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DOI | 10.1073/pnas.1511705112 |
Ancient low-molecular-weight organic acids in permafrost fuel rapid carbon dioxide production upon thaw | |
Drake T.W.; Wickland K.P.; Spencer R.G.M.; McKnight D.M.; Striegl R.G. | |
发表日期 | 2015 |
ISSN | 0027-8424 |
起始页码 | 13946 |
结束页码 | 13951 |
卷号 | 112期号:45 |
英文摘要 | Northern permafrost soils store a vast reservoir of carbon, nearly twice that of the present atmosphere. Current and projected climate warming threatens widespread thaw of these frozen, organic carbon (OC)-rich soils. Upon thaw, mobilized permafrost OC in dissolved and particulate forms can enter streams and rivers, which are important processors of OC and conduits for carbon dioxide (CO2) to the atmosphere. Here, we demonstrate that ancient dissolved organic carbon (DOC) leached from 35,800 y B.P. permafrost soils is rapidly mineralized to CO2. During 200-h experiments in a novel high-Temporal-resolution bioreactor, DOC concentration decreased by an average of 53%, fueling a more than sevenfold increase in dissolved inorganic carbon (DIC) concentration. Eighty-seven percent of the DOC loss to microbial uptake was derived from the low-molecular-weight (LMW) organic acids acetate and butyrate. To our knowledge, our study is the first to directly quantify high CO2 production rates from permafrost-derived LMW DOC mineralization. The observed DOC loss rates are among the highest reported for permafrost carbon and demonstrate the potential importance of LMW DOC in driving the rapid metabolism of Pleistocene-Age permafrost carbon upon thawand the outgassing of CO2 to the atmosphere by soils and nearby inland waters. |
语种 | 英语 |
scopus关键词 | carbon dioxide; carboxylic acid; fuel; organic carbon; acid; carbon dioxide; organic compound; bacterial growth; biodegradability; biodegradation; climate change; Conference Paper; controlled study; fluorescence; leaching; microbial biomass; mineralization; molecular weight; permafrost; photochemistry; photooxidation; Pleistocene; priority journal; room temperature; soil; thawing; molecular weight; Acids; Carbon Dioxide; Molecular Weight; Organic Chemicals; Permafrost |
来源期刊 | Proceedings of the National Academy of Sciences of the United States of America
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/158979 |
作者单位 | Drake, T.W., National Research Program, US Geological Survey, Boulder, CO 80303, United States, Environmental Studies Program, University of Colorado, Boulder, CO 80302, United States, Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, United States; Wickland, K.P., National Research Program, US Geological Survey, Boulder, CO 80303, United States; Spencer, R.G.M., Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, United States; McKnight, D.M., Environmental Studies Program, University of Colorado, Boulder, CO 80302, United States, Department of Civil, Environmental and Architectural Engineering, University of Colorado, Boulder, CO, United States; Striegl, R.G., National Research Program, US Geological Survey, Boulder, CO 80303, United States |
推荐引用方式 GB/T 7714 | Drake T.W.,Wickland K.P.,Spencer R.G.M.,et al. Ancient low-molecular-weight organic acids in permafrost fuel rapid carbon dioxide production upon thaw[J],2015,112(45). |
APA | Drake T.W.,Wickland K.P.,Spencer R.G.M.,McKnight D.M.,&Striegl R.G..(2015).Ancient low-molecular-weight organic acids in permafrost fuel rapid carbon dioxide production upon thaw.Proceedings of the National Academy of Sciences of the United States of America,112(45). |
MLA | Drake T.W.,et al."Ancient low-molecular-weight organic acids in permafrost fuel rapid carbon dioxide production upon thaw".Proceedings of the National Academy of Sciences of the United States of America 112.45(2015). |
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