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rdf:type
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Description
| - To characterize Late Pleniglacial (LPG: 26.5-15 lea cal BP) and particularly Last Glacial Maximum (LGM: 21 +/- 2 lea cal BP) vegetation and climate, fossil pollen assemblages are often compared with modern pollen assemblages. Given the non-analogue climate of the LPG, a key question is how glacial pollen assemblages and thereby vegetation compare with modern vegetation. In this paper we present three LPG pollen records from the Carpathian Basin and the adjoining Carpathian Mountains to address this question and provide a concise compositional characterization of the LPG vegetation. Fossil pollen assemblages were compared with surface pollen spectra from the Altai-Sayan Mountains in southern Siberia. This area shows many similarities with the LPG vegetation of eastern-central Europe, and has long been considered as its best modern analogue. Ordination and analogue matching were used to characterize vegetation composition and find the best analogues.
- To characterize Late Pleniglacial (LPG: 26.5-15 lea cal BP) and particularly Last Glacial Maximum (LGM: 21 +/- 2 lea cal BP) vegetation and climate, fossil pollen assemblages are often compared with modern pollen assemblages. Given the non-analogue climate of the LPG, a key question is how glacial pollen assemblages and thereby vegetation compare with modern vegetation. In this paper we present three LPG pollen records from the Carpathian Basin and the adjoining Carpathian Mountains to address this question and provide a concise compositional characterization of the LPG vegetation. Fossil pollen assemblages were compared with surface pollen spectra from the Altai-Sayan Mountains in southern Siberia. This area shows many similarities with the LPG vegetation of eastern-central Europe, and has long been considered as its best modern analogue. Ordination and analogue matching were used to characterize vegetation composition and find the best analogues. (en)
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Title
| - Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia?
- Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia? (en)
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skos:prefLabel
| - Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia?
- Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia? (en)
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skos:notation
| - RIV/00216224:14310/14:00074251!RIV15-GA0-14310___
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http://linked.open...avai/riv/aktivita
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http://linked.open...avai/riv/aktivity
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http://linked.open...iv/cisloPeriodika
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http://linked.open...vai/riv/dodaniDat
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http://linked.open...aciTvurceVysledku
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http://linked.open.../riv/druhVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...titaPredkladatele
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http://linked.open...dnocenehoVysledku
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http://linked.open...ai/riv/idVysledku
| - RIV/00216224:14310/14:00074251
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http://linked.open...riv/jazykVysledku
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http://linked.open.../riv/klicovaSlova
| - Last Glacial Maximum; Late Pleniglacial vegetation; Modern analogue; Carpathians; Carpathian Basin (en)
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http://linked.open.../riv/klicoveSlovo
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http://linked.open...odStatuVydavatele
| - GB - Spojené království Velké Británie a Severního Irska
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http://linked.open...ontrolniKodProRIV
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http://linked.open...i/riv/nazevZdroje
| - Quaternary Science Reviews
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http://linked.open...in/vavai/riv/obor
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http://linked.open...ichTvurcuVysledku
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http://linked.open...cetTvurcuVysledku
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http://linked.open...vavai/riv/projekt
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http://linked.open...UplatneniVysledku
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http://linked.open...v/svazekPeriodika
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http://linked.open...iv/tvurceVysledku
| - Chytrý, Milan
- Kuneš, Petr
- Pelánková, Barbora
- Braun, Mihály
- Jakab, Gusztav
- Magyari, Enikö Katalin
- Schäbitz, Frank
- Sümegi, Pál
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http://linked.open...ain/vavai/riv/wos
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issn
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number of pages
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http://bibframe.org/vocab/doi
| - 10.1016/j.quascirev.2014.04.020
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http://localhost/t...ganizacniJednotka
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