Mire surface wetness is jointly determined by climate and geothermy: A case from Chichi peatland in the Changbai Mountains

L LIU, H ZHAO, H LI, Z BU, S WANG - Quaternary Sciences, 2023 - dsjyj.com.cn
Peatlands record the changes in climate and environment during their formation and
development as one of the major geological archives. Previous studies from boreal …

A multi-proxy record of surface wetness in Hani mire of west Changbaishan Mountain and its possible drivers

Z Hongyan, L Hongkai, H Yi, B Zhaojun… - Quaternary …, 2014 - dsjyj.com.cn
Abstract Hani mire (42 11'~ 42 14'N, 126 28'~ 126 33'E) is a 16.78 km2mesotrophic to
oligotrophic peatland and lies in west Changbaishan Mountain, Jilin Province, China. A …

Plant assemblages-based quantitative reconstruction of past mire surface wetness: A case study in the Changbai Mountains region, Northeast China

Q Yang, H Li, H Zhao, FM Chambers, Z Bu, E Bai, G Xu - Catena, 2022 - Elsevier
Quantitative relationships between mire plant assemblages and environmental variables
have been investigated widely in Europe and North America, but hitherto insufficiently …

Peat development in the Napahai wetland and its response to variations in the intensity of the Indian summer monsoon, southwestern China, since the last …

B Liu, E Sheng, J Lan, K Yu - Palaeogeography, Palaeoclimatology …, 2022 - Elsevier
Abstract Knowledge of peatland dynamics and its response to the intensity of the Indian
summer monsoon (ISM) is crucial to predict the future fate of the peatlands in the …

Humification degree of peat and its implications for Holocene climate change in Hani peatland, Northeast China

T Huang, S Cheng, X Mao, B Hong, Z Hu… - Chinese Journal of …, 2013 - Springer
The humification degree of peat is a significant climatic proxy for paleoclimate change.
Using the alkali-extraction method, a time series of absorbance values of the Hani peatland …

Response of humification degree to monsoon climate during the Holocene from the Hongyuan peat bog, eastern Tibetan Plateau

H Wang, Y Hong, Q Lin, B Hong, Y Zhu, Y Wang… - Palaeogeography …, 2010 - Elsevier
The humification degree of peat has been used to indicate climate variations in Europe, with
a dominant maritime climate. However, little research has been done so far in Asia, with a …

Hydroclimate controls of the distribution and abundance of mosses in Hani mire, Northeast China: Modern vegetation survey and peat-core analysis

QN Yang, HC Li, HY Zhao, HK Li, ZJ Bu, SZ Wang… - Quaternary …, 2019 - Elsevier
Located on the western flank of the Changbai Mountains in Northeast China, Hani (HN)
peatland has been studied intensively for Holocene paleoclimate reconstruction on decadal …

Holocene climate changes inferred from peat humification: A case study from the Daiyun Mountains, Southeast China

C Ma, L Wu, L Zhao, Y Zhang, Y Deng, Z Xu - Quaternary International, 2021 - Elsevier
The investigation of two profiles (DYS1 and DYS5) from the Daiyun Mountains in
southeastern China sheds new light on the history of regional climate changes and the …

Quantitative reconstruction of the water table changes during the last 2000 years from Laolike peatland, Changbai Mountains

Y Li, H Li, Y Dong - Quaternary Sciences, 2020 - dsjyj.com.cn
Water table is one of the key factors that controlling the peatland initiation and development,
and therefore has attracted a lot of attentions in the field of peatland paleoenvironment …

A 4000-yr multi-proxy record of Holocene hydrology and vegetation from a peatland in the Sanjiang Plain, Northeast China

H Liu, X Yu, C Gao, Z Zhang, C Wang, W Xing… - Quaternary …, 2017 - Elsevier
Reconstructing historical hydrologic and vegetation conditions can provide useful insights
into the mechanisms underlying peatland development and can be used to construct …