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Leaky nitrogen cycle in pristine African montane rainforest soil
Author(s) -
Rütting Tobias,
Cizungu Ntaboba Landry,
Roobroeck Dries,
Bauters Marijn,
Huygens Dries,
Boeckx Pascal
Publication year - 2015
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1002/2015gb005144
Subject(s) - rainforest , tropical rainforest , environmental science , cycling , tropical and subtropical moist broadleaf forests , mineralization (soil science) , nitrogen cycle , humid subtropical climate , leaching (pedology) , tropics , nitrogen , tropical climate , ecology , subtropics , agroforestry , agronomy , soil water , forestry , geography , soil science , chemistry , biology , medicine , organic chemistry , pathology
Many pristine humid tropical forests show simultaneously high nitrogen (N) richness and sustained loss of bioavailable N forms. To better understand this apparent upregulation of the N cycle in tropical forests, process‐based understanding of soil N transformations, in geographically diverse locations, remains paramount. Field‐based evidence is limited and entirely lacking for humid tropical forests on the African continent. This study aimed at filling both knowledge gaps by monitoring N losses and by conducting an in situ 15 N labeling experiment in the Nyungwe tropical montane forest in Rwanda. Here we show that this tropical forest shows high nitrate (NO 3 − ) leaching losses, confirming findings from other parts of the world. Gross N transformation rates point to an open soil N cycle with mineralized N nitrified rather than retained via immobilization; gross immobilization of NH 4 + and NO 3 − combined accounted for 37% of gross mineralization, and plant N uptake is dominated by ammonium (NH 4 + ). This study provided new process understanding of soil N cycling in humid tropical forests and added geographically independent evidence that humid tropical forests are characterized by soil N dynamics and N inputs sustaining bioavailable N loss.