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DOI10.1073/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
ISSN0027-8424
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
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
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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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