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A new bathymetric map of Lake Baikal
In 1999 it was decided to create an international team of specialists and combine efforts and expertise to produce a new, more accurate bathymetric map of Lake Baikal. The aim... -
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... -
Related materials to Lauterbach et al. (2011) Environmental responses to Late...
Investigation of the sedimentary record of pre-Alpine Lake Mondsee (Upper Austria) focused on the environmental reaction to rapid Lateglacial climatic changes. Results of this... -
Density of Core Samples of the KTB Main Hole HB1a
The density of rocks depends on the mineral contents and is therefore a helpful property for the discrimination of lithological units. It is also used for the calculation of... -
Natural Remanent Magnetisation of Cores of the KTB Main Hole HB1a
Natural Remanent Magnetisation of Cores of the KTB Main Hole HB1a -
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 -
Magnetic Susceptibility of Mini-Cores of the KTB Main Hole HB1a
The magnetic susceptibility is measured by an inductive AC device (BARTINGTON). The sample is placed inside a coil which generates an alternating magnetic field. The applied... -
SAFOD Main Hole downhole logging data phase 1.2 1744-1932m
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major... -
Relative percentage diatom profile for BAIK38 (BAIK94-38A), using uncorrected...
Fig. 3 is the diatom stratigraphy of dominant phytoplankton taxa for BAIK38 expressed as relative percentages, plotted against the age scale. Zone 1 (c. 880 AD–c. 1180 AD) is... -
%dry weight and %loss on ignition for CON01-603-5
%dry weight and %loss on ignition for CON01-603-5 -
XRD of Cores of the KTB Main Hole HB1a
The qualitative and quantitative phase analyses were performed in the KTB field laboratory by x-ray powder diffraction using SIEMENS D 500 diffractometer. During early stages of... -
Gas chromatography of gas samples of the KTB pilot hole VB!
The main objective of this drilling fluid analysis was the detection of inflows of formation fluids. Therefore different gases dissolved in the drilling mud were measured... -
Depth profiles of the contribution to total chlorophyll a+chlorophyllide a by...
Calculations were based on factors established for 89 water samples across Lake Baikal in July 2001 (see text). The traps were deployed for about 16 months and the core top... -
Lacustrine sediments of Lake Baikal
Lake Baikal sediment map from Sturm, M., Vologina, E. G., Levina, O. V., Flower, R. J., Ryves, D. B. & Lees, J. A. (1998) Hemipelagic sedimentation and turbidites in the... -
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... -
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... -
Supplementary material to Mangili et al. (2010): Climatic implications of ann...
Stable oxygen isotope analyses at annual, 2-, 5-, 10- and 20-varve sample resolutions were carried out on two selected varve intervals from the interglacial sediment record of... -
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... -
Thermal Conductivity of Cuttings of the KTB Main Hole HB1 (measured data)
In the KTB field laboratory, thermal conductivity was measured on cuttings material in depth intervals of 10 m and on available drill core material. The results on drill cores...
