25	0.14
4.06	1.08	0.09	2.45	0.21
4.16	1.33	0.12	3.02	0.27
4.26	0.83	0.06	1.88	0.12
4.36	0.91	0.05	2.06	0.12
4.47	1.77	0.12	2.32	0.16
4.57	1.90	0.18	2.50	0.24
4.67	1.59	0.12	2.09	0.16
4.77	1.55	0.10	2.03	0.13
4.87	1.58	0.12	2.07	0.16
4.97	1.63	0.11	2.14	0.15
5.07	1.51	0.09	1.99	0.11
5.17	1.43	0.08	1.87	0.10
5.27	1.20	0.06	1.57	0.08
5.37	1.15	0.09	1.34	0.11
5.47	1.03	0.08	1.21	0.09
5.57	1.53	0.15	1.80	0.18
5.67	1.25	0.09	1.46	0.11
5.77	1.40	0.09	1.64	0.10
5.87	1.39	0.09	1.62	0.11
5.97	1.54	0.13	1.81	0.15
6.07	1.36	0.12	1.59	0.14
6.17	1.64	0.14	1.92	0.16
6.29	1.47	0.13	1.72	0.15
6.39	1.71	0.14	2.01	0.17
6.47	1.33	0.10	1.55	0.11
6.57	1.66	0.13	1.94	0.15
6.67	1.27	0.13	1.49	0.15
6.77	1.60	0.14	1.88	0.16
6.87	1.42	0.11	1.66	0.12
6.97	1.86	0.20	2.19	0.24
7.07	2.36	0.31	2.78	0.36
7.17	1.44	0.13	1.69	0.15
7.27	0.67	0.09	1.96	0.25
7.37	1.09	0.31	3.21	0.90
7.47	1.21	0.27	3.56	0.78
7.57	0.86	0.19	2.52	0.55
7.67	0.38	0.03	1.10	0.09
7.77	1.89	0.18	1.34	0.13
7.87	2.52	0.30	1.79	0.21
7.97	2.07	0.12	1.47	0.09
8.07	1.82	0.13	1.29	0.09
8.17	1.84	0.10	1.31	0.07
8.27	1.37	0.06	0.97	0.04
8.37	1.57	0.10	1.11	0.07
8.47	1.51	0.13	1.06	0.09
8.57	1.51	0.13	1.07	0.09