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TZID:Europe/Berlin
TZUNTIL:20180325T010000Z
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TZNAME:CET
DTSTART:20151025T030000
TZOFFSETFROM:+0200
TZOFFSETTO:+0100
RDATE:20161030T030000
RDATE:20171029T030000
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UID:www.bayceer.uni-bayreuth.de-bayceer-t130712id
DTSTAMP:20260524T130713Z
DESCRIPTION:Since its introduction by the atmospheric chemistry the term 'A
 nthropocene' experienced an almost inflationary use. At first glance\, for
  many disciplines the concept of an age characterized by human-induced cli
 mate and environmental change is attractive. Even the International Commis
 sion on Stratigraphy examines whether the Anthropocene should be formally 
 recognized as new geological era.\nOn closer inspection\, however\, numero
 us difficulties occur\, and especially the begin of this new era is diffic
 ult to grasp. This is particularly evident in the dynamics of the earth's 
 surface: In many landscapes\, changes directly and indirectly caused by hu
 mans are more powerful than the 'natural' processes already for thousands 
 of years. In this talk\, the problem of spatio-temporal discontinuity of t
 he Anthropocene is illustrated using examples from Central Europe\, and a 
 rigid definition is rejected.\n*** invited by Ludwig Zöller\, Geomorpholog
 y
DTSTART;TZID=Europe/Berlin:20160630T120000
DTEND;TZID=Europe/Berlin:20160630T133000
LOCATION:H6\, GEO
SUMMARY:Prof. Dr. Andreas Lang\, Geomorphology and Environmental Systems\, 
 University of Salzburg\, AT (Homepage): The Anthropocene - is there a case
  for a new geological epoch?
TRANSP:TRANSPARENT
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