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3130 data publications found
Data concerning preparation of pollen concentrates and graphite targets and results of dating.
Piotrowska, Natalia | Bluszcz, Andrzej | Demske, Dieter | Granoszewski, Wojciech | Heumann, Georg
2006
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 optained concentrates were checked under the microscope and sample purity was estimated on the basis of particle...
Depth versus age based on relative magnetic paleointensity correlations for all six investigated sites
Demory, Francois | Nowaczyk, Norbert | Witt, Annette | Oberhänsli, Hedi
2006
In order to characterise Lake Baikal sedimentary responses to global climatic changes that may be recorded in marine sediments, we compared our paleomagnetically dated climate-proxy record from Lake Baikal with benthic and plankontic δ18O curves of ODP Site 983, a site close to ODP Site 984....
High temperature measurements of magnetic susceptibility in clay-rich layers for VER98-1-14
Demory, Francois | Oberhänsli, Hedi | Nowaczyk, Norbert | Gottschalk, Matthias | Wirth, Richard | Naumann, Rudolf
2006
High temperature measurements of magnetic susceptibility in clay-rich layers. Magnetite, characterised by a Curie temperature of 590 °C, dominates the signal.
High temperature measurements of magnetic susceptibility in clay-rich layers
Demory, Francois | Oberhänsli, Hedi | Nowaczyk, Norbert | Gottschalk, Matthias | Wirth, Richard | Naumann, Rudolf
2006
High temperature measurements of magnetic susceptibility in clay-rich layers. Magnetite, characterised by a Curie temperature of 590 °C, dominates the signal.
Down-core variations of the inclination and declination of ChRM of all investigated cores.
Demory, Francois | Nowaczyk, Norbert | Witt, Annette | Oberhänsli, Hedi
2006
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 such as dissolution of magnetite and mineralization of greigite are marked according to Fig. 4. Laschamp and Iceland...
High temperature measurements of magnetic susceptibility in diatomaceous layers for VER98-1-1
Demory, Francois | Oberhänsli, Hedi | Nowaczyk, Norbert | Gottschalk, Matthias | Wirth, Richard | Naumann, Rudolf
2006
High temperature measurements of magnetic susceptibility in diatomaceous layers. Most of the weak susceptibility is still present up to the temperature of 670 °C and carried by hematite.
Related materials to Lauterbach et al. (2011) Environmental responses to Lateglacial climatic fluctuations recorded in the sediments of pre-Alpine Lake Mondsee (northeastern Alps)
Lauterbach, Stefan | Brauer, Achim | Andersen, Nils | Danielopol, Dan | Dulski, Peter | Hüls, Matthias | Milecka, Krystyna | Namiotko, Tadeusz | Obremska, Milena | Von Grafenstein, Ulrich
2011
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 study reveal complex proxy responses that are variable in time and influenced by the long-term evolution of the lake...
Supplementary material to Lauterbach et al. (2010): Multi-proxy evidence for early to mid-Holocene environmental and climatic changes in northeastern Poland
Lauterbach, S | Brauer, A. | Andersen, N. | Danielopol, D.L. | Dulski, P. | Hüls, M. | Milecka, K. | Namiotko, T. | Plessen, B. | Von Grafenstein, U. | Participants DECLAKES
2010
We investigated the sedimentary record of Lake Hancza (northeastern Poland) using a multi-proxy approach, focusing on early to mid-Holocene climatic and environmental changes. AMS 14C dating of terrestrial macrofossils and sedimentation rate estimates from occasional varve thickness...
Down-core variations of normalised relative paleointensity and ARM/SIRM after diagenetic correction for CON01-603-2.
Demory, Francois | Nowaczyk, Norbert | Witt, Annette | Oberhänsli, Hedi
2006
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 concentration-related parameter, such as κLF, ARM or SIRM, in order to generate relative paleointensity records free of the...
XRD of Cuttings of the KTB Main Hole HB1i
KTB, WG Geochemistry
2010
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 the KTB project a new method for quantitative phase analysis was developed (see references below). The method is...