Characteristics of peat humification, magnetic susceptibility and trace elements of Hani peatland, northeastern China: paleoclimatic implications
Abstract A high‐resolution peat humification record is obtained from Hani peatland, northeastern China to study climate change. An absorbance value time series from alkali‐extraction is used as a peat humification indicator. In addition, Hani peat magnetic susceptibility and trace elements have also...
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crwiley:10.1002/asl.736 2024-06-02T08:11:32+00:00 Characteristics of peat humification, magnetic susceptibility and trace elements of Hani peatland, northeastern China: paleoclimatic implications Xiao, He Cheng, Shenggao Mao, Xumei Huang, Ting Hu, Zhongxia Zhou, Ying Liu, Xiaotong National Natural Science Foundation of China 2017 http://dx.doi.org/10.1002/asl.736 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl.736 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.736 en eng Wiley http://creativecommons.org/licenses/by/4.0/ Atmospheric Science Letters volume 18, issue 3, page 140-150 ISSN 1530-261X 1530-261X journal-article 2017 crwiley https://doi.org/10.1002/asl.736 2024-05-06T07:03:51Z Abstract A high‐resolution peat humification record is obtained from Hani peatland, northeastern China to study climate change. An absorbance value time series from alkali‐extraction is used as a peat humification indicator. In addition, Hani peat magnetic susceptibility and trace elements have also been investigated. There is a sensitive response to abrupt climate changes when comparing a high‐resolution peat humification record with a Hani δ 18 O temperature proxy record and a drift ice record from the North Atlantic Ocean. Based on analyses of factors that affect peat decomposition, we suggest similar paleoclimate significance between the Hani and Dajiuhu peat on the degree of humification with a higher peat humification indicating colder and drier climate conditions. In contrast, a warm and moist climate provides a deoxidized condition that results in lower peat humification. Moreover, the Rb/Sr ratios and χ lf in Hani peatland also indicate different climate conditions, especially in late Holocene. According to the Hani peat data, regional paleoclimate variations can be divided into the following five phases: 11.5–10.0 cal. kyr BP with warm climate conditions; 10.0–8.8 cal. kyr BP with sharply cooling and warming climate conditions; 8.8–4.8 cal. kyr BP with alternating cooling and warming climate conditions; 4.8–1.6 cal. kyr BP with warm climate conditions overall and 1.6–0 cal. kyr BP with cold climate conditions. Article in Journal/Newspaper North Atlantic Wiley Online Library Hani ENVELOPE(-20.331,-20.331,63.441,63.441) Atmospheric Science Letters 18 3 140 150 |
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Wiley Online Library |
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language |
English |
description |
Abstract A high‐resolution peat humification record is obtained from Hani peatland, northeastern China to study climate change. An absorbance value time series from alkali‐extraction is used as a peat humification indicator. In addition, Hani peat magnetic susceptibility and trace elements have also been investigated. There is a sensitive response to abrupt climate changes when comparing a high‐resolution peat humification record with a Hani δ 18 O temperature proxy record and a drift ice record from the North Atlantic Ocean. Based on analyses of factors that affect peat decomposition, we suggest similar paleoclimate significance between the Hani and Dajiuhu peat on the degree of humification with a higher peat humification indicating colder and drier climate conditions. In contrast, a warm and moist climate provides a deoxidized condition that results in lower peat humification. Moreover, the Rb/Sr ratios and χ lf in Hani peatland also indicate different climate conditions, especially in late Holocene. According to the Hani peat data, regional paleoclimate variations can be divided into the following five phases: 11.5–10.0 cal. kyr BP with warm climate conditions; 10.0–8.8 cal. kyr BP with sharply cooling and warming climate conditions; 8.8–4.8 cal. kyr BP with alternating cooling and warming climate conditions; 4.8–1.6 cal. kyr BP with warm climate conditions overall and 1.6–0 cal. kyr BP with cold climate conditions. |
author2 |
National Natural Science Foundation of China |
format |
Article in Journal/Newspaper |
author |
Xiao, He Cheng, Shenggao Mao, Xumei Huang, Ting Hu, Zhongxia Zhou, Ying Liu, Xiaotong |
spellingShingle |
Xiao, He Cheng, Shenggao Mao, Xumei Huang, Ting Hu, Zhongxia Zhou, Ying Liu, Xiaotong Characteristics of peat humification, magnetic susceptibility and trace elements of Hani peatland, northeastern China: paleoclimatic implications |
author_facet |
Xiao, He Cheng, Shenggao Mao, Xumei Huang, Ting Hu, Zhongxia Zhou, Ying Liu, Xiaotong |
author_sort |
Xiao, He |
title |
Characteristics of peat humification, magnetic susceptibility and trace elements of Hani peatland, northeastern China: paleoclimatic implications |
title_short |
Characteristics of peat humification, magnetic susceptibility and trace elements of Hani peatland, northeastern China: paleoclimatic implications |
title_full |
Characteristics of peat humification, magnetic susceptibility and trace elements of Hani peatland, northeastern China: paleoclimatic implications |
title_fullStr |
Characteristics of peat humification, magnetic susceptibility and trace elements of Hani peatland, northeastern China: paleoclimatic implications |
title_full_unstemmed |
Characteristics of peat humification, magnetic susceptibility and trace elements of Hani peatland, northeastern China: paleoclimatic implications |
title_sort |
characteristics of peat humification, magnetic susceptibility and trace elements of hani peatland, northeastern china: paleoclimatic implications |
publisher |
Wiley |
publishDate |
2017 |
url |
http://dx.doi.org/10.1002/asl.736 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl.736 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.736 |
long_lat |
ENVELOPE(-20.331,-20.331,63.441,63.441) |
geographic |
Hani |
geographic_facet |
Hani |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Atmospheric Science Letters volume 18, issue 3, page 140-150 ISSN 1530-261X 1530-261X |
op_rights |
http://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1002/asl.736 |
container_title |
Atmospheric Science Letters |
container_volume |
18 |
container_issue |
3 |
container_start_page |
140 |
op_container_end_page |
150 |
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1800757702093176832 |