Knowledge Management System of Northwest Institute of Plateau Biology, CAS
The carbon stock of alpine peatlands on the Qinghai-Tibetan Plateau during the Holocene and their future fate | |
Chen, Huai1,2,3,4; Yang, Gang3,4; Peng, Changhui3,5; Zhang, Yao3; Zhu, Dan1,2,4; Zhu, Qiuan3,4; Hu, Ji3,4; Wang, Mei1,2,4; Zhan, Wei3,4; Zhu, Erxiong3,4; Bai, Zengzhi3; Li, Wei1,2,4; Wu, Ning1,2,4,6; Wang, Yanfen4,7; Gao, Yongheng4,8; Tian, Jianqing4,9; Kang, Xiaoming4,10; Zhao, Xinquan1,2,4,11; Wu, Jianghua4,12 | |
2014-07-01 | |
发表期刊 | QUATERNARY SCIENCE REVIEWS |
ISSN | 0277-3791 |
卷号 | 95页码:151-158 |
文章类型 | Article |
摘要 | Most studies about carbon dynamics of peatlands have been focused on boreal, subarctic and tropical peatlands. However, there is limited data about carbon dynamics of alpine peatlands, like Zoige peatlands on the Qinghai-Tibetan Plateau (QTP), which are sensitive to climate change and human disturbance. We studied the role of these peat deposits on the Zoige as a C reserve and sink by measuring peat depth, radiocarbon age and peat and C accumulation rates at 7 sites. The peat depths of the sample sites ranged from 0.20 to 6.0 m; the basal age on the plateau varied from 1635 to 14095 cal yr BP; the peat accumulation rates ranged from 0.12 to 0.85 mm yr(-1), and the C accumulation rates from 5 to 48 g m(-2) yr(-1). Based on data of field studies and remote sensing, we regarded that with 3179 km(2) of intact peatlands, about 1426 km(2) of degraded peatlands, and the total area of Zoige peatlands was 4605 km(2). The current peat C stock of Zoige peatlands was0.477 Pg (ranging from 0.206 to 0.672 Pg). We also estimated that peatlands covered an area of about 5091 krn(2)on the QTP and sequestered 0.543 Pg C, 88% in Zoige and the rest in other parts of the plateau. Human activities, together with the ubiquitous warming on the plateau (temperature increased by 0.2 degrees C per decade over the past 50 years) not only shrank the area of intact peatlands, but also caused substantial carbon releasing from peatlands. (C) 2014 Elsevier Ltd. All rights reserved.; Most studies about carbon dynamics of peatlands have been focused on boreal, subarctic and tropical peatlands. However, there is limited data about carbon dynamics of alpine peatlands, like Zoige peatlands on the Qinghai-Tibetan Plateau (QTP), which are sensitive to climate change and human disturbance. We studied the role of these peat deposits on the Zoige as a C reserve and sink by measuring peat depth, radiocarbon age and peat and C accumulation rates at 7 sites. The peat depths of the sample sites ranged from 0.20 to 6.0 m; the basal age on the plateau varied from 1635 to 14095 cal yr BP; the peat accumulation rates ranged from 0.12 to 0.85 mm yr(-1), and the C accumulation rates from 5 to 48 g m(-2) yr(-1). Based on data of field studies and remote sensing, we regarded that with 3179 km(2) of intact peatlands, about 1426 km(2) of degraded peatlands, and the total area of Zoige peatlands was 4605 km(2). The current peat C stock of Zoige peatlands was0.477 Pg (ranging from 0.206 to 0.672 Pg). We also estimated that peatlands covered an area of about 5091 krn(2)on the QTP and sequestered 0.543 Pg C, 88% in Zoige and the rest in other parts of the plateau. Human activities, together with the ubiquitous warming on the plateau (temperature increased by 0.2 degrees C per decade over the past 50 years) not only shrank the area of intact peatlands, but also caused substantial carbon releasing from peatlands. (C) 2014 Elsevier Ltd. All rights reserved. |
关键词 | The Third Pole Climate Change Wetlands Carbon Budget Holocene Anthropocene |
WOS标题词 | Science & Technology ; Physical Sciences |
关键词[WOS] | SOIL ORGANIC-CARBON ; NORTHERN PEATLAND ; CLIMATIC-CHANGE ; PALEOCLIMATE RECONSTRUCTION ; ACCUMULATION RATES ; GREENHOUSE GASES ; NATURAL WETLANDS ; EASTERN TIBET ; CHINA ; ZOIGE |
收录类别 | SCI |
语种 | 英语 |
WOS研究方向 | Physical Geography ; Geology |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:000338604200009 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://210.75.249.4/handle/363003/4216 |
专题 | 中国科学院西北高原生物研究所 |
作者单位 | 1.Chinese Acad Sci, Chengdu Inst Biol, Key Lab Mt Ecol Restorat & Bioresource Utilizat, Beijing 100864, Peoples R China 2.Chinese Acad Sci, Chengdu Inst Biol, Ecol Restorat Biodivers Conservat Key Lab Sichuan, Beijing 100864, Peoples R China 3.Northwest A&F Univ, Coll Forestry, State Key Lab Soil Eros & Thyland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China 4.Chinese Acad Sci, Zoige Peatland & Global Change Res Stn, Hongyuan 624400, Peoples R China 5.Univ Quebec Montreal, Dept Biol Sci, Ctr CEF ESCER, Montreal C3H 3P8, PQ, Canada 6.Int Ctr Integrated Mt Dev, Kathmandu, Nepal 7.Univ Chinese Acad Sci, Beijing 100039, Peoples R China 8.Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China 9.Chinese Acad Sci, Inst Microbiol, Beijing 100101, Peoples R China 10.Chinese Acad Forestry, Inst Wetland Res, Beijing 100091, Peoples R China 11.Chinese Acad Sci, Northwest Inst Plateau Biol, Xining 810008, Peoples R China 12.Mem Univ Newfoundland, Corner Brook, NF A2H 6P9, Canada |
推荐引用方式 GB/T 7714 | Chen, Huai,Yang, Gang,Peng, Changhui,et al. The carbon stock of alpine peatlands on the Qinghai-Tibetan Plateau during the Holocene and their future fate[J]. QUATERNARY SCIENCE REVIEWS,2014,95:151-158. |
APA | Chen, Huai.,Yang, Gang.,Peng, Changhui.,Zhang, Yao.,Zhu, Dan.,...&Wu, Jianghua.(2014).The carbon stock of alpine peatlands on the Qinghai-Tibetan Plateau during the Holocene and their future fate.QUATERNARY SCIENCE REVIEWS,95,151-158. |
MLA | Chen, Huai,et al."The carbon stock of alpine peatlands on the Qinghai-Tibetan Plateau during the Holocene and their future fate".QUATERNARY SCIENCE REVIEWS 95(2014):151-158. |
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