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Down-core variations of normalised relative paleointensity and ARM/SIRM after...
The concentration in ferromagnetic particles is much lower in the interglacial sediments than in glacial sediments. Therefore, the NRM needs to be normalised by a... -
Diatom concentration for Continent Ridge core CON01-603-5
All diatoms in the analysed section were extensively affected by dissolution with only c. 1% of valves in a “pristine” condition. Diatom concentrations were generally extremely... -
Pollen counts from Kasten corer CON01-603-5, CONTINENT Ridge
Pollen counts from Kasten corer CON01-603-5 at CONTINENT Ridge. -
XRF titanium, iron counting and ratio Fe/Ti for CON01-603-2 and VER98-1-14
In selected intervals, we measured titanium and iron contents in parallel to rock magnetic parameters (Fig. 9). Titanium content is a good reflection of detrital input since... -
Dry bulk density and water content of piston core CON01-605-3 from Vydrino
Dry bulk density and water content of piston core CON01-605-3 from Vydrino -
Hysteresis measurements (uncorrected and corrected for the paramagnetic influ...
Hysteresis measurements of a greigite dominated clay -rich layer with single-domain behaviour hysteresis loop for VER98-1-1. -
Selected electron-microprobe analyses of vivianite and santabarbaraite from L...
Electron-microprobe analyses (Table 5) were completed on a selection of grains from 11 samples, with a CAMECA SX-50 instrument (University of Louvain-la-Neuve, Belgium), under... -
Wet bulk density of core CON01-604-2a, the trigger core to piston core CON01-...
Wet bulk density of core CON01-604-2a, the trigger core to piston core CON01-604-2 at Posolskoe -
Downcore variations of the S-ratio for CON01-603-2, CON01-604-2, CON01-605-3,...
In interglacial sediments, the magnetic assemblages depict changes in the sedimentation rate, which are traced using the ratio of magnetite over hematite (S-ratio). At the... -
Unit-cell parameters and Mn(Fe+Mn) ratios of vivianites from Lake Baikal
The unit-cell parameters (Table 4) were calculated with the least-squares refinement program LCLSQ 8.4 (Burnham, 1991), from the d-spacings corrected with an internal standard... -
Vertical distribution in the sediment of the different animal groups found in...
The vertical distribution of organisms in the sediment indicates that animals can be present as deep as 15 cm although at very low abundance at such depths (Fig. 4, Fig. 5 and... -
Composition of major oxide in bulk sediments from lake Baikal: ICP-AES data f...
The sediment cores were sampled with a resolution of 10 cm, resulting in a total of 290 samples (Table 2). Around 250 mg of dried sediments was mechanically crushed through... -
%dry weight and %loss on ignition for CON01-603-5
%dry weight and %loss on ignition for CON01-603-5 -
Raw pollen data from kasten core CON01-605-5 (Vydrino)
Sediment slices of 0.5 cm thickness were obtained from gravity core segments and of 1 cm thickness from the Vydrino piston core. Volumetric subsamples of 5 cm3 (10 cm3 in case... -
Wet bulk density of core CON01-603-4a, the trigger core to piston core CON01-...
Wet bulk density of core CON01-603-4a, the trigger core to piston core CON01-603-4 at CONTINENT Ridge -
Paleointensity versus age of all the sedimentary sequences of the present study
Paleointensity versus age of all the sedimentary sequences of the present study, of the synthetic curve resulting from its compilation from other curves, and of the reference... -
Wet bulk density of core CON01-605-2a, the trigger core to piston core CON01-...
Wet bulk density of core CON01-605-2a, the trigger core to piston core CON01-605-2 at Vydrino -
Downcore variations of the opal content for the sedimentary sequence of VER98...
Opal content was obtained by measuring the NaCO3 leached solution by inductive coupled plasma with an optical emission spectrometer (ICP-OES). The clay-rich layers are... -
Wet bulk density of pilot core to CON01-603-2 (CONTINENT Ridge) measured by G...
Wet bulk density of pilot core to CON01-603-2 (CONTINENT Ridge) measured by GRAPE density -
Densities of benthic taxa with depth (CON 01-01 and CON 01-04 expeditions).
In all abyssal stations, densities are never over an average of c. 3100 individuals m−2 (Fig. 3, Table 1). In contrast, the shallow station (CON01-427, Posolskoe Bank) harbours...