2007
DOI: 10.1007/s11104-007-9361-y
|View full text |Cite
|
Sign up to set email alerts
|

Effects of elevated atmospheric CO2 and tropospheric O3 on nutrient dynamics: decomposition of leaf litter in trembling aspen and paper birch communities

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

2
18
0

Year Published

2009
2009
2018
2018

Publication Types

Select...
4
3
1

Relationship

1
7

Authors

Journals

citations
Cited by 24 publications
(20 citation statements)
references
References 61 publications
2
18
0
Order By: Relevance
“…However, there was a modest overall O 3 effect and elevated CO 2 did significantly reduce N conc for aspen in the mixed-species communities. These results are not surprising given similarly mixed findings in previous N conc measurements at Rhinelander FACE for CO 2 and O 3 effects in green foliage (Kopper and others 2001;Takeuchi and others 2001;Zak and others 2007) and leaf litter (Liu andothers 2007, Parsons andothers 2008). More consistent at Rhinelander FACE is the finding that N mass has been increased by elevated CO 2 and decreased by elevated O 3 (this study, Liu and others 2007;Zak and others 2007 A stimulation of N uptake by elevated CO 2 at Rhinelander FACE has also been observed for roots, stems, and branches (Zak and others 2007).…”
Section: Canopy Nitrogen Cyclingsupporting
confidence: 70%
“…However, there was a modest overall O 3 effect and elevated CO 2 did significantly reduce N conc for aspen in the mixed-species communities. These results are not surprising given similarly mixed findings in previous N conc measurements at Rhinelander FACE for CO 2 and O 3 effects in green foliage (Kopper and others 2001;Takeuchi and others 2001;Zak and others 2007) and leaf litter (Liu andothers 2007, Parsons andothers 2008). More consistent at Rhinelander FACE is the finding that N mass has been increased by elevated CO 2 and decreased by elevated O 3 (this study, Liu and others 2007;Zak and others 2007 A stimulation of N uptake by elevated CO 2 at Rhinelander FACE has also been observed for roots, stems, and branches (Zak and others 2007).…”
Section: Canopy Nitrogen Cyclingsupporting
confidence: 70%
“…Although too early for definitive conclusions, the developing scientific consensus is that atmospheric CO 2 and O 3 will affect litter decomposition and subsequent nutrient cycling more through their effects on the quantity, than quality, of foliage produced, and by shifting the species composition of forests (Finzi and Schlesinger 2002;Cotrufo et al 2005b;Liu et al 2007Liu et al , 2009Hillstrom, Meehan, Kelly and Lindroth, unpublished data). For example, soil carbon sequestration at Aspen FACE appears to be more closely related to CO 2 -and O 3 -mediated changes in input quantity and species composition than to qualitative changes in litter chemical composition (Loya et al 2003;Liu et al 2007Liu et al , 2009.…”
Section: Litter Decompositionmentioning
confidence: 99%
“…On the other hand, litter chemistry was not affected by short-term O 3 exposure in a study with beech Fagus sylvatica (Schloter et al 2005). In free air type O 3 exposure experiments, it has been demonstrated that O 3 -induced changes in litter quality of Populus tremuloides and Betula papyrifera communities led to reduced inputs of hemicellulose and lignin (Liu et al 2005;Meehan et al 2010) and thus caused a decrease in nutrient flux into soil (Liu et al 2007). In contrast, Stoelken et al (2010) detected additional nitrogen incorporation into the soil down to 30 cm resulting from an enhanced nitrogen mobilisation from leaf litter in an O 3 exposure experiment with Fagus sylvatica grown in lysimeters.…”
Section: Below-ground Effectsmentioning
confidence: 99%