Data Publications

Depth versus age based on relative magnetic paleointensity correlations (Fig. 8) for all six investigated sites

hasData_Center_Short_Name
  • SDDB
hasDataset_Online_Resource
hasProject_Long_Name
  • Vereshchagin 98 Expedition
  • Vereshchagin Expedition 98
  • Vereshchagin Long Cores Expedition 2001
  • High-resolution CONTINENTal paleoclimate record in Lake Baikal
hasDataset_Release_Date
  • 2006-09-15
hasDataset_Title
  • Depth versus age based on relative magnetic paleointensity correlations (Fig. 8) for all six investigated sites
hasEntry_ID
  • 10.1594/GFZ.SDDB.1013
hasKeyword
  • age (calendar years)
hasReference
  • 10.1016/j.gloplacha.2004.09.016 http://dx.doi.org/10.1016/j.gloplacha.2004.09.016 Francois Demory, Norbert R. Nowaczyk, Annette Witt and Hedi Oberhansli, High-resolution magnetostratigraphy of late quaternary sediments from Lake Baikal, Siberia: timing of intracontinental paleoclimatic responses, Global and Planetary Change, Volume 46,
hasSummary
  • 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 of the diagram covering 200 cm shows the AMS 14C dating for the last 20 ka, including error bars. (see Fig.9)The long, continuous paleointensity record (CON 01-603-2) has a resolution of ca. 350 years, and the resolution of its correlation with the reference curve is of ca. 3.5 ka or approximately every 10 samples (55 points of correlation span the last 200 ka). Such high resolution for telecorrelation might be more critical because of possible delays caused by differing remanence acquisition processes, local sedimentary or unresolved geochemical influences and regional nondipolar components of the geomagnetic field.
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