-
Data concerning preparation of pollen concentrates and graphite targets and r...
Laboratory processing of concentrates was aimed at the removal of non-sporomorph organic matter by means of chemical treatment, micro-sieving and heavy liquid seperation. The... -
Raw pollen data from kasten core CON01-603-5 part1 (counts)
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... -
Biovolume accumulation rates for the dominant planktonic taxa plotted against...
S. grandis is by far the species that contributes the most to the total biovolume accumulation rate with a peak value just above 4×106 μm3 cm−2 year−1. Its relative contribution... -
Wet bulk density (GRAPE) of pilot core CONT01-604-3a to piston core CON01-604...
Wet bulk density (GRAPE) of pilot core CONT01-604-3a to piston core CON01-604-3 at Posolskoe -
Wet bulk density (GRAPE) of trigger core CON01-605-4a to piston core CON01-60...
Wet bulk density (GRAPE) of trigger core CON01-605-4a to piston core CON01-605-4a at Vydrino -
Raw pollen data from kasten core CON01-603-5 part1 (%)
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... -
Down-core variations of the inclination and declination of ChRM of all invest...
Dashed lines mark some correlation levels of the cores from Lake Baikal with the dated δ18O record from ODP 677 (Shackleton et al., 1990), see also Fig. 3. Diagenetic features... -
Downcore variations of rock magnetic parameters (ARM, S-ratio and HIRM) for C...
No significant HIRM change is observed at the transition between oxidising and reducing conditions in the sediment (Fig. 9A). This implies that HIRM is not affected by redox... -
Inclination, declination and the reversal angle of the ChRM for CON01-603-2
Selected intervals of down-core variations of normalised relative paleointensity, ChRM inclination and declination, and the reversal angle. (A) Core CON 01-603-2: numbers in the... -
Downcore variations of the SIRM/κLF for CON01-603-2, CON01-604-2, CON01-605-3...
Greigite levels in glacial sediments cannot be correlated between cores (Fig. 12), which suggests that greigite concentrations are driven by local processes. We suggest that... -
Downcore variations of SIRM/κLF for CON01-603-2
Increased presence of greigite (high SIRM/κLF) coincides with maximum sulphur contents observed at the beginning of interglacial stages (Fig. 11A). At similar levels in another... -
Downcore variations of normalised relative paleointensity for CON01-603-2, VE...
Selected intervals of down-core variations of normalised relative paleointensity, ChRM inclination and declination, and the reversal angle. (A) Core CON 01-603-2: numbers in the... -
Down-core variations of anhysteretic remanent magnetisation and simplified li...
Conceptual intercorrelation between ARM and simplified lithology and correlation to the δ18O record from ODP Site 677 (Shackleton et al., 1990), assuming that clay-rich layers... -
Raw pollen data from piston core CON01-605-3 (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... -
Down-core variations of normalised relative paleointensity after removal of i...
Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis (magnetite dissolution and/or greigite formation) and correlation to... -
Raw pollen data from kasten core CON01-603-5 part2 (%)
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 (GRAPE) of piston core CON01-603-2 from CONTINENT Ridge
Wet bulk density (GRAPE) of piston core CON01-603-2 from CONTINENT Ridge -
Data for the relative percentages of the dominant diatom taxa related to core...
Dissolution was high throughout the profile—in most cases, only 10–20% of the valves considered as pristine (Fig. 4). High relative percentages of A. baicalensis and of benthic... -
Vector endpoint data for CON01-603-2.
Three representative vector endpoint diagrams: (A) sample from a clay-rich layer, exhibiting normal polarity; (B) sample from a clay-rich layer, exhibiting reverse polarity,... -
Down-core variations of the SIRM for CON01-603-2.
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...
