About: Succession of vascular plants in front of retreating glaciers in central Spitsbergen     Goto   Sponge   NotDistinct   Permalink

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Description
  • Vegetation succession in front of five retreating glaciers was studied using phytosociological releves (60) located at different distances between the Little Ice Age (LIA) moraines and the present glacier fronts around Petunia Bay. Approximate dating of succession stages was based on a study of the changing position of glacier fronts in the past approximately 100 years. The described succession corresponds to the uni-directional, non-replacement model of succession. All constituent species, except one, present in the nearby old tundra have colonized the glacier forelands since the end of the LIA. The first species appeared about 5 years after deglaciation. The latest succession stages closely resemble the old tundra.
  • Vegetation succession in front of five retreating glaciers was studied using phytosociological releves (60) located at different distances between the Little Ice Age (LIA) moraines and the present glacier fronts around Petunia Bay. Approximate dating of succession stages was based on a study of the changing position of glacier fronts in the past approximately 100 years. The described succession corresponds to the uni-directional, non-replacement model of succession. All constituent species, except one, present in the nearby old tundra have colonized the glacier forelands since the end of the LIA. The first species appeared about 5 years after deglaciation. The latest succession stages closely resemble the old tundra. (en)
Title
  • Succession of vascular plants in front of retreating glaciers in central Spitsbergen
  • Succession of vascular plants in front of retreating glaciers in central Spitsbergen (en)
skos:prefLabel
  • Succession of vascular plants in front of retreating glaciers in central Spitsbergen
  • Succession of vascular plants in front of retreating glaciers in central Spitsbergen (en)
skos:notation
  • RIV/60076658:12310/12:43884218!RIV13-MSM-12310___
http://linked.open...avai/predkladatel
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(LA341), P(LM2010009), Z(AV0Z60050516), Z(MSM6007665801)
http://linked.open...iv/cisloPeriodika
  • 4
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 172378
http://linked.open...ai/riv/idVysledku
  • RIV/60076658:12310/12:43884218
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • vegetation succession; glacier forelands; climate warming; Svalbard; Arctic (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • PL - Polská republika
http://linked.open...ontrolniKodProRIV
  • [0DF6007C476A]
http://linked.open...i/riv/nazevZdroje
  • Polish Polar Research
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 33
http://linked.open...iv/tvurceVysledku
  • Prach, Karel
  • Rachlewicz, Grzegorz
http://linked.open...ain/vavai/riv/wos
  • 000312928500003
http://linked.open...n/vavai/riv/zamer
issn
  • 0138-0338
number of pages
http://bibframe.org/vocab/doi
  • 10.2478/v10183-012-0022-3
http://localhost/t...ganizacniJednotka
  • 12310
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