Last glacial maximum biomes reconstructed from pollen and plant macrofossil data from northern Eurasia
Biome reconstructions for northern Eurasia 2 1 Pollen and plant macrofossil data from northern Eurasia were used to reconstruct the vegetation of the last glacial maximum (LGM: 18,000±2000 14C yr B.P.) using an objective quantitative method for interpreting pollen data in terms of the biomes they re...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.549.9746 2023-05-15T16:40:39+02:00 Last glacial maximum biomes reconstructed from pollen and plant macrofossil data from northern Eurasia The Pennsylvania State University CiteSeerX Archives 2000 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.9746 http://www.bridge.bris.ac.uk/projects/BIOME_6000/SpecialIssue2/BIOME2_downloads/tarasov.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.9746 http://www.bridge.bris.ac.uk/projects/BIOME_6000/SpecialIssue2/BIOME2_downloads/tarasov.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.bridge.bris.ac.uk/projects/BIOME_6000/SpecialIssue2/BIOME2_downloads/tarasov.pdf text 2000 ftciteseerx 2016-01-08T11:28:09Z Biome reconstructions for northern Eurasia 2 1 Pollen and plant macrofossil data from northern Eurasia were used to reconstruct the vegetation of the last glacial maximum (LGM: 18,000±2000 14C yr B.P.) using an objective quantitative method for interpreting pollen data in terms of the biomes they represent (Prentice et al., 1996). The results confirm previous qualitative vegetation reconstructions at the LGM but provide a more comprehensive analysis of the data. 2 Tundra dominated a large area of northern Eurasia (north of 57°N) to the west, south and east of the Scandinavian ice sheet at the LGM. Text Ice Sheet Tundra Unknown |
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ftciteseerx |
language |
English |
description |
Biome reconstructions for northern Eurasia 2 1 Pollen and plant macrofossil data from northern Eurasia were used to reconstruct the vegetation of the last glacial maximum (LGM: 18,000±2000 14C yr B.P.) using an objective quantitative method for interpreting pollen data in terms of the biomes they represent (Prentice et al., 1996). The results confirm previous qualitative vegetation reconstructions at the LGM but provide a more comprehensive analysis of the data. 2 Tundra dominated a large area of northern Eurasia (north of 57°N) to the west, south and east of the Scandinavian ice sheet at the LGM. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
title |
Last glacial maximum biomes reconstructed from pollen and plant macrofossil data from northern Eurasia |
spellingShingle |
Last glacial maximum biomes reconstructed from pollen and plant macrofossil data from northern Eurasia |
title_short |
Last glacial maximum biomes reconstructed from pollen and plant macrofossil data from northern Eurasia |
title_full |
Last glacial maximum biomes reconstructed from pollen and plant macrofossil data from northern Eurasia |
title_fullStr |
Last glacial maximum biomes reconstructed from pollen and plant macrofossil data from northern Eurasia |
title_full_unstemmed |
Last glacial maximum biomes reconstructed from pollen and plant macrofossil data from northern Eurasia |
title_sort |
last glacial maximum biomes reconstructed from pollen and plant macrofossil data from northern eurasia |
publishDate |
2000 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.9746 http://www.bridge.bris.ac.uk/projects/BIOME_6000/SpecialIssue2/BIOME2_downloads/tarasov.pdf |
genre |
Ice Sheet Tundra |
genre_facet |
Ice Sheet Tundra |
op_source |
http://www.bridge.bris.ac.uk/projects/BIOME_6000/SpecialIssue2/BIOME2_downloads/tarasov.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.9746 http://www.bridge.bris.ac.uk/projects/BIOME_6000/SpecialIssue2/BIOME2_downloads/tarasov.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766031057030742016 |