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Can differences in microbial abundances help explain enhanced N2O emissions in a permanent grassland under elevated atmospheric CO2?
- Source :
- Global Change Biology; Oct2011, Vol. 17 Issue 10, p3176-3186, 11p, 3 Charts, 7 Graphs
- Publication Year :
- 2011
-
Abstract
- Long-term effects of elevated atmospheric CO<subscript>2</subscript> on the ammonia-oxidizing and denitrifying bacteria in a grassland soil were investigated to test whether a shift in abundance of these N-cycling microorganisms was responsible for enhanced N<subscript>2</subscript>O emissions under elevated atmospheric CO<subscript>2</subscript>. Soil samples (7.5 cm increments to 45 cm depth) were collected in 2008 from the University of Giessen Free Air Carbon dioxide Enrichment ( GiFACE), a permanent grassland exposed to moderately elevated atmospheric CO<subscript>2</subscript> (+20%) since 1998. GiFACE plots lay on a soil moisture gradient because of gradually changing depth to the underlying water table and labeled as the DRY block (furthest from water table), MED block (intermediate to water table), and WET block (nearest to water table). Mean N<subscript>2</subscript>O emissions measured since 1998 have been significantly higher under elevated CO<subscript>2</subscript>. This study sought to identify microbial and biochemical parameters that might explain higher N<subscript>2</subscript>O emissions under elevated CO<subscript>2</subscript>. Soil biochemical parameters [extractable organic carbon ( EOC), dissolved organic nitrogen (DON), NH<subscript>4</subscript><superscript>+</superscript>, NO<subscript>3</subscript><superscript>−</superscript>], and abundances of genes encoding the key enzymes involved in ammonia oxidation ( amoA) and denitrification ( nirK, nirS, nosZ) depended more on soil depth and block (underlying soil moisture gradient) than on elevated CO<subscript>2</subscript>. Ammonia oxidation and denitrification gene abundances, relative abundances (ratios) of nirS to nirK, of nosZ to both nirS and to nirK, and of the measured soil biochemical properties DON and NO<subscript>3</subscript><superscript>−</superscript> tended to be lower in elevated CO<subscript>2</subscript> plots as compared with ambient plots in the MED and WET blocks while the DRY block exhibited an opposite trend. High N<subscript>2</subscript>O emissions under elevated CO<subscript>2</subscript> in the MED and WET blocks correlated with lower nosZ to nirK ratios, suggesting that increased N<subscript>2</subscript>O emissions under elevated CO<subscript>2</subscript> might be caused by a higher proportion of N<subscript>2</subscript>O-producing rather than N<subscript>2</subscript>O consuming ( N<subscript>2</subscript> producing) denitrifiers. [ABSTRACT FROM AUTHOR]
Details
- Language :
- English
- ISSN :
- 13541013
- Volume :
- 17
- Issue :
- 10
- Database :
- Complementary Index
- Journal :
- Global Change Biology
- Publication Type :
- Academic Journal
- Accession number :
- 65217804
- Full Text :
- https://doi.org/10.1111/j.1365-2486.2011.02470.x