Modern tundra landscapes of the Kolyma Lowland and their evolution in the Holocene
The different tundra landscapes of the Kolyma Lowland, northern Siberia are described, focusing on landscape typology, digital mapping and the calculation of areas occupied by different landscape complexes. The genesis, age and evolution of ‘yedoma’ sediments and associated alas (thermokarst basins)...
Published in: | Permafrost and Periglacial Processes |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
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Online Access: | https://doi.org/10.1002/ppp.674 |
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ftrepec:oai:RePEc:wly:perpro:v:20:y:2009:i:4:p:399-406 2023-05-15T18:32:57+02:00 Modern tundra landscapes of the Kolyma Lowland and their evolution in the Holocene Alexandra Veremeeva Stanislav Gubin https://doi.org/10.1002/ppp.674 unknown https://doi.org/10.1002/ppp.674 article ftrepec https://doi.org/10.1002/ppp.674 2020-12-04T13:31:03Z The different tundra landscapes of the Kolyma Lowland, northern Siberia are described, focusing on landscape typology, digital mapping and the calculation of areas occupied by different landscape complexes. The genesis, age and evolution of ‘yedoma’ sediments and associated alas (thermokarst basins) topography are inferred from the calculation of lake‐basin and lake‐area changes over three decades. Connections between the present landscape and its evolution during the Holocene are described. Copyright © 2009 John Wiley & Sons, Ltd. Article in Journal/Newspaper Thermokarst Tundra Siberia RePEc (Research Papers in Economics) Kolyma ENVELOPE(161.000,161.000,69.500,69.500) Permafrost and Periglacial Processes 20 4 399 406 |
institution |
Open Polar |
collection |
RePEc (Research Papers in Economics) |
op_collection_id |
ftrepec |
language |
unknown |
description |
The different tundra landscapes of the Kolyma Lowland, northern Siberia are described, focusing on landscape typology, digital mapping and the calculation of areas occupied by different landscape complexes. The genesis, age and evolution of ‘yedoma’ sediments and associated alas (thermokarst basins) topography are inferred from the calculation of lake‐basin and lake‐area changes over three decades. Connections between the present landscape and its evolution during the Holocene are described. Copyright © 2009 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Alexandra Veremeeva Stanislav Gubin |
spellingShingle |
Alexandra Veremeeva Stanislav Gubin Modern tundra landscapes of the Kolyma Lowland and their evolution in the Holocene |
author_facet |
Alexandra Veremeeva Stanislav Gubin |
author_sort |
Alexandra Veremeeva |
title |
Modern tundra landscapes of the Kolyma Lowland and their evolution in the Holocene |
title_short |
Modern tundra landscapes of the Kolyma Lowland and their evolution in the Holocene |
title_full |
Modern tundra landscapes of the Kolyma Lowland and their evolution in the Holocene |
title_fullStr |
Modern tundra landscapes of the Kolyma Lowland and their evolution in the Holocene |
title_full_unstemmed |
Modern tundra landscapes of the Kolyma Lowland and their evolution in the Holocene |
title_sort |
modern tundra landscapes of the kolyma lowland and their evolution in the holocene |
url |
https://doi.org/10.1002/ppp.674 |
long_lat |
ENVELOPE(161.000,161.000,69.500,69.500) |
geographic |
Kolyma |
geographic_facet |
Kolyma |
genre |
Thermokarst Tundra Siberia |
genre_facet |
Thermokarst Tundra Siberia |
op_relation |
https://doi.org/10.1002/ppp.674 |
op_doi |
https://doi.org/10.1002/ppp.674 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
20 |
container_issue |
4 |
container_start_page |
399 |
op_container_end_page |
406 |
_version_ |
1766217169467604992 |