Back to Search
Start Over
PLANT AND MICROBIAL CONTROLS ON NITROGEN RETENTION AND LOSS IN A HUMID TROPICAL FOREST.
- Source :
-
Ecology [Ecology] 2008 Nov; Vol. 89 (11), pp. 3030-3040. - Publication Year :
- 2008
-
Abstract
- Humid tropical forests are generally characterized by the lack of nitrogen (N) limitation to net primary productivity, yet paradoxically have high potential for N loss. We conducted an intensive field experiment with <superscript>15</superscript> NH <subscript>4</subscript> and <superscript>15</superscript> NO <subscript>3</subscript> additions to highly weathered tropical forest soils in Puerto Rico to determine the relative importance of N retention and loss mechanisms. Over one-half of all the NH <subscript>4</subscript> <superscript>+</superscript> produced was rapidly converted to NO <subscript>3</subscript> <superscript>-</superscript> via the process of gross nitrification. During the first 24 hours, plant roots took up 28% of the inorganic N produced, dominantly as NH <subscript>4</subscript> <superscript>+</superscript> , and were a greater sink for N than soil microbial biomass. Soil microbes were not a significant sink for added <superscript>15</superscript> NH <subscript>4</subscript> <superscript>+</superscript> or <superscript>15</superscript> NO <subscript>3</subscript> <superscript>-</superscript> during the first 24 hours, and only for <superscript>15</superscript> NH <subscript>4</subscript> <superscript>+</superscript> after 7 days. Patterns of microbial community composition, as determined by terminal restriction fragment length polymorphism analysis (TRFLP), were weakly but significantly correlated with nitrification and denitrification to N <subscript>2</subscript> O. Rates of dissimilatory NO <subscript>3</subscript> <superscript>-</superscript> reduction to NH <subscript>4</subscript> <superscript>+</superscript> (DNRA) were high in this forest, accounting for up to 25% of gross NH <subscript>4</subscript> <superscript>+</superscript> production and 35% of gross nitrification. DNRA was a major sink for NO <subscript>3</subscript> <superscript>-</superscript> , which may have contributed to the lower rates of N <subscript>2</subscript> O and leaching losses. Despite considerable N conservation via DNRA and plant NH <subscript>4</subscript> <superscript>+</superscript> uptake, the fate of ∼45% of the NO <subscript>3</subscript> <superscript>-</superscript> produced and 4% of the NH <subscript>4</subscript> <superscript>+</superscript> produced were not measured in our fluxes, suggesting that other important pathways for N retention and loss (e.g., denitrification to N <subscript>2</subscript> ) are important in this system. The high proportion of mineralized N that was rapidly nitrified and the fates of that NO <subscript>3</subscript> <superscript>-</superscript> highlight the key role of gross nitrification as a proximate control on N retention and loss in humid tropical forest soils. Furthermore, our results demonstrate the importance of the coupling between DNRA and plant uptake of NH <subscript>4</subscript> <superscript>+</superscript> as a potential N-conserving mechanism within tropical forests.<br /> (© 2008 by the Ecological Society of America.)
Details
- Language :
- English
- ISSN :
- 1939-9170
- Volume :
- 89
- Issue :
- 11
- Database :
- MEDLINE
- Journal :
- Ecology
- Publication Type :
- Academic Journal
- Accession number :
- 31766805
- Full Text :
- https://doi.org/10.1890/07-1631.1