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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 -
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... -
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 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 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... -
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... -
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 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... -
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 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... -
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... -
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 -
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 -
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... -
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... -
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...