Holocene periglacial processes and environmental changes in Daqingshan mountains, inner Mongolia, China
Abstract Periglacial phenomena and palaeobotany evidence of environmental changes are present in the Daqingshan area, northern China. This arid‐semiarid area is sensitive to climatic change. There were four climatic periods during the Holocene. During the Hypsithermal, the annual mean temperature wa...
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crwiley:10.1002/ppp.3430030108 2024-06-02T08:13:10+00:00 Holocene periglacial processes and environmental changes in Daqingshan mountains, inner Mongolia, China Zhijiu, Cut Changqing, Song 1992 http://dx.doi.org/10.1002/ppp.3430030108 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030108 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030108 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 3, issue 1, page 55-62 ISSN 1045-6740 1099-1530 journal-article 1992 crwiley https://doi.org/10.1002/ppp.3430030108 2024-05-03T11:12:50Z Abstract Periglacial phenomena and palaeobotany evidence of environmental changes are present in the Daqingshan area, northern China. This arid‐semiarid area is sensitive to climatic change. There were four climatic periods during the Holocene. During the Hypsithermal, the annual mean temperature was 1–2 °C higher than today. On the other hand, the annual mean temperature was 2.0–2.5 °C lower during recent glaciation and about 7 °C lower at the end of the Late Pleistocene. The fluctuation of vertical vegetation belts was about 200–600 m during the Holocene. Des phénomènes périglaciaires et des observations paléobotaniques démontrent l'existence de changements de l'environnement dans la région de Daqingshan, au nord de la Chine. Cette région aride ou semi‐aride est très sensible aux changements climatiques. Quatre périodes climatiques ont été reconnues pendant l'Holocène. Pendant l'Hypsithermal, la température moyenne annuelle était 1 á 2 °C plus élevée qu'aujourd'hui. D'autre part, la température moyenne annuelle était 2,0 a 2,5 °C plus basse pendant la glaciation récente et environ 7 °C plus élevée à la fin du Pléistocène. Les modifications des limites verticales de la végétation pendant l'Holocène ont été comprises approximativement entre 200 et 600 m. Article in Journal/Newspaper Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 3 1 55 62 |
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English |
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Abstract Periglacial phenomena and palaeobotany evidence of environmental changes are present in the Daqingshan area, northern China. This arid‐semiarid area is sensitive to climatic change. There were four climatic periods during the Holocene. During the Hypsithermal, the annual mean temperature was 1–2 °C higher than today. On the other hand, the annual mean temperature was 2.0–2.5 °C lower during recent glaciation and about 7 °C lower at the end of the Late Pleistocene. The fluctuation of vertical vegetation belts was about 200–600 m during the Holocene. Des phénomènes périglaciaires et des observations paléobotaniques démontrent l'existence de changements de l'environnement dans la région de Daqingshan, au nord de la Chine. Cette région aride ou semi‐aride est très sensible aux changements climatiques. Quatre périodes climatiques ont été reconnues pendant l'Holocène. Pendant l'Hypsithermal, la température moyenne annuelle était 1 á 2 °C plus élevée qu'aujourd'hui. D'autre part, la température moyenne annuelle était 2,0 a 2,5 °C plus basse pendant la glaciation récente et environ 7 °C plus élevée à la fin du Pléistocène. Les modifications des limites verticales de la végétation pendant l'Holocène ont été comprises approximativement entre 200 et 600 m. |
format |
Article in Journal/Newspaper |
author |
Zhijiu, Cut Changqing, Song |
spellingShingle |
Zhijiu, Cut Changqing, Song Holocene periglacial processes and environmental changes in Daqingshan mountains, inner Mongolia, China |
author_facet |
Zhijiu, Cut Changqing, Song |
author_sort |
Zhijiu, Cut |
title |
Holocene periglacial processes and environmental changes in Daqingshan mountains, inner Mongolia, China |
title_short |
Holocene periglacial processes and environmental changes in Daqingshan mountains, inner Mongolia, China |
title_full |
Holocene periglacial processes and environmental changes in Daqingshan mountains, inner Mongolia, China |
title_fullStr |
Holocene periglacial processes and environmental changes in Daqingshan mountains, inner Mongolia, China |
title_full_unstemmed |
Holocene periglacial processes and environmental changes in Daqingshan mountains, inner Mongolia, China |
title_sort |
holocene periglacial processes and environmental changes in daqingshan mountains, inner mongolia, china |
publisher |
Wiley |
publishDate |
1992 |
url |
http://dx.doi.org/10.1002/ppp.3430030108 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430030108 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430030108 |
genre |
Permafrost and Periglacial Processes |
genre_facet |
Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 3, issue 1, page 55-62 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.3430030108 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
3 |
container_issue |
1 |
container_start_page |
55 |
op_container_end_page |
62 |
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1800736568412995584 |