Changes in labile soil organic carbon fractions in wetland ecosystems along a latitudinal gradient in Northeast China

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• 作者：Jiaoyue Wang^a ; ^b ; Changchun Song^a ; ^{songcc@neigae.ac.cn} ; Xianwei Wang^a ; Yanyu Song^a
• 关键词：SOC ; soil organic carbon ; LFOC ; light fraction organic carbon ; POC ; particulate organic carbon ; MBC ; microbial biomass carbon ; DOC ; dissolved organic carbon ; LF ; light fraction ; POM ; particulate organic matter ; WS ; whole soil ; CPF ; Ass. Ledum palustre&nda
• 刊名：Catena
• 出版年：2012
• 期刊代码：11_03418162
• 类别：ear
• 出版时间：September, 2012
• 卷：96
• 期：Complete
• 页码：83-89
• 文件大小：498 K

摘要

Wetlands in mid-high latitude regions play a vital role in climate change, due to their high organic carbon density. Nonetheless, the stabilization of soil organic carbon (SOC) and its fractions in these regions is largely unknown. The objectives of this study were to examine the changes in SOC and its fractions along a latitudinal gradient and to analyze the influencing factors in the southern margin of the permafrost region on the Eurasian continent. Topsoil (0-20 cm) was collected from five wetlands along a latitudinal gradient in Northeast China. We analyzed SOC and some labile fractions. Our results demonstrated that wetland SOC and its labile fractions concentration declined with decreasing latitude. The Permafrost regions had greater organic carbon content than the regions with seasonally frozen ground. The light fraction organic carbon and particulate organic carbon accounted for 5-83%and 21-32%, respectively, of the SOC and were particularly enriched in the permafrost region. Microbial biomass carbon and dissolved organic carbon showed a similar decreasing trend to that of SOC. At the same latitude, vegetation affected SOC stock and the dynamics of its labile fractions. Therefore, wetlands in mid-high latitudes contain a large carbon pool, and carbon stock varies with latitude. Although the labile fractions were higher in the permafrost region, their activities were lower, due to low temperature and poor nutrient status. Under global warming, the labile carbon pool may be mobilized and contribute to the greenhouse effect. Moreover, vegetation differences should be considered in obtaining an accurate carbon calculation.