Data Publications

Paleointensity versus age of all the sedimentary sequences of the present study

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
  • Paleointensity versus age of all the sedimentary sequences of the present study
hasEntry_ID
  • 10.1594/GFZ.SDDB.1017
hasKeyword
  • age (calendar years)
  • normalised relative palaeointensity
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
  • 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 curve from ODP Site 984 (Channell, 1999). For the compilation, data have been averaged using a sliding window of 2 ka (the variance is marked by the grey shadow). Dashed lines show some of the correlations. The grey lines show the location of the low paleointensities related to geomagnetic excursions. Note that the lowest paleointensities in the time span of Blake are at c. 129 ka. (see Fig.11)
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