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TZUNTIL:20161030T010000Z
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DTSTART:20141026T030000
TZOFFSETFROM:+0200
TZOFFSETTO:+0100
RDATE:20151025T030000
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DTSTART:20140330T020000
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UID:www.bayceer.uni-bayreuth.de-bayceer-t119656id
DTSTAMP:20260405T032645Z
DESCRIPTION:Time scales are the backbone of very most studies dealing with 
 past environments and climates. Ironically\, the time scales and their (in
 )accuracy are often much less understood than proxy data for past environm
 ental conditions. The ‘state of the art’ of the (Quaternary) geological ti
 me scale\, including some shortcomings and improvement potential are outli
 ned. Integrated stratigraphy using independent geochronometers is the best
  way to obtain reliable age models\, statistical combination of methods is
 \, however\, not straightforward. Finally an example is given how more pre
 cise time scales can lead to a much better understanding of geoarchives. A
  personal perspective is given where time scale development may improve in
  the coming years.\n***\nEingeladen von Ulrich Hambach\, Lehrstuhl für Geo
 morphologie
DTSTART;TZID=Europe/Berlin:20141113T000000
DTEND;TZID=Europe/Berlin:20141113T235959
SUMMARY:Dr. Christian Zeeden\, Department of Geography - RWTH Aachen Univer
 sity (Homepage): Time matters: about constructing geological time scales
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