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Elemental ratios from sediment core MD01-2444 on the Portuguese Margin, Marin...
XRF Analysis: Archive halves of sections from Core MD01-2444 were analysed using an Avaatech XRF core scanner at the University of Cambridge. The core surface was carefully... -
Age model output of ice core Skytrain Ice Rise
Age model derived using Paleochrono program using fixed tiepoints described in the paper. Our recommended ice age scale uses ALC age until 1337 a bp and Paleochrono for all... -
Methane concentrations of ice core Skytrain Ice Rise
Continuous CH4 determined by cavity ringdown spectroscopy (Picarro G2301 CRDS) on air separated from meltwater from a continuous flow melt device. -
Gas properties in ice core #23 from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Gas properties at core depth 1.95 m in ice cores from Larsen blue ice area, E...
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Ice properties at core depth 1.95 m in ice cores from Larsen blue ice area, E...
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Properties of ice core #23 from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Ice surface measurements from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
Delta age in ice cores from Larsen blue ice area, East Antarctica
Blue ice areas (BIAs) have several advantages for reconstructing past climate. However, the complicated ice flow in the areas hinders constraining the age. We apply... -
CaCO3 content from sediment core MD01-2444 on the Portuguese Margin, Marine I...
Carbonate content: Bulk sediment was acidified with 10% phosphoric acid using an AutoMateFX carbonate preparation system and evolved CO2 was measured using a UIC (Coulometrics)... -
Pollen data from sediment core MD01-2444 on the Portuguese Margin, Marine Iso...
Pollen analysis: Sediment samples of 1.5-4 cm3 were prepared for pollen analysis using the standard hot acid digestion technique. Fine sieving, through a mesh of 10 m or less,... -
Alkenone sea surface temperatures Uk'37-SST from sediment core MD01-2444 on t...
Alkenone SST: Sediment samples (2.5 to 2.57 g) were freeze-dried and extracted by sonication using dichloromethane. The extracts were dried under nitrogen and hydrolysed with 7%... -
Neogloboquadrina pachyderma and Ice rafted detritus abundance from sediment c...
Planktonic Foraminifera Fauna: Identification of N. pachyderma in the greater than 150 micron size fraction was carried out on split subsamples containing at least 300 whole... -
d18O of bulk carbonate from sediment core MD01-2444 on the Portuguese Margin,...
Bulk carbonate oxygen isotopes: Oxygen isotopes were measured using a ThermoFisher GasBench II equipped with a CTC Combi-Pal autosampler and interfaced via continuous flow with... -
δ¹⁸O of benthic foraminifera from sediment core MD01-2444 on the Portuguese M...
Benthic foraminifera oxygen isotopes: The benthic isotope record was generated by the late N.J. Shackleton. Measurements were carried out in the Godwin Laboratory for... -
d18O of Globigerina bulloides from sediment core MD01-2444 on the Portuguese ...
Planktonic foraminifera (G. bulloides) oxygen isotopes: Measurements of foraminiferal stable isotopes were carried out in the Godwin Laboratory for Palaeoclimate Research... -
Ice core O2 clumped isotope data from the Last Glacial Maximum measured in We...
Laboratory O2 clumped-isotope data (as D36 values measured at Rice University) for air occluded in ice core WDC06A spanning gas ages of 18000-21000 ky BP for the Last Glacial...
