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231224s2016 xx |||||o 00| ||eng c |
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|a 10.1111/gcb.13188
|2 doi
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|a pubmed24n0851.xml
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|a (DE-627)NLM255563426
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|a (NLM)26667780
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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 |
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|a Yang, Jinyan
|e verfasserin
|4 aut
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| 245 |
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|a Global patterns and predictors of stem CO2 efflux in forest ecosystems
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|c 2016
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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 13.12.2016
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|a Date Revised 30.12.2016
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|a published: Print
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|a Citation Status MEDLINE
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|a © 2015 John Wiley & Sons Ltd.
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|a Stem CO2 efflux (ES) plays an important role in the carbon balance of forest ecosystems. However, its primary controls at the global scale are poorly understood and observation-based global estimates are lacking. We synthesized data from 121 published studies across global forest ecosystems and examined the relationships between annual ES and biotic and abiotic factors at individual, biome, and global scales, and developed a global gridded estimate of annual ES . We tested the following hypotheses: (1) Leaf area index (LAI) will be highly correlated with annual ES at biome and global scales; (2) there will be parallel patterns in stem and root CO2 effluxes (RA) in all forests; (3) annual ES will decline with forest age; and (4) LAI coupled with mean annual temperature (MAT) and mean annual precipitation (MAP) will be sufficient to predict annual ES across forests in different regions. Positive linear relationships were found between ES and LAI, as well as gross primary production (GPP), net primary production (NPP), wood NPP, soil CO2 efflux (RS), and RA . Annual ES was correlated with RA in temperate forests after controlling for GPP and MAT, suggesting other additional factors contributed to the relationship. Annual ES tended to decrease with stand age. Leaf area index, MAT and MAP, predicted 74% of variation in ES at global scales. Our statistical model estimated a global annual ES of 6.7 ± 1.1 Pg C yr(-1) over the period of 2000-2012 with little interannual variability. Modeled mean annual ES was 71 ± 43, 270 ± 103, and 420 ± 134 g C m(2) yr(-1) for boreal, temperate, and tropical forests, respectively. We recommend that future studies report ES at a standardized constant temperature, incorporate more manipulative treatments, such as fertilization and drought, and whenever possible, simultaneously measure both aboveground and belowground CO2 fluxes
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|a Journal Article
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|a Research Support, U.S. Gov't, Non-P.H.S.
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|a gross primary production
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|a leaf area index
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|a respiration
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|a root CO2 efflux
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| 650 |
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|a stem CO2 efflux
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| 650 |
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|a Carbon Dioxide
|2 NLM
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| 650 |
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|a 142M471B3J
|2 NLM
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| 700 |
1 |
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|a He, Yujie
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Aubrey, Doug P
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Zhuang, Qianlai
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Teskey, Robert O
|e verfasserin
|4 aut
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| 773 |
0 |
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|i Enthalten in
|t Global change biology
|d 1999
|g 22(2016), 4 vom: 21. Apr., Seite 1433-44
|w (DE-627)NLM098239996
|x 1365-2486
|7 nnns
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| 773 |
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|g volume:22
|g year:2016
|g number:4
|g day:21
|g month:04
|g pages:1433-44
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|u http://dx.doi.org/10.1111/gcb.13188
|3 Volltext
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