Similar response of labile and resistant soil organic matter pools to changes in temperature. [Erratum: 2005 Aug. 11, v. 436, no. 7052, p. 881.]
Our understanding of the relationship between the decomposition of soil organic matter (SOM) and soil temperature affects our predictions of the impact of climate change on soil-stored carbon. One current opinion is that the decomposition of soil labile carbon is sensitive to temperature variation w...
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| Published in | Nature (London) Vol. 433; no. 7021; pp. 57 - 59 |
|---|---|
| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
| Published |
London
Nature Publishing Group UK
06.01.2005
Nature Publishing Nature Publishing Group |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Our understanding of the relationship between the decomposition of soil organic matter (SOM) and soil temperature affects our predictions of the impact of climate change on soil-stored carbon. One current opinion is that the decomposition of soil labile carbon is sensitive to temperature variation whereas resistant components are insensitive. The resistant carbon or organic matter in mineral soil is then assumed to be unresponsive to global warming. But the global pattern and magnitude of the predicted future soil carbon stock will mainly rely on the temperature sensitivity of these resistant carbon pools. To investigate this sensitivity, we have incubated soils under changing temperature. Here we report that SOM decomposition or soil basal respiration rate was significantly affected by changes in SOM components associated with soil depth, sampling method and incubation time. We find, however, that the temperature sensitivity for SOM decomposition was not affected, suggesting that the temperature sensitivity for resistant organic matter pools does not differ significantly from that of labile pools, and that both types of SOM will therefore respond similarly to global warming. |
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| AbstractList | Our understanding of the relationship between the decomposition of soil organic matter (SOM) and soil temperature affects our predictions of the impact of climate change on soil-stored carbon. One current opinion is that the decomposition of soil labile carbon is sensitive to temperature variation whereas resistant components are insensitive. The resistant carbon or organic matter in mineral soil is then assumed to be unresponsive to global warming. But the global pattern and magnitude of the predicted future soil carbon stock will mainly rely on the temperature sensitivity of these resistant carbon pools. To investigate this sensitivity, we have incubated soils under changing temperature. Here we report that SOM decomposition or soil basal respiration rate was significantly affected by changes in SOM components associated with soil depth, sampling method and incubation time. We find, however, that the temperature sensitivity for SOM decomposition was not affected, suggesting that the temperature sensitivity for resistant organic matter pools does not differ significantly from that of labile pools, and that both types of SOM will therefore respond similarly to global warming. Our understanding of the relationship between the decomposition of soil organic matter (SOM) and soil temperature affects our predictions of the impact of climate change on soil-stored carbon. One current opinion is that the decomposition of soil labile carbon is sensitive to temperature variation whereas resistant components are insensitive. The resistant carbon or organic matter in mineral soil is then assumed to be unresponsive to global warming. But the global pattern and magnitude of the predicted future soil carbon stock will mainly rely on the temperature sensitivity of these resistant carbon pools. To investigate this sensitivity, we have incubated soils under changing temperature. Here we report that SOM decomposition or soil basal respiration rate was significantly affected by changes in SOM components associated with soil depth, sampling method and incubation time. We find, however, that the temperature sensitivity for SOM decomposition was not affected, suggesting that the temperature sensitivity for resistant organic matter pools does not differ significantly from that of labile pools, and that both types of SOM will therefore respond similarly to global warming. [PUBLICATION ABSTRACT] Our understanding of the relationship between the decomposition of soil organic matter (SOM) and soil temperature affects our predictions of the impact of climate change on soil-stored carbon. One current opinion is that the decomposition of soil labile carbon is sensitive to temperature variation whereas resistant components are insensitive. The resistant carbon or organic matter in mineral soil is then assumed to be unresponsive to global warming. But the global pattern and magnitude of the predicted future soil carbon stock will mainly rely on the temperature sensitivity of these resistant carbon pools. To investigate this sensitivity, we have incubated soils under changing temperature. Here we report that SOM decomposition or soil basal respiration rate was significantly affected by changes in SOM components associated with soil depth, sampling method and incubation time. We find, however, that the temperature sensitivity for SOM decomposition was not affected, suggesting that the temperature sensitivity for resistant organic matter pools does not differ significantly from that of labile pools, and that both types of SOM will therefore respond similarly to global warming.Our understanding of the relationship between the decomposition of soil organic matter (SOM) and soil temperature affects our predictions of the impact of climate change on soil-stored carbon. One current opinion is that the decomposition of soil labile carbon is sensitive to temperature variation whereas resistant components are insensitive. The resistant carbon or organic matter in mineral soil is then assumed to be unresponsive to global warming. But the global pattern and magnitude of the predicted future soil carbon stock will mainly rely on the temperature sensitivity of these resistant carbon pools. To investigate this sensitivity, we have incubated soils under changing temperature. Here we report that SOM decomposition or soil basal respiration rate was significantly affected by changes in SOM components associated with soil depth, sampling method and incubation time. We find, however, that the temperature sensitivity for SOM decomposition was not affected, suggesting that the temperature sensitivity for resistant organic matter pools does not differ significantly from that of labile pools, and that both types of SOM will therefore respond similarly to global warming. Soil carbon: all for one The effect of temperature change on decomposition of soil organic matter is an important factor when considering the effect of global warming on soil-stored carbon. It is commonly assumed that soil carbon exists as two fractions, a ‘labile’ fraction sensitive to temperature variation and a ‘resistant’ fraction insensitive to temperature. This implies that higher losses of carbon would occur from soils in forest and tundra, which have the largest store of labile organic matter, and that the effect of warming on soil organic matter decomposition may decline with time. Not so, according to an experiment on samples of forest soil. The temperature sensitivity of decomposition was not affected by soil organic matter composition, suggesting that all soil organic matter will respond similarly to global warming. Our understanding of the relationship between the decomposition of soil organic matter (SOM) and soil temperature affects our predictions of the impact of climate change on soil-stored carbon 1 . One current opinion is that the decomposition of soil labile carbon is sensitive to temperature variation whereas resistant components are insensitive 2 , 3 , 4 . The resistant carbon or organic matter in mineral soil is then assumed to be unresponsive to global warming 2 , 4 . But the global pattern and magnitude of the predicted future soil carbon stock will mainly rely on the temperature sensitivity of these resistant carbon pools. To investigate this sensitivity, we have incubated soils under changing temperature. Here we report that SOM decomposition or soil basal respiration rate was significantly affected by changes in SOM components associated with soil depth, sampling method and incubation time. We find, however, that the temperature sensitivity for SOM decomposition was not affected, suggesting that the temperature sensitivity for resistant organic matter pools does not differ significantly from that of labile pools, and that both types of SOM will therefore respond similarly to global warming. |
| Audience | Academic |
| Author | Smith, P Fang, C Moncrieff, J.B Smith, J.U |
| Author_xml | – sequence: 1 fullname: Fang, C – sequence: 2 fullname: Smith, P – sequence: 3 fullname: Moncrieff, J.B – sequence: 4 fullname: Smith, J.U |
| BackLink | http://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=16427500$$DView record in Pascal Francis https://www.ncbi.nlm.nih.gov/pubmed/15635408$$D View this record in MEDLINE/PubMed |
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| Issue | 7021 |
| Keywords | Climatology Organic carbon Organic matter Property composition relationship Cultivated soil Chemical stability resistant pool Temperature effect labile pool Ecology Decomposition Forest soil Mineral soils Earth science Experimental study Chemical instability Carbon cycle Biogeochemistry Arable land Global change Pool Climate modification Grassland soil |
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| References | K Coleman (BFnature03138_CR23) 1996 RD Lovell (BFnature03138_CR19) 1998; 30 NW MacDonald (BFnature03138_CR15) 1995; 59 B Grisi (BFnature03138_CR21) 1998; 30 WH Schlesinger (BFnature03138_CR7) 2000; 48 DJ Ross (BFnature03138_CR16) 1994; 25 J Liski (BFnature03138_CR2) 1999; 28 WT Peterjohn (BFnature03138_CR10) 1993; 93 A Lomander (BFnature03138_CR20) 1998; 30 EG Jobbágy (BFnature03138_CR8) 2000; 10 WT Peterjohn (BFnature03138_CR11) 1994; 4 M Reichstein (BFnature03138_CR17) 2000; 32 CP Giardina (BFnature03138_CR4) 2000; 404 C Fang (BFnature03138_CR5) 2001; 33 P Dalias (BFnature03138_CR12) 2001; 6 LE Rustad (BFnature03138_CR9) 2001; 126 SE Allen (BFnature03138_CR24) 1974 JHM Thornley (BFnature03138_CR3) 2001; 87 IPCC (BFnature03138_CR22) 2000 SE Trumbore (BFnature03138_CR13) 1996; 272 P Martin-Olmedo (BFnature03138_CR25) 1999; 29 N Fierer (BFnature03138_CR18) 2003; 9 R Öhlinger (BFnature03138_CR26) 1995 TM Lenton (BFnature03138_CR1) 2003; 9 BFnature03138_CR6 JP Winkler (BFnature03138_CR14) 1996; 28 Nature. 2005 Aug 11:436(7052):881 |
| References_xml | – volume: 30 start-page: 2077 year: 1998 ident: BFnature03138_CR19 publication-title: Soil Biol. Biochem. doi: 10.1016/S0038-0717(98)00084-4 – volume: 32 start-page: 947 year: 2000 ident: BFnature03138_CR17 publication-title: Soil Biol. Biochem. doi: 10.1016/S0038-0717(00)00002-X – volume: 28 start-page: 171 year: 1999 ident: BFnature03138_CR2 publication-title: Ambio – volume: 48 start-page: 7 year: 2000 ident: BFnature03138_CR7 publication-title: Biogeochemistry doi: 10.1023/A:1006247623877 – volume: 25 start-page: 477 year: 1994 ident: BFnature03138_CR16 publication-title: Soil Biol. Biochem. doi: 10.1016/0038-0717(93)90073-K – volume: 9 start-page: 1322 year: 2003 ident: BFnature03138_CR18 publication-title: Glob. Change Biol. doi: 10.1046/j.1365-2486.2003.00663.x – volume: 30 start-page: 2017 year: 1998 ident: BFnature03138_CR20 publication-title: Soil Biol. Biochem. doi: 10.1016/S0038-0717(98)00076-5 – volume: 93 start-page: 18 year: 1993 ident: BFnature03138_CR10 publication-title: Oecologia doi: 10.1007/BF00321185 – ident: BFnature03138_CR6 doi: 10.1029/2001GB001833 – volume: 87 start-page: 591 year: 2001 ident: BFnature03138_CR3 publication-title: Ann. Bot. doi: 10.1006/anbo.2001.1372 – start-page: 137 volume-title: Chemical Analysis of Ecological Materials year: 1974 ident: BFnature03138_CR24 – volume: 4 start-page: 617 year: 1994 ident: BFnature03138_CR11 publication-title: Ecol. Appl. doi: 10.2307/1941962 – volume: 59 start-page: 233 year: 1995 ident: BFnature03138_CR15 publication-title: Soil Sci. Soc. Am. J. doi: 10.2136/sssaj1995.03615995005900010036x – volume: 28 start-page: 1067 year: 1996 ident: BFnature03138_CR14 publication-title: Soil Biol. Biochem. doi: 10.1016/0038-0717(96)00076-4 – start-page: 237 volume-title: Evaluation of Soil Organic Matter Models Using Existing Long-Term Datasets year: 1996 ident: BFnature03138_CR23 doi: 10.1007/978-3-642-61094-3_17 – volume: 6 start-page: 181 year: 2001 ident: BFnature03138_CR12 publication-title: Glob. Change Biol. doi: 10.1046/j.1365-2486.2001.00386.x – volume: 126 start-page: 543 year: 2001 ident: BFnature03138_CR9 publication-title: Oecologia doi: 10.1007/s004420000544 – start-page: 56 volume-title: Methods in Soil Biology year: 1995 ident: BFnature03138_CR26 – volume: 30 start-page: 1309 year: 1998 ident: BFnature03138_CR21 publication-title: Soil Biol. Biochem. doi: 10.1016/S0038-0717(98)00016-9 – volume: 404 start-page: 858 year: 2000 ident: BFnature03138_CR4 publication-title: Nature doi: 10.1038/35009076 – volume: 272 start-page: 393 year: 1996 ident: BFnature03138_CR13 publication-title: Science doi: 10.1126/science.272.5260.393 – volume: 9 start-page: 1333 year: 2003 ident: BFnature03138_CR1 publication-title: Glob. Change Biol. doi: 10.1046/j.1365-2486.2003.00674.x – volume: 10 start-page: 423 year: 2000 ident: BFnature03138_CR8 publication-title: Ecol. Appl. doi: 10.1890/1051-0761(2000)010[0423:TVDOSO]2.0.CO;2 – volume-title: Special Report on Emissions Scenarios year: 2000 ident: BFnature03138_CR22 – volume: 29 start-page: 386 year: 1999 ident: BFnature03138_CR25 publication-title: Biol. Fert. Soils doi: 10.1007/s003740050569 – volume: 33 start-page: 155 year: 2001 ident: BFnature03138_CR5 publication-title: Soil Biol. Biochem. doi: 10.1016/S0038-0717(00)00125-5 – reference: - Nature. 2005 Aug 11:436(7052):881 |
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| Snippet | Our understanding of the relationship between the decomposition of soil organic matter (SOM) and soil temperature affects our predictions of the impact of... Soil carbon: all for one The effect of temperature change on decomposition of soil organic matter is an important factor when considering the effect of global... |
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| SubjectTerms | Agricultural and forest climatology and meteorology. Irrigation. Drainage Agricultural and forest meteorology Agronomy. Soil science and plant productions Animal and plant ecology Animal, plant and microbial ecology biodegradation Biodegradation, Environmental biological activity in soil Biological and medical sciences Carbon Carbon - metabolism Cell Respiration Chemical, physicochemical, biochemical and biological properties Climate Climate change Climatology, meteorology Decomposition Environmental impact Fundamental and applied biological sciences. Psychology General agronomy. Plant production Generalities. Techniques. Climatology. Meteorology. Climatic models of plant production Global warming Greenhouse Effect Humanities and Social Sciences letter multidisciplinary Organic Chemicals - metabolism Organic matter Physics, chemistry, biochemistry and biology of agricultural and forest soils Picea - physiology Poaceae - physiology Science Science (multidisciplinary) Scotland Soil - analysis Soil depth Soil Microbiology soil microorganisms Soil organic matter soil respiration Soil science Soil temperature Soils Synecology Temperature Temperature effects Terrestrial ecosystems Time Factors Trees - physiology |
| Title | Similar response of labile and resistant soil organic matter pools to changes in temperature. [Erratum: 2005 Aug. 11, v. 436, no. 7052, p. 881.] |
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