Data Publications

Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis

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
  • 2006-09-13
hasDataset_Title
  • Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis
hasEntry_ID
  • 10.1594/GFZ.SDDB.1012
hasKeyword
  • NRM30/ARM30
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
  • Down-core variations of normalised relative paleointensity after removal of intervals affected by diagenesis (magnetite dissolution and/or greigite formation) and correlation to the relative paleointensity record from ODP Site 984 (Channell, 1999). In addition to AMS 14C dating and the geomagnetic excursions, the age model was completed and refined by tuning the relative paleointensity records to the equivalent record from ODP Site 984 (Channell, 1999; Fig. 8). The relative paleointensity variations in Lake Baikal and ODP Site 984 are well correlated. This confirms the global geomagnetic field origin of the relative paleointensity variations documented in the present study. In addition, it shows that local sedimentary variations have no effect on the paleomagnetic records.
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