Ecol1_10PanovaLO.fm
Abstract-A comprehensive analysis of samples from a frozen peat deposit in the upper reaches of the Khadytayakha River by palynological, carpological, entomological, and radiocarbon methods has been per formed to reconstruct changes in the regional and local vegetation and climatic conditions during...
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1050.5518 |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1050.5518 2023-05-15T18:28:12+02:00 Ecol1_10PanovaLO.fm Tavolk The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1050.5518 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1050.5518 Metadata may be used without restrictions as long as the oai identifier remains attached to it. https://ipae.uran.ru/sites/default/files/publications/Trofimova_SS/Trofimova_2010_1_eng.pdf text ftciteseerx 2020-04-05T00:28:24Z Abstract-A comprehensive analysis of samples from a frozen peat deposit in the upper reaches of the Khadytayakha River by palynological, carpological, entomological, and radiocarbon methods has been per formed to reconstruct changes in the regional and local vegetation and climatic conditions during the Holocene. The results show that this peat deposit was formed from 8000 to 5000 years BP. During that period, the climate in the southern Yamal Peninsula was considerably warmer, and the present day subarctic shrub tundra zone was occupied by plant communities of spruce, birch, and larch forests. Text Subarctic Tundra Yamal Peninsula Unknown Khadytayakha ENVELOPE(69.250,69.250,66.800,66.800) Yamal Peninsula ENVELOPE(69.873,69.873,70.816,70.816) |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
| description |
Abstract-A comprehensive analysis of samples from a frozen peat deposit in the upper reaches of the Khadytayakha River by palynological, carpological, entomological, and radiocarbon methods has been per formed to reconstruct changes in the regional and local vegetation and climatic conditions during the Holocene. The results show that this peat deposit was formed from 8000 to 5000 years BP. During that period, the climate in the southern Yamal Peninsula was considerably warmer, and the present day subarctic shrub tundra zone was occupied by plant communities of spruce, birch, and larch forests. |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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Tavolk |
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Tavolk Ecol1_10PanovaLO.fm |
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Tavolk |
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Tavolk |
| title |
Ecol1_10PanovaLO.fm |
| title_short |
Ecol1_10PanovaLO.fm |
| title_full |
Ecol1_10PanovaLO.fm |
| title_fullStr |
Ecol1_10PanovaLO.fm |
| title_full_unstemmed |
Ecol1_10PanovaLO.fm |
| title_sort |
ecol1_10panovalo.fm |
| url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1050.5518 |
| long_lat |
ENVELOPE(69.250,69.250,66.800,66.800) ENVELOPE(69.873,69.873,70.816,70.816) |
| geographic |
Khadytayakha Yamal Peninsula |
| geographic_facet |
Khadytayakha Yamal Peninsula |
| genre |
Subarctic Tundra Yamal Peninsula |
| genre_facet |
Subarctic Tundra Yamal Peninsula |
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https://ipae.uran.ru/sites/default/files/publications/Trofimova_SS/Trofimova_2010_1_eng.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1050.5518 |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766210581130379264 |