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Sedimentological data of permafrost cores from Barentburg area
The geochronology was established on the basis of Accelerator Mass Spectrometry (AMS) radiocarbon dates using a Mini Carbon Dating System (MICADAS) implemented at Alfred Wegener... -
AMS 14C ages and calibrated calendar ages of sediment core GeoB22229-1 from R...
AMS-14C ages and calibrated calendar ages, reported as median probability ages. AMS 14C dating was performed at the Analytical Center for Environmental Science, Atmosphere and... -
A global compilation of diatom silica oxygen isotope records from lake sedime...
Oxygen isotopes in biogenic silica (δ18O BSi) from lake sediments allow for quantitative reconstruction of past hydroclimate and proxy–model comparison in terrestrial... -
Foraminifera-bound nitrogen isotope ratios of sediment from the Arctic Ocean
This dataset has no description
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Primary and alternative 14C Bayesian age-depth models of sediment from the Ar...
This dataset has no description
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87Sr/86Sr values and age determination from the Il-Blata section, Malta Islan...
This dataset has no description
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Updated ages for the McMurdo erratics and basis for age changes
LAD: last appearance datum, FAD: first appearance datum, LO: Last occurrence, LCO: Last common occurrence, FO: First occurrenceAntarctica New Zealand Sir Robin Irvine PhD... -
Planktonic 14C dates and calculated calendar ages in core GGC90 (Supplementar...
This dataset has no description
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Radiocarbon dates for DY081-GVY005
All measurements were made on the planktonic foraminifera N. pachyderma.Radiocarbon dates are converted to calendar age using Marine 13, and the mean ocean mixed layer reservoir... -
Age model of sediment core SAT-048A
This dataset includes the age model results of sediment core SAT-048A. -
Age-depth model of sediment core GeoB1720-2 and associated dating uncertainty
Undatable run on 2019-06-17 12:35:41. nsim=10000 bootpc=10 xfactor=0.1 combine=Yes -
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... -
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... -
(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...