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X-WR-TIMEZONE:Europe/Berlin
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TZID:Europe/Berlin
TZUNTIL:20171029T010000Z
BEGIN:STANDARD
TZNAME:CET
DTSTART:20151025T030000
TZOFFSETFROM:+0200
TZOFFSETTO:+0100
RDATE:20161030T030000
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TZNAME:CEST
DTSTART:20150329T020000
TZOFFSETFROM:+0100
TZOFFSETTO:+0200
RDATE:20160327T020000
RDATE:20170326T020000
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UID:www.bayceer.uni-bayreuth.de-bayceer-t127720id
DTSTAMP:20260818T120649Z
DESCRIPTION:Climate change\, warming and associated drought effects in part
 icular\, affect the species composition in low-temperature determined high
  mountain vegetation. A complex topography and thus high habitat diversity
  over short distances as well the persistence abilities of many alpine pla
 nt species may counter biodiversity losses caused by climate-driven specie
 s migrations. Revisitation studies in the late 20th century\, nevertheless
 \, mostly report on increasing species numbers on mountain tops\, resultin
 g from upward moving leading edges of species’ distribution margins. Repea
 ted revisitations now show a marked acceleration of growing species richne
 ss on high mountain peaks. At the same time\, the species composition shif
 ts towards more thermophilous species numbers across Europe – a process wh
 ich also tends to accelerate. Recent monitoring results of the central hig
 h Alps\, however\, show that rates of colonising species remained constant
  in the past decade\, compared to the previous one\, but the proportion of
  species not found again was rising. In parts of Europe’s mountains\, the 
 projected period or era of warming-driven biodiversity losses\, thus\, may
  already have commenced.\n\n \n***\nInvited by Cyrus Samimi\, Climatology
DTSTART;TZID=Europe/Berlin:20151203T120000
DTEND;TZID=Europe/Berlin:20151203T133000
LOCATION:H6\, GEO
SUMMARY:Dr. Harald Pauli\, Department of Conservation Biology\, Vegetation 
 and Landscape Ecology Institute of Ecology and Conservation Biology Univer
 sity of Vienna (Homepage): Past and recent changes in European alpine plan
 t diversity: increases\, declines\, stagnations and accelerations driven b
 y climate change
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