Journal article

Global soil nitrogen cycle pattern and nitrogen enrichment effects: Tropical versus subtropical forests


Authors listElrys, Ahmed S; Zhu, QiLin; Jiang, Chunlan; Liu, Juan; Sobhy, Hamida HH; Shen, Qunli; Uwiragiye, Yves; Wu, Yanzheng; El-Tarabily, Khaled A; Meng, Lei; Müller, Christoph; Zhang, Jinbo

Publication year2023

Pages1905-1921

JournalGlobal Change Biology

Volume number29

Issue number7

ISSN1354-1013

eISSN1365-2486

DOI Linkhttps://doi.org/10.1111/gcb.16603

PublisherWiley


Abstract

Tropical and subtropical forest biomes are a main hotspot for the global nitrogen (N) cycle. Yet, our understanding of global soil N cycle patterns and drivers and their response to N deposition in these biomes remains elusive. By a meta-analysis of 2426-single and 161-paired observations from 89 published 15 N pool dilution and tracing studies, we found that gross N mineralization (GNM), immobilization of ammonium (INH4) and nitrate (INO3), and dissimilatory nitrate reduction to ammonium (DNRA) were significantly higher in tropical forests than in subtropical forests. Soil N cycle was conservative in tropical forests with ratios of gross nitrification (GN) to INH4 (GN/INH4) and of soil nitrate to ammonium (NO3−/NH 4+) less than one, but was leaky in subtropical forests with GN/INH4 and NO3−/NH 4+ higher than one. Soil NH4+ dynamics were mainly controlled by soil substrate (e.g., total N), but climatic factors (e.g., precipitation and/or temperature) were more important in controlling soil NO3− dynamics. Soil texture played a role, as GNM and INH4 were positively correlated with silt and clay contents, while INO3 and DNRA were positively correlated with sand and clay contents, respectively. The soil N cycle was more sensitive to N deposition in tropical forests than in subtropical forests. Nitrogen deposition leads to a leaky N cycle in tropical forests, as evidenced by the increase in GN/INH4, NO3−/NH 4+, and nitrous oxide emissions and the decrease in INO3 and DNRA, mainly due to the decrease in soil microbial biomass and pH. Dominant tree species can also influence soil N cycle pattern, which has changed from conservative in deciduous forests to leaky in coniferous forests. We provide global evidence that tropical, but not subtropical, forests are characterized by soil N dynamics sustaining N availability and that N deposition inhibits soil N retention and stimulates N losses in these biomes.




Citation Styles

Harvard Citation styleElrys, A., Zhu, Q., Jiang, C., Liu, J., Sobhy, H., Shen, Q., et al. (2023) Global soil nitrogen cycle pattern and nitrogen enrichment effects: Tropical versus subtropical forests, Global Change Biology, 29(7), pp. 1905-1921. https://doi.org/10.1111/gcb.16603

APA Citation styleElrys, A., Zhu, Q., Jiang, C., Liu, J., Sobhy, H., Shen, Q., Uwiragiye, Y., Wu, Y., El-Tarabily, K., Meng, L., Müller, C., & Zhang, J. (2023). Global soil nitrogen cycle pattern and nitrogen enrichment effects: Tropical versus subtropical forests. Global Change Biology. 29(7), 1905-1921. https://doi.org/10.1111/gcb.16603


Last updated on 2025-21-05 at 17:36