Premium
PLANT AND MICROBIAL CONTROLS ON NITROGEN RETENTION AND LOSS IN A HUMID TROPICAL FOREST
Author(s) -
Templer Pamela H.,
Silver Whendee L.,
Pett-Ridge Jennifer,
M. DeAngelis Kristen,
Firestone Mary K.
Publication year - 2008
Publication title -
ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.144
H-Index - 294
eISSN - 1939-9170
pISSN - 0012-9658
DOI - 10.1890/07-1631.1
Subject(s) - nitrification , denitrification , nitrogen , soil water , sink (geography) , environmental chemistry , nitrogen cycle , tropical and subtropical moist broadleaf forests , chemistry , agronomy , environmental science , ecology , subtropics , biology , cartography , organic chemistry , geography
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 15 NH 4 and 15 NO 3 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 4 + produced was rapidly converted to NO 3 − via the process of gross nitrification. During the first 24 hours, plant roots took up 28% of the inorganic N produced, dominantly as NH 4 + , and were a greater sink for N than soil microbial biomass. Soil microbes were not a significant sink for added 15 NH 4 + or 15 NO 3 − during the first 24 hours, and only for 15 NH 4 + 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 2 O. Rates of dissimilatory NO 3 − reduction to NH 4 + (DNRA) were high in this forest, accounting for up to 25% of gross NH 4 + production and 35% of gross nitrification. DNRA was a major sink for NO 3 − , which may have contributed to the lower rates of N 2 O and leaching losses. Despite considerable N conservation via DNRA and plant NH 4 + uptake, the fate of ∼ 45% of the NO 3 − produced and 4% of the NH 4 + produced were not measured in our fluxes, suggesting that other important pathways for N retention and loss (e.g., denitrification to N 2 ) are important in this system. The high proportion of mineralized N that was rapidly nitrified and the fates of that NO 3 − 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 4 + as a potential N‐conserving mechanism within tropical forests.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom