-
Age models based on palaeomagnetic measurements for the two cores analysed, C...
Palaeomagnetism was the method used for dating sediments older than the time span covered by AMS 14C dating. Geomagnetic palaeointensities recorded in Lake Baikal sediments were... -
Water content and dry bulk density of pilot core CON01-605-3a to piston core ...
Water content and dry bulk density of pilot core CON01-605-3a to piston core CON01-605-3 at Vydrino -
Trace element composition of concretions, ICP–MS measurements
In order to get a complete geochemical signature, 14 P-rich concretions, chosen among the different cores, were acid digested (Table 3a and Table 3b). In a clean laboratory, 1.7... -
Diatom valve concentration in wet sediment, diatom frustule accumulation rate...
At both sites, the lowest dry bulk density values (ca. 0.40 g cm−3) correspond to intervals with high diatom concentrations and high sediment accumulation rate. By contrast, the... -
Water content and dry bulk density of piston core CON01-603-2 from CONTINENT ...
Water content and dry bulk density of piston core CON01-603-2 from CONTINENT Ridge -
δ13C(organic), C/N mass ratios and %TOC for Continent Ridge core CON01-603-5
C/N mass ratios remain constant throughout MIS 3 and into MIS 2, with values between 6.3 and 8.9, indicating no significant terrestrial input of organic matter (Fig. 3). Low... -
HIRM record for CON01-603-2
We established a mastercurve “Baikal 200” of relative paleointensity, which represents a new synthetic paleomagnetic archive for Central Eurasia. The synthetic record is... -
Relative paleointensity record for CON01-603-2
We established a mastercurve “Baikal 200” of relative paleointensity, which represents a new synthetic paleomagnetic archive for Central Eurasia. The synthetic record is... -
Wet bulk density of piston core CON01-605-3 at Vydrino
Wet bulk density of piston core CON01-605-3 at Vydrino -
AMS radiocarbon dates of pollen from Lake Baikal sediments
AMS radiocarbon dates of pollen from Lake Baikal sediments -
Depth versus age based on relative magnetic paleointensity correlations (Fig....
In the figure, the average sedimentation rates are also indicated. The grey bands correspond to the time span of stadial+glacial periods. To the right, the blow-up of the area... -
Depth versus age based on relative magnetic paleointensity correlations for a...
In order to characterise Lake Baikal sedimentary responses to global climatic changes that may be recorded in marine sediments, we compared our paleomagnetically dated... -
Wet bulk density of core CON01-605-3a, the trigger core to piston core CON01-...
Wet bulk density of core CON01-605-3a, the trigger core to piston core CON01-605-3 at Vydrino -
Raw pollen data from the Eemian core CON01-603-2
The studied core CON01-603-2 was recovered from the Continent site, Northern Basin from a water depth of 386 m (Fig. 1) (see Charlet et al., 2005-this volume). The analysed... -
Major composition (wt.%) of concretions, ICP-AES measurements
In order to get a complete geochemical signature, 14 P-rich concretions, chosen among the different cores, were acid digested (Table 3a and Table 3b). In a clean laboratory, 1.7... -
Water content and dry bulk density of pilot core to CON01-603-2, PANGAEA
Water content and dry bulk density of pilot core to CON01-603-2 -
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... -
Water content and dry bulk density of pilot core CON01-604-2a to piston core ...
Water content and dry bulk density of pilot core CON01-604-2a to piston core CON01-604-2 from Posolskoe -
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,...