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231226s2022 xx |||||o 00| ||eng c |
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|a 10.1111/gcb.16286
|2 doi
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|a pubmed24n1139.xml
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|a (DE-627)NLM341746703
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|a (NLM)35652687
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|a DE-627
|b ger
|c DE-627
|e rakwb
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|a eng
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| 100 |
1 |
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|a He, Yue
|e verfasserin
|4 aut
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| 245 |
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|a Observation-based global soil heterotrophic respiration indicates underestimated turnover and sequestration of soil carbon by terrestrial ecosystem models
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|c 2022
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|a Text
|b txt
|2 rdacontent
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|a ƒaComputermedien
|b c
|2 rdamedia
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|a ƒa Online-Ressource
|b cr
|2 rdacarrier
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|a Date Completed 16.08.2022
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|a Date Revised 26.09.2022
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|a published: Print-Electronic
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|a Citation Status MEDLINE
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|a © 2022 John Wiley & Sons Ltd.
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|a Soil heterotrophic respiration (Rh ) refers to the flux of CO2 released from soil to atmosphere as a result of organic matter decomposition by soil microbes and fauna. As one of the major fluxes in the global carbon cycle, large uncertainties still exist in the estimation of global Rh , which further limits our current understanding of carbon accumulation in soils. Here, we applied a Random Forest algorithm to create a global data set of soil Rh , by linking 761 field observations with both abiotic and biotic predictors. We estimated that global Rh was 48.8 ± 0.9 Pg C year-1 for 1982-2018, which was 16% less than the ensemble mean (58.6 ± 9.9 Pg C year-1 ) of 16 terrestrial ecosystem models. By integrating our observational Rh with independent soil carbon stock data sets, we obtained a global mean soil carbon turnover time of 38.3 ± 11 year. Using observation-based turnover times as a constraint, we found that terrestrial ecosystem models simulated faster carbon turnovers, leading to a 30% (74 Pg C) underestimation of terrestrial ecosystem carbon accumulation for the past century, which was especially pronounced at high latitudes. This underestimation is equivalent to 45% of the total carbon emissions (164 Pg C) caused by global land-use change at the same time. Our analyses highlight the need to constrain ecosystem models using observation-based and locally adapted Rh values to obtain reliable projections of the carbon sink capacity of terrestrial ecosystems
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4 |
|a Journal Article
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4 |
|a carbon cycling
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| 650 |
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4 |
|a carbon turnover time
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| 650 |
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4 |
|a random forest
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| 650 |
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|a soil heterotrophic respiration
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| 650 |
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4 |
|a terrestrial carbon sink
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| 650 |
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4 |
|a terrestrial ecosystem models
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| 650 |
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|a Soil
|2 NLM
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| 650 |
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|a Carbon Dioxide
|2 NLM
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| 650 |
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7 |
|a 142M471B3J
|2 NLM
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| 650 |
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|a Carbon
|2 NLM
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| 650 |
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7 |
|a 7440-44-0
|2 NLM
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| 700 |
1 |
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|a Ding, Jinzhi
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Dorji, Tsechoe
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Wang, Tao
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Li, Juan
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Smith, Pete
|e verfasserin
|4 aut
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| 773 |
0 |
8 |
|i Enthalten in
|t Global change biology
|d 1999
|g 28(2022), 18 vom: 14. Sept., Seite 5547-5559
|w (DE-627)NLM098239996
|x 1365-2486
|7 nnns
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| 773 |
1 |
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|g volume:28
|g year:2022
|g number:18
|g day:14
|g month:09
|g pages:5547-5559
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|u http://dx.doi.org/10.1111/gcb.16286
|3 Volltext
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|h 5547-5559
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