Citation:

PANGAEA.676730

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

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Related to:

Brückner, Sylvia (2008): Climatic and hydrographic variability in the late Holocene Skagerrak as deduced from benthic foraminiferal proxies (Klimatische und hydrographische Variabilität im holozänen Sagerrak, abgeleitet aus benthischen Foraminiferen). Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 572, 139 pp, hdl:10013/epic.28879

Brückner, Sylvia; Mackensen, Andreas; Blanz, Thomas; Emeis, Kay-Christian (submitted): Benthic foraminifera and relative organic matter contents in Holocene Skagerrak sediments, NE North Sea. Journal of Foraminiferal Research

Project(s):

Paleoenvironmental Reconstructions from Marine Sediments @ AWI (AWI_Paleo)

Coverage:

Latitude: 58.042220 * Longitude: 9.621440

Date/Time Start: 2000-05-10T00:00:00 * Date/Time End: 2000-05-10T00:00:00

Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 5.44 m

Event(s):

AL159_225510 * Latitude: 58.042220 * Longitude: 9.621440 * Date/Time: 2000-05-10T00:00:00 * Elevation: -285.0 m * Recovery: 5.44 m * Location: Skagerrak * Campaign: * Basis: * Method/Device: Gravity corer (GC)

Comment:

Project: Integrated Baltic Sea Environmental Study (IBSEN); funded by German Ministry of Education and Research (BMBF)

Parameter(s):

#	Name	Short Name	Unit	Principal Investigator	Method/Device	Comment
1	DEPTH, sediment/rock	Depth sed	m			Geocode
2	Age	Age	a AD/CE	Mackensen, Andreas	Age model in radiocarbon 14C ages
3	Carbon/Nitrogen ratio	C/N		Mackensen, Andreas
4	Carbon, organic, total	TOC	%	Mackensen, Andreas
5	Accumulation rate, total organic carbon	Acc rate TOC	g/cm²/ka	Mackensen, Andreas

License:

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

Size:

221 data points

Data

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

1 Depth sed [m]	2 Age [a AD/CE]	3 C/N	4 TOC [%]	5 Acc rate TOC [g/cm²/ka]
0.00	2000	11.3	2.19	788.5
0.04	1999	11.2
0.10	1998	10.0	2.35	906.1
0.20	1996	11.4	2.59	982.8
0.28	1994	10.3
0.30	1994		2.19	856.8
0.34	1993	11.0
0.40	1992	12.3	2.23	989.7
0.48	1990	10.6
0.50	1990		2.21	983.2
0.54	1989	10.7
0.60	1988	11.2	2.56	1103.6
0.70	1986	12.2	2.70	1057.4
0.80	1985	10.8	2.44	1074.8
0.90	1983	10.7	2.24	839.8
1.00	1981	10.9	2.03	826.5
1.10	1979	12.4	2.46	973.0
1.20	1977	10.8	1.91	673.0
1.30	1975	11.6
1.40	1973	9.6	1.75	643.6
1.50	1971	10.6	2.01	906.9
1.60	1969	10.5	1.82	776.9
1.70	1967		1.98	745.3
1.72	1967	10.4
1.80	1965	9.7	1.99	870.2
1.90	1963		1.80	704.9
1.92	1961	12.4
2.00	1951	10.9	2.25	125.5
2.10	1940		2.25	121.1
2.12	1937	9.7
2.20	1926	9.7	2.20	196.1
2.30	1914		1.92	129.0
2.32	1911	9.3
2.40	1901	11.6	1.65	119.7
2.50	1888	10.8	1.44	91.9
2.60	1876		1.74	122.2
2.62	1873	13.1
2.70	1863		2.24	135.2
2.74	1858	11.5
2.80	1850	10.0	2.09	134.8
2.90	1838		2.44	150.3
2.92	1835	11.2
3.00	1825		2.19	118.3
3.04	1820	10.5
3.10	1813		2.15	119.8
3.14	1807	10.6
3.20	1800		2.24	147.9
3.30	1787		2.37	154.2
3.34	1782	10.7
3.40	1775		1.78	119.3
3.50	1762		2.05	144.5
3.60	1749		2.15	152.2
3.70	1737		2.20	150.3
3.71	1735	10.7
3.80	1724		1.77	107.0
3.90	1711		1.78	121.9
4.00	1699		2.41	145.1
4.01	1697	11.3
4.10	1686		2.02	121.5
4.11	1684	12.9
4.20	1673		2.05	140.2
4.30	1661		2.23	149.3
4.40	1648		2.06	116.0
4.55	1629	10.8
4.56	1628		2.29	137.3
4.68	1612		2.22	138.0
4.78	1600		2.21	141.5
4.88	1587		1.75	119.0
5.09	1561		1.81	120.2
5.20	1548		2.12	152.0
5.29	1535		1.81	145.0
5.35	1527	10.9
5.39	1523		1.37	134.9
5.44	1516		1.16	161.9