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Diatom assebmlages from sediment core Co1305
Diatom analysis was carried out on permanent slides prepared following the settling method of Scherer (1994). -
N-alkanes from sediment core Co1305
n-Alkanes were identified and quantified with a gas chromatograph (GC Agilent 7890B, Agilent Technologies, USA) with flame ionization detector (FID) and capillary column of 50 m... -
Ice rafted debris from sediment core Co1305
The number of particles >1 mm in diameter was quantified by wet sieving on a 1 mm steel mesh sieve. The number of mineral grains retained on the sieve were counted and... -
Water content from sediment core Co1305
This dataset has no description
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Total sulfur, total carbon, carbon stable isotopes, carbon and nitrogen conte...
Elemental analyses of total sulphur (S) and total carbon (C) were conducted with a Vario Micro Cube combustion elemental analyser (Elementar, Germany) was quantified on parallel... -
XRF elemental data of silicon, titanium and sulfur from sediment core Co1305
XRF analysis: We used an ITRAX XRF core scanner (Cox Ltd). Measurements were performed with a chromium X-ray tube with 30 mA, 30 kV, and an exposure time of 20 sec at 2 mm... -
Dinoflagellate cyst counts from IODP Hole 318-U1356A
This dataset has no description
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N-isotopes and amino acids from sediment push cores of SONNE cruise SO242/2 a...
Zero Values = Below Detection Limit -
(Appendix 1) Isoprenoid tetraether lipids in surface sediments of the Mediter...
This dataset has no description
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(Table S4c) Age control points used for calculation of sedimentation rates of...
This dataset has no description
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(Table S3b) 14C ages measured on Globigerinoides sacculifer of sediment core ...
Jaeschke et al.. 2007; 14C ages from GeoB 3910-2. depths are correlated based on tuned Ti/Ca ratios (see Table S2).14C ages, 14C plateaus, and age conversion into calendar ages... -
(Table S1 b) Definition of planktic 14C plateaus for sediment core GeoB3910-1
Very low sedimentation rates below Plateau 3 suggest hiatus. -
(Table S1 a) Definition of planktic 14C plateaus for sediment core GeoB1711-4
Plateau No. 1 - 3: By comparison with Suigetsu Plateau 3 the short length of Plateau 3 may be explained by a ~200-yr drop in local 14C reservoir age over Plateau 3. Its actual... -
(Table S14) Paleomagnetic stratigraphy of ODP Site 208-1266
This dataset has no description
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(Table S13) Paleomagnetic stratigraphy of ODP Site 208-1265
This dataset has no description
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(Table 1) Sample information and stable hydrogen isotope composition of long-...
WMA: Weighted mean average stable hydrogen isotope composition (WMA).Standard deviation: 1 Sigma.a: Analysed sediment interval in cm below sea floor.b: Number of replicate... -
Fatty acid composition of calanoid copepods in the open eastern Atlantic Ocea...
The parameters number 13 and 14, lipids and dry mass, were erroneously marked as "per individual" in [µg/#]. This mistake was corrected on the 2016-05-12. The values are not per... -
(Table 3) Geochemistry of sediment cores from the Souther Ocean
This dataset has no description
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Biomarker distributions at the Last Glacial Maximum (LGM)
Note that '' and '*' denote the LGM time slice identified based on age models published in Nørgaard-Pedersen et al. (2003) and Bazhenova (2012) and Jang et al. (2013),... -
(Table 3) Definition of 14C plateaus for sediment cores SO50-37KL and GIK17940
Combined profil of SO50-37KL and GIK17940.